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by Donald B. MacGowan

New at iTunes: Hawaii Dream Vacation iPhone/iPod Touch App Puts the Magic of Hawaii in the Palm of Your Hand. Interactive maps, GPS and WiFi enabled, dozens of videos…available at iTunes or www.tourguidehawaii.com.

The Mauna Ulu A'a and Pahoehoe Lava Flows at Alanui Kahiko, Hawaii Volcanoes National Park: Graphic from Photo by Donnie MacGowan

There are many wondrous, enigmatic and fascinating attractions on the Big Island of Hawaii, some better known than others, many out of the way and generally off the beaten track. Tour Guide Hawaii has produced an encyclopedic collection of the most up-to-date information, presented as short GPS-cued videos, in an app downloadable to iPhone and iPod Touch that covers the entire Big Island, highlighting the popular and the uncrowded, the famous and the secluded, the adventurous and the relaxing.

New at iTunes: Hawaii Dream Vacation iPhone/iPod Touch App Puts the Magic of Hawaii in the Palm of Your Hand. Interactive maps, GPS and WiFi enabled, dozens of videos…available at iTunes or www.tourguidehawaii.com.

Pahoehoe flow at night on Kilauea, Hawaii Volcanoes National Park: Photo Courtesy of Big Island Air

Pahoehoe, A’a, Pele’s Tears and Pele’s Hair

It is obvious to even the most causal observer that various lava formations and lava fields of Hawaii display two distinctly different types of lava flows. Some flows are very smooth, with obvious, well-preserved flow structures, looking almost like poured taffy that has hardened. Others appear more clunky, clinkery and jagged like a field of sharp boulders and cobbles. These two unique rock types result from two distinctly different types of lava flows, Pahoehoe and A’a.

New at iTunes: Hawaii Dream Vacation iPhone/iPod Touch App Puts the Magic of Hawaii in the Palm of Your Hand. Interactive maps, GPS and WiFi enabled, dozens of videos…available at iTunes or www.tourguidehawaii.com.

Pahoehoe lava flow, showing well-developed flow structures at La'epuki, Hawaii Volcanoes National Park: Photo by Donald B MacGowan

The onomatopoetic word “pahoehoe” flows across your tongue in the same fashion that pahoehoe lava flows down the volcano. Gelatinous and smooth, it looks a bit like small waves with bulbous, lobate “toes” at the front of the flow. As the advancing lobe cools, a thin crust forms on its surface. This crust is expanded and broken by the pressure of lava flowing in behind, in a continually advancing flow. A distinctive breaking-glass sound is made when that cooling crust fractures, which can be disorienting and surprising at first.

New at iTunes: Hawaii Dream Vacation iPhone/iPod Touch App Puts the Magic of Hawaii in the Palm of Your Hand. Interactive maps, GPS and WiFi enabled, dozens of videos…available at iTunes or www.tourguidehawaii.com.

A flowing field of pahoehoe lava, note the intense orange glow just under the chilled surface, Hawaii Volcanoes National Park: Photo by Donald B MacGowan

The Hawaiian word “pahoehoe” means “to paddle a canoe vigorously” or “well stirred” and indeed, pahoehoe lava has the look of water being furiously paddled by canoeists, or indeed, of well-stirred poi. These highly fluid pahoehoe flows form from the hottest lava with high dissolved fluid content. As the lava cools and de-gasses, the second kind of flow, a’a lava, is formed from it.

New at iTunes: Hawaii Dream Vacation iPhone/iPod Touch App Puts the Magic of Hawaii in the Palm of Your Hand. Interactive maps, GPS and WiFi enabled, dozens of videos…available at iTunes or www.tourguidehawaii.com.

An a'a lava flow, piled up on a pahoehoe flow in front of Pu'u Huluhulu, Hawaii Volcanoes National Park: Photo by Donald B MacGowan

A’a flows travel along as a dense mass of highly viscous lava covered in sharp, broken shards called clinkers. Like a tractor tread, a’a clinkers fall off the advancing front of the flow and are buried as the flow moves forward over them, sounding for all the world like a herd of wild bulls has run amok in the world’s largest china shop.

New at iTunes: Hawaii Dream Vacation iPhone/iPod Touch App Puts the Magic of Hawaii in the Palm of Your Hand. Interactive maps, GPS and WiFi enabled, dozens of videos…available at iTunes or www.tourguidehawaii.com.

The Kuamo'o Battlefield, near Kailua Kona Hawaii is an example of a Hawaiian battle that was fought on an a'a flow. Note the large Hawaiian tombs made of a'a: Photo by Donald B MacGowan

A’a lava, which cools to great piles of razor sharp clinkers, has given rise to the myth that its name derives from Hawaiian’s walking across the cooled a’a barefoot, wincing and saying “Ah! Ah!” with every cringing step. In fact, the word “a’a” in Hawaiian not only means “to blaze or glow” but also “to dare or challenge”. It is a testament to the toughness of Hawaiian warriors that when choosing the site for a battle field, inevitably they chose to fight on an a’a field—using the razor sharp a’a strewn along the landscape as a weapon in and of itself.

New at iTunes: Hawaii Dream Vacation iPhone/iPod Touch App Puts the Magic of Hawaii in the Palm of Your Hand. Interactive maps, GPS and WiFi enabled, dozens of videos…available at iTunes or www.tourguidehawaii.com.

An a'a lava flow engulfs pahoehoe lava flow at Alanui Kahiko, Hawaii Volcanoes National Park: Photo by Donald B MacGowan

Flows generally emerge from the volcano as pahoehoe and change to a’a as they cool and de-gas or as they are subjected to stress and strain forces. It is especially common to find pahoehoe flows changing to a’a in the midst of a steep drop over a cliff, or when butted-up against an impediment to flow. Like the cucumber becoming a pickle, once pahoehoe turns to a’a, in can never turn back into pahoehoe.

New at iTunes: Hawaii Dream Vacation iPhone/iPod Touch App Puts the Magic of Hawaii in the Palm of Your Hand. Interactive maps, GPS and WiFi enabled, dozens of videos…available at iTunes or www.tourguidehawaii.com.

Littoral explosions cause lava to splatter out into the blowing wind where Pele's Tears and Pele's Hair can form, Waikupanaha, Hawaii: Photo by Donald B MacGowan

Where fire fountains and geysers of lava occur, Pele’s hair and Pele’s tears will form. Pele’s hair are thin, fiber-like strands of basalt glass pulled and spun from the lava fountain by the blowing wind,. Pele’s tears are the droplet-sized, cooled splashes of basalt glass that from from showering, spraying lava.

New at iTunes: Hawaii Dream Vacation iPhone/iPod Touch App Puts the Magic of Hawaii in the Palm of Your Hand. Interactive maps, GPS and WiFi enabled, dozens of videos…available at iTunes or www.tourguidehawaii.com.

Pele's Hair from Kilauea Volcano, Hawaii Photo by Donald B MacGowan

All media copyright 2010 by Donald B. MacGowan. All rights reserved.

New at iTunes: Hawaii Dream Vacation iPhone/iPod Touch App Puts the Magic of Hawaii in the Palm of Your Hand. Interactive maps, GPS and WiFi enabled, dozens of videos…available at iTunes or www.tourguidehawaii.com.

Pele's Tears from Kilauea Volcano, Hawaii: Photo by Donald B MacGowan

The best of Tour Guide Hawaii’s free content about traveling to, and exploring, the Big island, can be found here.

For more information on traveling to Hawaii in general and on touring the Big Island in particular, please also visit www.tourguidehawaii.com and www.tourguidehawaii.blogspot.com.
All media copyright 2010 by Donald B. MacGowan. All rights reserved.
New at iTunes: Hawaii Dream Vacation iPhone/iPod Touch App Puts the Magic of Hawaii in the Palm of Your Hand. Interactive maps, GPS and WiFi enabled, dozens of videos…available at iTunes or www.tourguidehawaii.com.

Pahoehoe lava flowing on Kilauea Volcano, Hawaii, showing large-scale flow structures: Photo Courtesy of Big Island Air

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by Donald B. MacGowan

New at iTunes: Hawaii Dream Vacation iPhone/iPod Touch App Puts the Magic of Hawaii in the Palm of Your Hand. Interactive maps, GPS and WiFi enabled, dozens of videos…available at iTunes or www.tourguidehawaii.com.

Hikers pause to look over the summit from Mauna Loa from the summit of Mauna Kea, Hawaii Graphic From Photo by Donald B MacGowan

There are many wondrous, enigmatic and fascinating attractions on the Big Island of Hawaii, some better known than others, many out of the way and generally off the beaten track. Tour Guide Hawaii has produced an encyclopedic collection of the most up-to-date information, presented as short GPS-cued videos, in an app downloadable to iPhone and iPod Touch that covers the entire Big Island, highlighting the popular and the uncrowded, the famous and the secluded, the adventurous and the relaxing.

New at iTunes: Hawaii Dream Vacation iPhone/iPod Touch App Puts the Magic of Hawaii in the Palm of Your Hand. Interactive maps, GPS and WiFi enabled, dozens of videos…available at iTunes or www.tourguidehawaii.com.

A view from the summit of Hualalai to Mauna Loa Hawaii Photo by Donald B MacGowan

The Volcanoes of Hawaii Island

The Hawaiian Archipelago, part of the Hawaiian Island-Emperor Seamount chain, is the most isolated island group earth and is comprised entirely of volcanic islands and their fringing reefs.  The archipelago was formed as one of the Earth’s great tectonic plates, the Pacific Plate, moved steadily northwest over a stationary plume of molten material welling up from the Earth’s mantle, called a “hot spot”.

New at iTunes: Hawaii Dream Vacation iPhone/iPod Touch App Puts the Magic of Hawaii in the Palm of Your Hand. Interactive maps, GPS and WiFi enabled, dozens of videos…available at iTunes or www.tourguidehawaii.com.

Fumes bellow from skylights in an active lava tube on Kilauea Volcano, Hawaii Photo by Kelly Kuchman

Creating a chain of volcanic islands that, today, stretches from the Aleutian Islands to the Big Island of Hawaii, this hotspot gave rise to at least 129 separate volcanoes in the past 86 million years.  There are 19 islands and atolls, and dozens of separate islets, seamounts, reefs and shoals in the Hawaiian Island portion of this chain, stretching from Kure Atoll to Hawaii Island (please go here for a complete discussion of the geologic history of the Hawaiian Islands).

New at iTunes: Hawaii Dream Vacation iPhone/iPod Touch App Puts the Magic of Hawaii in the Palm of Your Hand. Interactive maps, GPS and WiFi enabled, dozens of videos…available at iTunes or www.tourguidehawaii.com.

Halema'uma'u Crater and Eruption on Kilauea, Hawaii Photo by Donnie MacGowan

Hawai’i is the youngest island in the Archipelago and first began forming about a million years ago as volcanic vents opened above the mantle “hot spot” on the ocean bottom and molten lava began pouring onto the sea floor. Over the centuries, the making of the Big Island as we know it today eventually entailed the growth and conjoining of six separate volcanoes, building all the way up from the seafloor, some 18,000 feet below the ocean’s surface.  These volcanoes, from northwest to southeast, are named Mahukona, Kohala, Mauna Kea, Hualalai, Mauna Loa and Kilauea, and become younger as one moves north to south.

New at iTunes: Hawaii Dream Vacation iPhone/iPod Touch App Puts the Magic of Hawaii in the Palm of Your Hand. Interactive maps, GPS and WiFi enabled, dozens of videos…available at iTunes or www.tourguidehawaii.com.

Lava Flowing Into the Sea at Waikupanaha, Hawaii Photo by Donald B MacGowan

Mahukona Volcano, just off the Big Island’s northwest coast, was the first volcano to start forming. Now submerged beneath the surface of the ocean because it is sinking into the Earth’s crust under its own vast weight, Mahukona is no longer visible.  As the Pacific Plate slowly continued moving northwestward over the hotspot, the location of the rising magma moved relatively southeastward, and through time the rest of the Big Island volcanoes formed along that path.

New at iTunes: Hawaii Dream Vacation iPhone/iPod Touch App Puts the Magic of Hawaii in the Palm of Your Hand. Interactive maps, GPS and WiFi enabled, dozens of videos…available at iTunes or www.tourguidehawaii.com.

Kohala Mountain from the slopes of Mauna Kea Photo by Donald B MacGowan

After Mahukona, Kohala Volcano, the precursor to today’s Kohala Mountain, erupted next.  As Kohala Volcano emerged from the sea and joined with Mahukona, a much larger Big Island began forming. With continued movement of the Pacific Plate, the center of volcanism migrated on to Mauna Kea and Hualalai, the middle-aged volcanoes, and finally on to Mauna Loa and Kilauea, which are the youngest volcanoes on the island.  Over the geologically short time of several hundred thousand years, these volcanoes erupted thousands of thin flows which spread over, and built upon, older flows; each volcano growing until it finally emerged from the sea. As time went on, lava flows from one volcano began to overlap flows from other, nearby volcanoes and eventually the peaks coalesced into a single island, the Big Island.

New at iTunes: Hawaii Dream Vacation iPhone/iPod Touch App Puts the Magic of Hawaii in the Palm of Your Hand. Interactive maps, GPS and WiFi enabled, dozens of videos…available at iTunes or www.tourguidehawaii.com.

Lava from Kilauea flows into the sea at La'epuki, Hawaii Photo by Donald B MacGowan

In geologically recent times, a new volcano, Lo’ihi, began forming about 18 miles off the southeast coast of the Big Island.  In time, Loihi may join its mass with that of Kilauea, again changing the size and shape of the Big Island.  It is estimated that Lo’ihi, whose summit lies approximately 3,178 feet below the surface of the ocean today, will begin to protrude above the surface in about 10,000 years.

New at iTunes: Hawaii Dream Vacation iPhone/iPod Touch App Puts the Magic of Hawaii in the Palm of Your Hand. Interactive maps, GPS and WiFi enabled, dozens of videos…available at iTunes or www.tourguidehawaii.com.

Hualalai Volcano from Saddle Road, Hawaii Photo by Donald B MacGowan

Currently, the remnants of Mahukona and Kohala volcanoes are completely extinct; Hualalai and Mauna Kea are considered dormant and Mauna Loa, Kilauea and Loihi are still very active.   This means that eruptions of Mahukona and Kohala are not at all likely. Eruptions of Mauna Kea and Hualalai are probable at some time in the future, though the major phase of mountain building is over for these volcanoes.  Movement of the Pacific Plate has moved both Hualalai and Mauna Kea off the hot spot so only remnants of liquid magma reside beneath them. These late-stage, mature Hawaiian volcanoes experience violent, explosive eruptions which are spectacular but comparatively small, volume-wise.  Late-stage Hawaiian volcanic eruptions are characterized by crater-forming explosions, tephra-cone building and ash ejecting events.

New at iTunes: Hawaii Dream Vacation iPhone/iPod Touch App Puts the Magic of Hawaii in the Palm of Your Hand. Interactive maps, GPS and WiFi enabled, dozens of videos…available at iTunes or www.tourguidehawaii.com.

Mauna Loa from Bird Park in Hawaii Volcanoes National Park: Photo by Donald B MacGowan

Mauna Loa and Kilauea are both considered active volcanoes. Although inflation and dilation events are common on the summit of Mauna Loa, it has not erupted since 1984; Mauna Loa could, however, erupt at any time.  Since 1833 when accurate records began to be kept, there have been 33 eruptions of Mauna Loa, making it one of the most active volcanoes on earth.  Its name means “long mountain”, and Mauna Loa is capable of erupting huge amounts of lava in a very short time, dwarfing the current output of Kilauea.  The most massive mountain on earth, this prolific effusion of molten rock accounts for Mauna Loa’s vast bulk.

New at iTunes: Hawaii Dream Vacation iPhone/iPod Touch App Puts the Magic of Hawaii in the Palm of Your Hand. Interactive maps, GPS and WiFi enabled, dozens of videos…available at iTunes or www.tourguidehawaii.com.

Kilauea eruption in Halema'uma'u Crater at night, Hawaii Volcanoes National Park: Photo by Donald B MacGowan

Kilauea, once believed to be a mere satellite vent on Mauna Loa, is known to be a separate and distinct volcano with its own, geologically separate magma chamber and subterranean plumbing. Nearly half a million years old, Kilauea’s most recent eruption has been continuous since 1983 making it currently the world’s most active volcano. Indeed, between 1983 and 2009 about 700 acres of new land were produced by lava flows from Kilauea.  Articles on how to see the active lava flows on Kilauea can be found here and here. A detailed guide to enjoying Hawaii Volcanoes National Park, featuring Kilauea and Mauna Loa Volcanoes can be found here.

New at iTunes: Hawaii Dream Vacation iPhone/iPod Touch App Puts the Magic of Hawaii in the Palm of Your Hand. Interactive maps, GPS and WiFi enabled, dozens of videos…available at iTunes or www.tourguidehawaii.com.

Kilauea buried the town of Kalapana in the early 1990s and formed Kaimu Black, Hawaii: Photo by Donald B MacGowan

Because the time-scale of human experience is virtually instantaneous compared to the aeons-long march of geologic history, there is continuing human drama, a tension, between short-sighted humans attempting to establish roads, villages and towns, and the ongoing geologic processes of the landscapes they choose to inhabit.  In very recent decades, the towns of Kapoho, Kalapana and Kaimu have been inundated, destroyed and buried by Kilauea Volcano (please see a related article on the death and rebirth of Kalapana, here).  As more people move to Hawaii, more such drama is inevitable.

New at iTunes: Hawaii Dream Vacation iPhone/iPod Touch App Puts the Magic of Hawaii in the Palm of Your Hand. Interactive maps, GPS and WiFi enabled, dozens of videos…available at iTunes or www.tourguidehawaii.com.

Mauna Loa floats above the fields of Kohala, Hawaii Photo by Donald B MacGowan

The evolution of Hawaiian volcanoes continues even after the major phase of eruptive activity subsides. There are great differences, obvious to even the most casual observer, between the elongated, fluted ridge-like shape of Kohala Mountain and the lower angled slopes of Mauna Loa and Kilauea.  Likewise, steep-sided Mauna Kea has a greatly different physical aspect than does gently-sloped, shield-shaped Mauna Loa.  These differences are accounted for by the differences in their relative ages, and thus eruptive and erosive stages.

New at iTunes: Hawaii Dream Vacation iPhone/iPod Touch App Puts the Magic of Hawaii in the Palm of Your Hand. Interactive maps, GPS and WiFi enabled, dozens of videos…available at iTunes or www.tourguidehawaii.com.

The steeper, crater-poked slopes of Hualalai indicate it has moved on to the later stages of volcanism Photo by Donald B MacGowan

Remembering that the angle of repose of Hawaiian lava is about 6 degrees, the shield-shaped, gentle slopes of Mauna Loa and Kilauea reflect the fact that they are quite young and are still in the shield-building stage, being built-up by successive flows of highly fluid lava.  The much steeper flanks of Hualalai and Mauna Kea volcanoes are due to the late-stage, explosive eruptions, to erosion and to ashfall which piles up much more steeply than the flowing lava.  The fluted ridges of Kohala volcano result from the deep dissection of the once shield-shaped slopes of the original volcano by streams and surface flow of water.  The distinctive steep valleys and great cliffs seen on the north and east sides of Kohala Volcano result from later process of normal faulting and giant landslides (see further discussion in an article about Waipi’o Valley, here).

New at iTunes: Hawaii Dream Vacation iPhone/iPod Touch App Puts the Magic of Hawaii in the Palm of Your Hand. Interactive maps, GPS and WiFi enabled, dozens of videos…available at iTunes or www.tourguidehawaii.com.

Glacial cirques and moraines along the Mauna Kea summit ridge, Hawaii: Photo by Donnie MacGowan

Another process, operative in the geologically recent past, has served to shape the slopes of the volcanoes of the Big Island, at least those which are or great height.  Glaciers covered the summit of Mauna Kea (and possibly Mauna Loa) three times between 200,000 and 13,000 years ago, leaving behind many glacial features such as cirques, u-shaped valleys and scoured bedrock; surviving into the present is a remnant rock glacier near the summit of Mauna Kea (a related article on the summit of Mauna Kea and the Hawaiian Snow Goddess, Poliahu, can be found here; details on exploring Mauna Kea can be found here).  Any evidence on Mauna Loa of ice-age glaciers has been covered by recent eruptions.

New at iTunes: Hawaii Dream Vacation iPhone/iPod Touch App Puts the Magic of Hawaii in the Palm of Your Hand. Interactive maps, GPS and WiFi enabled, dozens of videos…available at iTunes or www.tourguidehawaii.com.New at iTunes: Hawaii Dream Vacation iPhone/iPod Touch App Puts the Magic of Hawaii in the Palm of Your Hand. Interactive maps, GPS and WiFi enabled, dozens of videos…available at iTunes or www.tourguidehawaii.com.

Kohala Volcano is subsiding, cut by enormous valleys and giant cliff-forming landslides, Hawaii: Photo by Donald B MacGowan

Simultaneously with the ongoing eruptions and island building, due to their enormous mass, the great volcanoes of the Hawaiian Chain begin to subside into the oceanic crust.  After the majority of eruptions cease, with cooling and with a great amount of time, they eventually disappear beneath the surface of the sea completely, as Mahukona Volcano already has.

New at iTunes: Hawaii Dream Vacation iPhone/iPod Touch App Puts the Magic of Hawaii in the Palm of Your Hand. Interactive maps, GPS and WiFi enabled, dozens of videos…available at iTunes or www.tourguidehawaii.com.

Originally carved above sea level, these 500-year old petroglyphs at Keauhou today are awash due to subsidence of Hualalai Volcano: Photo by Donald B MacGowan

Today, the Big Island of Hawai’i comprises more than twice the area of all the other Hawaiian Islands combined.  It’s size is not anomalous, however, considering the geologic history of the archipelago. All the other Hawaiian Islands experienced the same pattern of volcanic eruption, growth and coalescence, as well as the gradual subsidence and submersion that Hawaii Island has, and thus at one time may have been as large as the Big Island.  Indeed, geologists have demonstrated that Maui at one time formed a single landmass, known as Maui Nui or “Big Maui”, with the islands of Lana’i, Moloka’i, and Kaho’olawe.  Continued subsidence submerged the larger landmass, leaving the four, smaller islands above the ocean surface. Ultimately, this will happen to the Big Island, as well.

New at iTunes: Hawaii Dream Vacation iPhone/iPod Touch App Puts the Magic of Hawaii in the Palm of Your Hand. Interactive maps, GPS and WiFi enabled, dozens of videos…available at iTunes or www.tourguidehawaii.com.

Looking from Mauna Kea summit to Mauna Loa, Hawaii: Photo by Donald B MacGowan

The relentless movement of the Pacific Plate carries it, with the all the islands piggy-backed, inexorably northward to the Aleutian Trench, where it is subducted underneath the North American Plate, melted, and recycled as volcanic material in the Aleutian Island volcanoes.  The Emperor Seamounts are currently undergoing such destruction, and, the evolution of the Hawaiian-Emperor Chain is such that, eventually this fate also awaits the Big Island…but not for tens of millions of years.

New at iTunes: Hawaii Dream Vacation iPhone/iPod Touch App Puts the Magic of Hawaii in the Palm of Your Hand. Interactive maps, GPS and WiFi enabled, dozens of videos…available at iTunes or www.tourguidehawaii.com.

Magical Sunset at the lava ocean entry at Waikupanaha, Hawaii Photo by Donald B MacGowan

Given the ephemeral nature of this precious island, this geologic certainty should serve to make us love and treasure the Big Island more deeply, as well as to spur us to protect and preserve it more completely.

New at iTunes: Hawaii Dream Vacation iPhone/iPod Touch App Puts the Magic of Hawaii in the Palm of Your Hand. Interactive maps, GPS and WiFi enabled, dozens of videos…available at iTunes or www.tourguidehawaii.com.

Silent sunset descends upon Hawaii Island at Kahalu'u Beach: Photo by Donald B MacGowan

The best of Tour Guide Hawaii’s free content about traveling to, and exploring, the Big island, can be found here.

New at iTunes: Hawaii Dream Vacation iPhone/iPod Touch App Puts the Magic of Hawaii in the Palm of Your Hand. Interactive maps, GPS and WiFi enabled, dozens of videos…available at iTunes or www.tourguidehawaii.com.

Near the summit of Kohala Mountain, Photo by Donnie MacGowan

For more information on traveling to Hawaii in general and on touring the Big Island in particular, please also visit www.tourguidehawaii.com and www.tourguidehawaii.blogspot.com.

All media copyright 2010 by Donald B. MacGowan. All rights reserved.

New at iTunes: Hawaii Dream Vacation iPhone/iPod Touch App Puts the Magic of Hawaii in the Palm of Your Hand. Interactive maps, GPS and WiFi enabled, dozens of videos…available at iTunes or www.tourguidehawaii.com.

Full moon over Mauna Kea, Hawaii Photo by Donald B MacGowan

by Donald B. MacGowan

New at iTunes: Hawaii Dream Vacation iPhone/iPod Touch App Puts the Magic of Hawaii in the Palm of Your Hand. Interactive maps, GPS and WiFi enabled, dozens of videos…available at iTunes or www.tourguidehawaii.com.

Visitors Watch the Halema'uma'u eruption of Kilauea at Hawaii Volcanoes National Park Graphic from Photo by Donald B MacGowan

There are many wondrous, enigmatic and fascinating attractions on the Big Island of Hawaii, some better known than others, many out of the way and generally off the beaten track. Tour Guide Hawaii has produced an encyclopedic collection of the most up-to-date information, presented as short GPS-cued videos, in an app downloadable to iPhone and iPod Touch that covers the entire Big Island, highlighting the popular and the uncrowded, the famous and the secluded, the adventurous and the relaxing.

New at iTunes: Hawaii Dream Vacation iPhone/iPod Touch App Puts the Magic of Hawaii in the Palm of Your Hand. Interactive maps, GPS and WiFi enabled, dozens of videos…available at iTunes or www.tourguidehawaii.com.

Aerial view of Pu'u O'o Vent on Kilauea, Hawaii Volcanoes National Park Photo by Shannon Walker

The Geologic History of the Hawaiian Islands

The Hawaiian Islands, part of a much longer chain of oceanic islands and seamounts called the Hawaiian-Emperor Chain, is comprised of 8 principal islands and 124 islets, shoals, atolls, seamounts and banks, all volcanic in origin.  The Hawaiian Islands proper extend from Kure Atoll in the mid-Pacific, trending southeast to Hawaii Island (the Big Island) and Lo’ihi submarine volcano.  The eight major islands of the Hawaiian chain are named, from northwest to southeast, Ni’ihau, Kauai, O`ahu, Moloka`i, Lana`i, Kaho`olawe, Maui, and Hawai`i. Unraveling the geologic history of the Hawaiian Islands provides a fascinating glimpse into structures and process occurring deep within our Earth.  To understand how the Hawaiian Islands were formed, let’s review a bit about the nature of our planet.

New at iTunes: Hawaii Dream Vacation iPhone/iPod Touch App Puts the Magic of Hawaii in the Palm of Your Hand. Interactive maps, GPS and WiFi enabled, dozens of videos…available at iTunes or www.tourguidehawaii.com.

Kilauea Lava Stream, Hawaii Photo courtesy of Big Island Air

Layered like an onion, our seeming solid earth is actually a heaving mass composed of various solid, partially-molten, semi-plastic and liquid layers.  The solid crust (or lithosphere), which covers the entire surface of the earth, seems strong and robust but is, in fact, quite thin and malleable.  About the same thickness relative to the rest of the planet as an onion skin is to an onion, the Earth’s silica-rich crust more or less floats upon a much thicker, partially molten, more iron and magnesium-rich, semi-plastic layer of much hotter material called the “mantle”.  Below the mantle are the liquid outer core and the solid inner core of the Earth.

New at iTunes: Hawaii Dream Vacation iPhone/iPod Touch App Puts the Magic of Hawaii in the Palm of Your Hand. Interactive maps, GPS and WiFi enabled, dozens of videos…available at iTunes or www.tourguidehawaii.com.

Halema'uma'u Crater and eruption on Kilauea, Hawaii: Photo by Donnie MacGowan

Earth’s crust comes in basically two varieties, oceanic crust which is quite thin (only 5-7 km thick) and continental crust, which is much thicker than oceanic crust (up to 200 km thick).  Oceanic crust is composed almost wholly of an effusive volcanic rock type called “basalt”, its intrusive volcanic, subsurface equivalent called “gabbro” and a thin covering of sediment. The continental crust, which underlies the seven continents and the more massive islands, and upon which most human activity takes place, on the other hand, is composed not only of basalt and gabbro, but all the other rock types as well.  Continental crust is much less dense than oceanic crust, being much more silica-rich, and therefore is more buoyant on the mantle.  This, in part, accounts for its relative thickness and higher elevation compared to the denser, thinner oceanic crust.

New at iTunes: Hawaii Dream Vacation iPhone/iPod Touch App Puts the Magic of Hawaii in the Palm of Your Hand. Interactive maps, GPS and WiFi enabled, dozens of videos…available at iTunes or www.tourguidehawaii.com.

Lava from Kilauea flows into the sea at La'epuki, Hawaii: Photo by Donald B MacGowan

The Earth’s crust is further divided-up into various distinct pieces, called “tectonic plates”, all moving relative to each other. Plates are composed almost wholly of either oceanic or continental crustal material. These plates “float” on the semi-plastic mantle, and are carried along by currents on the mantle’s surface. Mantle currents are caused by various physical process of heat transport within the mantle.   Think of a pot of boiling soup; the point of the boil in the soup is analogous to the heat transfer in the mantle and the skim of chilled soup riding around on the surface is analogous to the moving tectonic plates carried on top of the mantle.

New at iTunes: Hawaii Dream Vacation iPhone/iPod Touch App Puts the Magic of Hawaii in the Palm of Your Hand. Interactive maps, GPS and WiFi enabled, dozens of videos…available at iTunes or www.tourguidehawaii.com.

Hikers pause to look over at the summit of Mauna Loa From the summit of Mauna Kea, Hawaii: Photo by Donald B MacGowan

Interactions along the edges of these plates, whether slipping past each other (such as along the San Andreas Fault), one riding up over another (such as beneath the Himalayan Mountains), or one being subducted beneath the other (such as along the western edge of North America), accounts for much of the earthquake, mountain-building and volcanic activity seen on the surface of the earth, and plate margins are certainly the most geologically active places on earth.

New at iTunes: Hawaii Dream Vacation iPhone/iPod Touch App Puts the Magic of Hawaii in the Palm of Your Hand. Interactive maps, GPS and WiFi enabled, dozens of videos…available at iTunes or www.tourguidehawaii.com.

Kilauea eruption in Halema'uma'u Crater at night Hawaii Volcanoes National Park: Photo by Donald B MacGowan

Occasionally, exceptions to this generality occur, and the Hawaiian Islands are one such spectacular exception. To understand the forces and process which shape the Hawaiian Islands, we must look a little closer at the origin and movement of the crust and the structure of the mantle.  Happily, we need only concern ourselves with oceanic crust in general and the Pacific Plate in particular, as well as one, singular feature of the mantle.

New at iTunes: Hawaii Dream Vacation iPhone/iPod Touch App Puts the Magic of Hawaii in the Palm of Your Hand. Interactive maps, GPS and WiFi enabled, dozens of videos…available at iTunes or www.tourguidehawaii.com.

Skylight at Kupaianaha Vent, Kilauea Volcano Hawaii: Photo by Donald B MacGowan

Oceanic crust is continually created by volcanic action along giant ridges which run generally north-south down the middle of the ocean basins.  The hot liquid magma at the ridges is much less dense than the surrounding, cold crustal rocks, and so “floats” these ridges and the still hot, newly-formed oceanic crust, up above the surrounding ocean basin, thus forming the ridge.  As volcanic eruptions along these ridges add hot, new material to the edge of the oceanic plates, the mass of new material drives the older oceanic crust away from the ridge, down both sides of it.  As the new material cools and becomes less dense, it sinks and further drives the crust away from the ridges.

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Lava Flowing Into the Sea at Waikupanaha, Hawaii Photo by Donald B MacGowan

Called “Mid-Ocean Ridge Spreading”, this process can be likened to a conveyor belt where new crust is created at the mid-ocean ridge, and is driven along by buoyancy and gravity, farther and farther away from the ridge until the plate’s leading edge interacts in some way with another tectonic plate.  Thus we see that the floors of the ocean basins, all around the world, are in constant, relative motion.  The Pacific Plate, upon which the Hawaiian Islands are built, has been moving at a rate of about 3.9 inches per year to the northwest, relative to other plate motions, for about the last 42 million years.

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Sunset on Haleakala from Kiholo, Hawaii Photo by Donnie MacGowan

But what causes the enormous volcanoes that comprise the Hawaiian Archipelago to form in the middle of the ocean basin?  As mentioned above, the mantle is far from uniform either compositionally, thermally or in terms of the processes controlling its internal motions.  There are places on the earth where, for a variety of reasons, hot and buoyant mantle plumes rise above the general surface of the mantle, into the crust, carrying great amounts of heat and semi-liquid material quite near the earth’s surface.  Called “Hot Spots”, extreme volcanism can result from these thermal plumes.  The volcanic fields at Yellowstone in North America are one such example of this “hot spot magmatism”; the Hawaiian Islands are yet another.

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The heavily-dissected mountains of Kauai completely obscure the original shield shape of the volcano Photo by Donald B MacGowan

The Hawaiian Hot Spot has caused the creation of at least 129 volcanoes on the ocean floor, the center of volcanism on the Pacific Plate continually migrating across the plate as it travels over the hot spot. Of these 129 volcanoes, 123 are extinct, three are dormant and three are active.  At first, the trend of volcanoes was almost due north-south.  Then, somewhere between 41 and 43 million years ago the relative motion between the Pacific Plate and the hot spot changed, becoming more northwesterly; this caused a sharp bend in the line of island-forming volcanoes.

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Aerial view of Pu'u O'o vent on Kilauea Volcano, Hawaii Volcanoes National Park Photo by Donald B MacGowan

Although all were formed by the same, continuing tectono-volcanic processes, two island groups are named from this bent line of islands, atolls and seamounts.  North of the bend are the Emperor Seamounts, a long chain of islands, seamounts, atolls and reefs trending steeply southeast to northwest between Abbot Seamount in the mid-Pacific and Meiji Seamount near the Aleutian Trench.  South of the bend are the Hawaiian Islands, trending from the active volcanism at the Big Island and Loihi Volcano today, gently northwest to Kure Atoll in the mid-Pacific. Movement of the Pacific Plate over the hotspot is such that Midway and Kure Atolls were where the Big Island is now, directly over the hot spot, about 30 million years ago.

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The steep sides of Mt. Rainier in Washington result from its relatively high-silica, viscous lava Photo by Donald B MacGowan

The chemical composition of the Hawaiian magmas plays a central role in determining the physical form of the Hawaiian Islands.  All crustal rocks are formed of minerals composed of aluminum and silicon oxides with varying amounts of iron, magnesium, sodium, calcium, potassium and other elements stirred in.  In lava, silica tends to polymerize and greatly increase the viscosity of the melt—thus silica-rich lavas are fairly “sticky”, forming slow moving lava flows that pile-up into steep volcanoes which are typified by explosive eruptions. Silica-poor melts, on the other hand, because they are not so polymerized, form very fluid lavas that flow quickly and easily, forming gently-sloped volcanoes typified by relatively quiescent eruptions.  Remember the key words here are: “relatively quiescent”.

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Mauna Loa floats above the fields of Kohala, Hawaii Photo by Donald B MacGowan

One glance at the profile of the Hawaiian volcanoes is enough to convince us that the lavas must be very silica poor, since they are very gently-sloped and the eruptions relatively peaceable; certainly civilized enough so that the casual viewer may approach them quite closely in relative safety.  Compare these with the very steep-sided, highly explosive eruptions of volcanoes like Mt. St. Helens, which is comprised of lava much more intermediate in silica composition, or the smoking hole in the ground that is the Yellowstone volcanic field, left by a massively explosive, very silica rich (and very, very viscous) lava erupting.

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Layered basalts in Waimea Canyon on Kauai show the structure of the Island, flow upon flow: Photo by Donald B MacGowan

The rocks formed when the lava from Hawaiian volcanoes hardens are called “basalt”.  Although you hear the term “lava rock” used by laymen, it is a nonsensical word geologically and the registered trademark of a commercial product.  Commonly misapplied, it makes even less sense than the equivalent of using the term “water solid” instead of “ice”. The name “basalt” denotes both the silica-poor composition, as well as the fact that it was erupted onto, and it has cooled at, the Earth’s surface.  When lavas cool within a magma chamber before being erupted onto the surface, they are called an “intrusive volcanic” rock; intrusive volcanic rocks formed from lavas of basalt-like composition are called “gabbros”.  There are a few rocks in the Hawaiian islands of differing composition and texture than basalt and gabbro, but they are unimportant to this discussion.

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The classic, low-angle shield shape of Mauna Loa seen from Hilo, Hawaii Photo by Donald B MacGowan

The angle of repose, which is controlled by the viscosity of the melt, is about 6 degrees for Hawaiian basalts. Melt viscosity is a function of its temperature, silica content and fluid composition.   Hawaiian basalts are very fluid because of the low silica content and high eruptive temperature (in excess of 1100 degrees C); this low viscosity accounts for low angle, “shield shape” of Hawaiian volcanoes.

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Kohala Volcano is dissected by several major fault-bounded valleys, further obscuring its original shield shape Photo by Donald B MacGowan

As soon as the Hawaiian volcano forms, other forces begin to act upon it, affecting the general “shield shape” of the volcano: tides and waves attack the edges, rivers and streams begin to dissect the shield into ridges.  As time goes on, erosion from surface water flow produces fluting along those ridges.  Great landslides produce enormous cliffs; faulting produces huge valleys and collapse produces enormous craters and calderas.  Further, the later stage of Hawaiian volcanism is typified by increasing violence, which makes deep explosion craters, steep-sided cinder cones and steeply sloped, but easily eroded, ash deposits.

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Stream erosion dissects the shield volcanoes into valley and knife-like ridges Photo by Donnie MacGowan

To look at the volcanoes of Hawaii starting in the southeast at Kilauea and Mauna Loa and moving northwest, one can see this evolution quite clearly.  Kilauea and Mauna Loa, being quite young, are still broad and shallow-sloped, basically the classic shield-shape.  Mauna Kea and Hualalai are obviously more mature, showing steeper slopes, a reflection of greater ashfall and greater erosion, as well as pocked with explosion craters and cinder cones.  Moving father along, Kohala Mountain is so deeply eroded and festooned with long, fluted ridges as well as cut by enormous canyons, that it is almost unrecognizable as a shield volcano.  And so it continues as one proceeds north through the older islands and the more highly eroded mountains; the original shield shape of the volcanoes become more and more obscured by deeper and deeper erosion.  By the time one gets to the famous and spectacular Na Pali Cliffs of Kaua’i, all that is left of the original volcano are the deeply fluted, now almost knife-like, ridges.

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Ancient Petroglyph, Keauhou Historic District, Hawaii Photo by Donald B MacGowan

The great mass of these volcanoes causes them to begin to sink back into the mantle.  This is evident on even relatively young volcanoes.  For instance, on the slopes of Hualalai Volcano on the Big Island, along the shore at Keauhou, numerous petroglyphs commemorating the famous victory of King Lonoikamakahiki of Hawaii over King Kamalalawalu of Maui were carved in the rock around the end of the 16th century.  Although when they were originally carved they stood above sea level, in the intervening four centuries, the island has sunk sufficiently that they are now mostly awash in the sea and submerged at high tide.

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Glacial cirque and terminal moraine on Mauna Kea, Hawaii Photo by Donald B MacGowan

Another process, operative in the geologically recent past, has served to shape the slopes of the Hawaiian volcanoes, at least those which are or great height.  Glaciers covered the summit of Mauna Kea (and possibly Mauna Loa and Haleakala) three times between 200,000 and 13,000 years ago, leaving behind many glacial features such as cirques, u-shaped valleys and scoured bedrock; surviving into the present is a remnant rock glacier near the summit of Mauna Kea.

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Valleys and Ridges of the Famous Na Pali Coast, Kauai Photo by Donald B MacGowan

The complex interaction of volcano growth, coalescing of various volcanoes forming a single island and the eventual subsidence of the volcanoes into the crust determines the shape and size of the individual Hawaiian Islands through time.  Today, the youngest islands are largest and the oldest islands, generally, are the smallest…this trend continues throughout the Hawaii Island/Emperor Seamount chain.

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Lava flows from Kilauea to the sea at Waikupanaha, Hawaii Photo by Donald B MacGowan

In the case of the Big Island, even though the first volcano to form, Mahukona, has completely subsided below sea level, the Big Island still comprises more than twice the area of all the other Hawaiian Islands combined, due to the large number of volcanic peaks forming it. However, through their history, all the Hawaiian Islands will experience the same pattern of growth, coalescence, subsidence and submersion, and so may have been much larger at one time.

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Haleakala from Kohala, Hawaii Photo by Donald B MacGowan

Maui, today comprised only of the remnant peaks of Haleakala and the West Maui Mountains, at one time formed a single giant landmass with the islands of Lana’i, Moloka’i, and Kaho’olawe.  As the continual northwest movement of the Pacific Plate carried Maui away from the Hawaiian hot spot, continued subsidence submerged the larger landmass, known as Maui Nui, or “Big Maui”, into the oceanic crust, leaving only these four, very much smaller, islands above the surface today.

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Superstition to Science, Pu'u Weiku Summit, Mauna Kea Photo by Donald B. MacGowan

In fact, Kaua’i, Ni’ihau and O’ahu all represent the tiny remnants of once much larger landmasses that are actively subsiding into the oceanic crust.  Tracing the Hawaiian Archipelago to the northwest, and thus to very much older islands, we see this evolution continue as the great volcanoes are completely submerged below the surface leaving only the fringing coral reefs and a tiny remnant island above sea level, such as we see at Laysan Atoll and Midway Island. Continuing along through the chain to the Emperor Seamounts, not even that much is left as all traces of these islands, once proud and beautiful like the Hawaiian Islands today, become totally submerged beneath the surface of the ocean.

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Alpen Glow on Hualalai Volcano and Sunset on Kailua Kona Hawaii: Photo by Donald B MacGowan

Add to this mental picture the fact that the Pacific Plate relentlessly drives northwestward, carrying all the Hawaiian-Emperor Chain with it, northward to the Aleutian Trench, where it is subducted and destroyed beneath the North American Plate.  Eventually, in the far-distant future, this fate awaits all these beautiful, precious islands.  Such is the ephemeral nature of the Hawaiian Islands, and this vision of their very delicate and temporary nature should make us respect and wonder at their splendor and beauty, all the more.  And increase our desire to protect and preserve them.

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The steeper, crater-poked slopes of Hualalai indicate it has moved on to the later stages of volcanism Photo by Donald B MacGowan

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Watching Lava Pour Into the Sea at Waikupanaha, Hawaii Photo by Donald B MacGowan

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Lava ocean entry, Waikupanaha, Hawaii: Graphic from Photo by Donnie MacGowan

by Donald B. MacGowan

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Halema'uma'u eruption from Sulfur Bank, Hawaii Volcanoes National Park: Graphic from Photo by Donald B MacGowan

There are many wondrous, enigmatic and fascinating attractions on the Big Island of Hawaii, some better known than others, many out of the way and generally off the beaten track. Tour Guide Hawaii has produced an encyclopedic collection of the most up-to-date information, presented as short GPS-cued videos, in an app downloadable to iPhone and iPod Touch that covers the entire Big Island, highlighting the popular and the uncrowded, the famous and the secluded, the adventurous and the relaxing.

Sulfur Banks/Steam Vents

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View along the sulfur banks to Volcano House, Hawaii Volcanoes National Park: Photo by Donnie MacGowan

Sulfur Banks, on the crater side of the road, is just one of hundreds of gas seeps on the flanks of the Kilauea summit crater spewing hydrogen sulfide, sulfur dioxide, carbon dioxide and steam. Hematite, native sulfur and gypsum minerals precipitate out of the gas flux streaming through the rocks, making colorful splashes on the outcrops. Children and people with heat or respiratory conditions, or anybody with a weak stomach should be wary of venturing down the road to see this.

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Steam vents at Hawaii Volcanoes National Park: Photo by Donald B MacGowan

Non-sulfurous steam vents, mostly across the road from the crater and at the aptly named Steaming Bluff, result from rainwater percolating down through the ground being boiled by the hot rock beneath and streaming up vents to the surface. There is a short walk to the Steaming Bluff from the Sulfur Banks parking area which comes to a breathtaking view of the crater and more productive steam vents.

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Looking past Steaming Bluff at the many steam vents in Kilauea Caldera to the eruption in Halema'uma'u Crater, Hawaii Volcanoes National Park:

Panoramic views of Kilauea Caldera and the Halema’uma’u Crater from the edge of the Sulfur Banks reveal other, numerous steam vents on the floor of the crater. Views of the current eruption in Halema’uma’u Crater are unsurpassed from this overlook…especially at night.

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Gazing into the pit of the volcano, a steam vent at Hawaii Volcanoes National Park: Photo by Donald B MacGowan

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Sulfur Banks with Mauna Loa looming in the background, Hawaii Volcanoes National Park: Photo by Donald B MacGowan

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New at iTunes: Hawaii Dream Vacation iPhone/iPod Touch App Puts the Magic of Hawaii in the Palm of Your Hand. Interactive maps, GPS and WiFi enabled, dozens of videos…available at iTunes or www.tourguidehawaii.com.

Halema'uma'u eruption from Steaming Bluff, Hawaii Volcanoes National Park: Graphic Photo By Donald B MacGowan

by Donald B. MacGowan

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The Hapuna Prince Hotel at Hapuna Beach, Kohala Coast Hawaii: Graphic from Photo by Donald B MacGowan

There are many wondrous, enigmatic and fascinating attractions on the Big Island of Hawaii, some better known than others, many out of the way and generally off the beaten track.  Tour Guide Hawaii has produced an encyclopedic collection of the most up-to-date information, presented as short GPS-cued videos, in an app downloadable to iPhone and iPod Touch that covers the entire Big Island, highlighting the popular and the uncrowded, the famous and the secluded, the adventurous and the relaxing.

Awesome, Sumptuous Hapuna Beach

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Aerial photo by Hapuna Beach, Kohala Coast Hawaii: Photo by Donald B MacGowan

Always rated in the Top 10 of American beaches, Hapuna Beach with it’s crystalline turquoise waters is the premiere beach destination on the Island of Hawai’i. A half-mile long, wide arc of phenomenal coral sand, it has everything one dreams of in a Hawai’ian beach: abundant sun, surf, clean, clear and quiet snorkeling water, palm-tree shade and well-maintained facilities.

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Hapuna Beach early in the morning, Kohala Coast, Hawaii: Photo by Donald B MacGowan

North of Kailua Kona along the Kohala Coast, the turnoff to Hapuna Beach is immediately south of the 69 Mile Marker on Highway 19. Follow the signs down to the end of the road, turn left and then right to parking. Parking is impossible after 10 a.m. on weekends and not much better on weekdays. Get there early!

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Hapuna is the ultimate family beach on Hawaii, Kohala Hawaii: Photo by Donald B MacGowan

The center of the beach is for wave play and boogie boarding, the north and south coves are quieter, for snorkeling or gentle floating. There is a small coral garden leading to amazing underwater topography and a large reef around the point on the south end of the beach.

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Hapuna Beach, Kohala Hawaii: Photo by Donald B MacGowan

Although most of the shore is relatively free of currents, only experienced snorkelers who are strong swimmers will want to snorkel around the south end of Hapuna, past a sea arch and to the reef and cove of Waialea Beach (Beach 69)—a long, but rewarding swim with some of the most incredible underwater vistas available to the snorkeler in the word.

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Sunbathing at Hapuna Beach, Kohala Coast Hawaii: Photo by Donald B MacGowan

As with all Kohala Beaches, it tends to get windy in the afternoon and there is generally a cloud cover by 2. Don’t fret; go take a hike around the rocks on the south side of the beach to the sea arch, take a nap in the shady grass fields, cook a big barbecue lunch—just be sure to stay here until sunset. I’m not joking. The sunset from Hapuna Beach, with Haleakala on Maui glowing golden-purple in the sea, is by itself worth the price of first class airfare to Hawaii. Do not forget your camera.

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It's a long hike from the parking lot to Hapuna Beach, plan ahead, Kohala Coast Hawaii: Photo by Donald B MacGowan

Within the park exist several pavilions, barbecues, picnic tables, restrooms, showers and a small vendor with some food and beach supplies. Don’t use the restrooms by the upper parking lot nor the ones on the south side of of the beach. Trust me. There are small camping cabins for rent behind the parking lot available for $30 a night. If you rent one, be prepared to thoroughly swab it out before you occupy it. Lifeguards are on duty sometimes, even though the sign on the north lifeguard tower says “No Lifeguard on Duty”.

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Hapuna is Hawaii's Most Popular Beach, Kohala Coast, Hawaii: Photo by Donald B MacGowan

Although most patrons must walk about 100 yards down a path from the parking lot, Handicapped Parking exists right on the beach. If you arrive with a lot of gear, it is permissible to drive to the handicapped lot, unload your gear (and leave a person to watch it) then go park in the regular parking.

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Lost in translation, Hapuna Beach, Kohala Coast Hawaii: Photo by Donnie MacGowan

To see the new iPhone/iPod Touch App, please visit http://www.tourguidehawaii.com/iphone.html. The best of Tour Guide Hawaii’s free content about traveling to, and exploring, the Big island, can be found here.

For more information on traveling to Hawaii in general and on touring the Big Island in particular, please also visit www.tourguidehawaii.com and www.tourguidehawaii.blogspot.com.
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All media copyright 2010 by Donald B. MacGowan. All rights reserved.

New at iTunes: Hawaii Dream Vacation iPhone/iPod Touch App Puts the Magic of Hawaii in the Palm of Your Hand. Interactive maps, GPS and WiFi enabled, dozens of videos…available at iTunes or www.tourguidehawaii.com.

Playtime at Hapuna Beach, Kohala Coast Hawaii: Graphic from Photo by Donald B MacGowan

by Donald B. MacGowan

New at iTunes: Hawaii Dream Vacation iPhone/iPod Touch App Puts the Magic of Hawaii in the Palm of Your Hand. Interactive maps, GPS and WiFi enabled, dozens of videos…available at iTunes or www.tourguidehawaii.com.

Sunset on Anaeho'omalu Bay, Hawaii: Graphic from Photo by Donnie MacGowan

There are many wondrous, enigmatic and fascinating attractions on the Big Island of Hawaii, some better known than others, many out of the way and generally off the beaten track.  Tour Guide Hawaii has produced an encyclopedic collection of the most up-to-date information, presented as short GPS-cued videos, in an app downloadable to iPhone and iPod Touch that covers the entire Big Island, highlighting the popular and the uncrowded, the famous and the secluded, the adventurous and the relaxing.

Anaeho’omalu Bay, Waikoloa Petroglyphs and Kapalaoa Beach

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Anaeho'omalu Bay, Kohala Coast, Hawaii: Photo by Donnie MacGowan

The most photographed sunset view on the Island of Hawai’i, Anaeho’omalu Bay is the icon of what most visitors envision Hawai’i to be like before they get here…swaying palm trees, a clean beach fronting warm, safe, swimmable ocean and hordes of eager beach boys bearing large, tropical drinks with comical names like “Malahini Wahine Wahoo”. Here at the bay, one can rent snorkel or surfing gear, sign-up for sailing trips, snorkel tours, windsurfing lessons or scuba dives, order food and drinks, or just lounge pleasantly in the niumalu (shade of the coconut palms).

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Early Morning on the Anaeho'omalu Beach isthmus, Kohala Coast, Hawaii: Photo by Donald B MacGowan

Named for the ancient fishponds behind the beach from the words anae (“mullet”) and ho’omalu (“to protect”), Anaeho’omalu Bay is known as “A”-Bay by locals. In addition to swimming, snorkeling, diving, windsurfing and just plain hanging-out, the area around A-Bay is also rich with archeological sites, including section of the Ala Ali’i (King’s Trail), fish ponds, heiau and petroglyphs.

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The Ku'u ali'i Fishpond from the south, Kohala Coast Hawaii: Photo by Donald B MacGowan

Ku’u ali’i (the southern fishpond) and Kahapapa (just to the north) fishponds are actively maintained and there are informational signs all along the paved walkways and trails. Ku’ula pohaku (sacred standing stones honoring Ku’ulakai, god of fishponds, and his wife, Hinapukui’a) and a coral pile made for offerings form the temple area where the kia’i loko, the keepers of the royal fishpond, performed their sacred rituals. There are numerous other archeological sites in the A-Bay vicinity, including a hale noa (dwelling place for a man and his wife) and a mua, or men’s eating-house.

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South of Anaeho'omalu Bay looking North, Kohala Coast, Hawaii: Photo by Donnie MacGowan

Walking the trail south from A-Bay to Kapalaoa Beach will take one along not only shoreline vistas of incomparable beauty and wildness, but also reveal numerous rarely-visited petroglyphs. There is good snorkeling along the farthest south pocket of sand on Kapalaoa Beach. One can follow this trail several miles all the way south to Pueo Bay and Ke-awa-iki Beach along lava flows and shoreline, but it is a long, hot hike with no water for drinking available. For more about Ke-awa-iki Golden Ponds and Pueo Bay, look here.

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Visitor's enjoy the deep shade of the coconut palms, Anaeho'omalu Beach, Kohala Coast Hawaii: Photo by Donnie MacGowan

Walking north along the beach trail (shoes required) over sand, lava and coral, to the Hilton Waikoloa Resort is an unforgettable sunset stroll, and a good introduction to the wild beauty of the Kohala Coast. There are numerous tidepools, a couple with resident Honu, Hawai’ian Green Sea Turtles.

The Wailkoloa Petroglyoh Field is justone of many areas rich in Hawaiian Rock Art, Kohala Coast, Hawaii: Photo by Donnie MacGowan

The Waikoloa Petroglyph Field is just one of many areas rich in Hawaiian Rock Art, Kohala Coast, Hawaii: Photo by Donnie MacGowan

The immense Waikoloa Petroglyph Field lies in the center of the golf course; follow the signs through the King’s Shops. The best time to view the petroglyphs is just after dawn or just before dusk, because the angle of the sunlight accentuates the carvings. Due to their fragility and antiquity, rubbings and casting of the petroglyphs are forbidden. A self-guided tour brochure is available from many locations in the Kings Shops. More information about Hawaiian petroglyphs can be found here.

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The wide arc of Anaeho'omalu Bay from the south, Kohala Coast, Hawaii: Photo by Donald B MacGowan

At the 79 mile marker, turn toward the ocean and follow the Waikoloa Resort road to the intersection just opposite the Kings Shops and before the Hilton Waikoloa; the left turn is clearly marked “Anaeho’omalu Bay”. Turn and proceed to the parking near the restrooms at the end of the road. Restrooms, showers, drinking water, picnic and other facilities and services are available at A-Bay and on the Resort Grounds. There are no lifeguards are on duty.

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Pedal Boats await the arrival of beachgoers at Anaeho'omalu Bay, Kohala Coast, Hawaii: Photo by Donnie MacGowan

To see the new iPhone/iPod Touch App, please visit http://www.tourguidehawaii.com/iphone.html. The best of Tour Guide Hawaii’s free content about traveling to, and exploring, the Big island, can be found here.

For more information on traveling to Hawaii in general and on touring the Big Island in particular, please also visit www.tourguidehawaii.com and www.tourguidehawaii.blogspot.com.
For independent reviews of our product, written by some of our legions of satisfied customers, please check this out.

All media copyright 2009 by Donald B. MacGowan. All rights reserved.

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Canoeists haul out of Anaeho'omalu Bay, Kohala Coast Hawaii: Graphic from Photo by Donald B MacGowan

by Donald B. MacGowan

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Lapakahi State Park, Kohala Coast, Hawaii: Graphic Photo by Donald B MacGowan

There are many wondrous, enigmatic and fascinating attractions on the Big Island of Hawaii, some better known than others, many out of the way and generally off the beaten track.  Tour Guide Hawaii has produced an encyclopedic collection of the most up-to-date information, presented as short GPS-cued videos, in an app downloadable to iPhone and iPod Touch that covers the entire Big Island, highlighting the popular and the uncrowded, the famous and the secluded, the adventurous and the relaxing.

Lapakahi State Historical Park

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Looking over Lapakahi Village, Kohala Coast, Hawaii: Photo by Donnie MacGowan_edited-1

How did the Hawai’ians of olden time survive in such an inhospitable, barren wasteland as Kohala? At Lapakahi (literally “Single ridge”) State Historical Park you can walk through the partially–restored remains of a 600-year old Hawai’ian fishing and farming village, Koai’e. Though the soil is stony and the area is quite windy, the people of Koai’e thrived here into historical times, when they were displaced by grazing cattle.

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Reconstruction of an ancient Hawaiian dwelling at Lapakahi State Park, Kohala Hawaii: Photo by Donnie MacGowan

One must bear in mind that Kohala was not always the barren wasteland seen today. Initially dryland forest, a thousand years ago or more the native Hawai’ians burned the forest to clear farmland for dryland crops such as sweet potato. Primitive farming techniques, overpopulation, erosion from storms, lava flows and lack of irrigation water eventually desertified much of the previously forested coast.

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View to Haleakala from a homesite reconstruction at Lapakahi State Park, Kohala Coast Hawaii: Photo by Donnie MacGowan

With the coming of Europeans, over-grazing by cattle prevented the ecosystem from repairing itself once the native Hawai’ians had deserted it.

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Haleakala on Maui is visible from the shores of Lapakahi State Park, Kohala Coast Hawaii: Photo by Donnie MacGowan

The docents are quite knowledgeable about local history and Hawaiian culture. There is self-guided tour which takes visitors past reconstructed houses, temple ruins and a canoe halau (long house). When park personnel are available, visitors may try spear throwing, ‘ulu maika (disc rolling) and konane (checkers) in the game area.

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Reconstruction of the Lapakahi Village common area, Lapakahi State Park, Kohala Coast Hawaii: Photo by Donald B MacGowan

Stunning views of Haleakala on Maui can be had from the shoreline, and visitors should remember to look for salt-drying pans and small offering shrines to Ku’ula, the god of fishermen along the shoreline.

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Lora and Trogdor at Lapakahi State Park, Kohala Coast Hawaii: Photo by Donald B MacGowan

Contrary to what Park staff may tell you, snorkeling is both permissible and delightful in Koai’e Cove, adjacent to this site. However, respect the ancient sacred sites and graves, and enter the bay only to the right of the rocky spine at the center of the bay. No towels or clothing may be left on the beach, only hat and shoes. Remember there is no water to rinse off with after your swim, and there is no lifeguard. Surf or winds can create treacherous currents, especially in winter.  However, abundant fish, amazing turquoise waters and lots of coral make this one of Kohala’s (and the Island’s) prime snorkel spots when conditions are right. You should not miss it.

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The ruins of Lapakahi Village under threatening skies, Lapakahi State Park, Kohala Coast Hawaii: Photo by Donald B MacGowan

Admission is free, the self-guided tour takes about 45 minutes. Portable toilets, but no water are available. In late 2009, NOAA’s Coastal Estaurine Land Conservation Program awarded the State of Hawaii $1.25 million to purchase 17 acres of privately held land adjoining the southern boundary of the park.

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Overlooking Lapakahi Village, Lapakahi State Park, Kohala Coast, Hawaii: Photo by Donald B MacGowan

To see the new iPhone/iPod Touch App, please visit http://www.tourguidehawaii.com/iphone.html. The best of Tour Guide Hawaii’s free content about traveling to, and exploring, the Big island, can be found here. For more information on traveling to Hawaii in general and on touring the Big Island in particular, please also visit www.tourguidehawaii.com and www.tourguidehawaii.blogspot.com.

For independent reviews of our product, written by some of our legions of satisfied customers, please check this out.

All media copyright 2009 by Donald B. MacGowan. All rights reserved.

New at iTunes: Hawaii Dream Vacation iPhone/iPod Touch App Puts the Magic of Hawaii in the Palm of Your Hand. Interactive maps, GPS and WiFi enabled, dozens of videos…available at iTunes or www.tourguidehawaii.com.

Lora and Trogdor wave goodbye from Lapakahi State Park, Hawaii: Graphic from Photo by Donnie MacGowan

by Donald B. MacGowan

New at iTunes: Hawaii Dream Vacation iPhone/iPod Touch App Puts the Magic of Hawaii in the Palm of Your Hand. Interactive maps, GPS and WiFi enabled, dozens of videos…available at iTunes or www.tourguidehawaii.com.

Hikers on the summit of Mauna Kea look over to Mauna Loa, Hawaii Island: Graphic from Photo by Donnie MacGowan

There are many wondrous, enigmatic and fascinating attractions on the Big Island of Hawaii, some better known than others, many out of the way and generally off the beaten track.  Tour Guide Hawaii has produced an encyclopedic collection of the most up-to-date information, presented as short GPS-cued videos, in an app downloadable to iPhone and iPod Touch that covers the entire Big Island, highlighting the popular and the uncrowded, the famous and the secluded, the adventurous and the relaxing.

Across the Roof of Hawaii

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Astronomical Observatories on Mauna Kea, Hawaii: Photo by Donald B. MacGowan

Recent improvements to the Saddle Road make it no longer the grinding, intimidating drive it once was and open hundreds of square miles of unimaginably beautiful, strange and wondrous landscape to the Hawaii Island Visitor.

Approximate minimum time start to finish (to see every site): 12 hours

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Looking from the Saddle Road to Mauna Kea, Hawaii: Photo by Donnie MacGowan

DIGEST: From Kona take Highway 190 to Highway 200 in 45 minutes of driving. Saddle Road, which cuts between the “saddle” of Mauna Loa on the south and Mauna Kea to the north, passes through ranch lands and the Pohakuloa Military Training Facility, for another 45 minutes, to the turn for Mauna Kea Access Road (John Burns Way). Nearby, Kipuka Huluhulu, or “shaggy hill”, is a 20 minute hike to the top and back. From here it is a 30 minute drive to the Mauna Kea Visitor Information Center. The small village is home to scientists and astronomers that work in the observatories and an amazing place to learn what their research tells us about our universe. Returning to Hwy 200, drive 45 minutes to the amazing Kaumana Cave lava tube, a short hike and a wonderful exploration. A further 30 minutes down Hwy 200 brings one to the outskirts of Hilo and fabulous Rainbow Falls. Continuing into downtown Hilo there there are shops, restaurants, fine museums, gorgeous waterfront beach parks and a fabulous Farmers Market. From Hilo, it is approximately three hours to return to Kailua Kona over Hwy 200; alternately one can take the faster though less scenic Hwy 19 to Waimea and then Hwy 190 into Kailua Kona, about a 2 1/2 hour drive.

Leg 1) In Kailua Kona, start at Ahu’ena Heiau; take Palani Road east to Hwy 190; take Hwy 190 to jct with Hwy 200, The Saddle Road

Ahu’ena Heiau and Kamakahonu Beach

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Ahu'ena Heiau, Kailua Kona, Hawaii: Photo by Donnie MacGowan

Centuries ago the inhabitants of this region built a series of sacred temples, or heiau, along the Kona Coast which were originally used for the purpose of sacrificing human beings to their war god, Kuka’ilimoku.  This particular archeological site is called Ahu’ena Heiau, which in Hawai’ian means “hill of Fire”.

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Sacred carved images at Ahu'ena Heiau, Kailua Kona, Hawaii: Photo by Donald B. MacGowan

Built originally in the 15th century and rededicated by Kamehameha the Great in the early 1800s as the main temple of his capital, the current structures seen at Ahu’ena Heiau were re-built in 1975 under the auspices of the Bishop Museum with financial help from the Hotel King Kamehameha and are constructed to 1/3 the original scale. There are restrooms and showers located on the pier near the beach. Adjacent Old Kailua Town is a treasure of shops, restaurants and aloha.  More detailed information is available about Ahu’ena Heiau, Kamakahonu Beach and Old Kailua Town, historic Mokuaikaua Church and Hulihe’e Palace; a walking tour of Kailua Kona is available here.

Leg 2) Take Hwy 200, The Saddle Road, east to jct with John Burns Way (also called Mauna Kea Access Road).

Saddle Road

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Saddle Road at Kipuka Pu'u Huluhulu, Hawaii Island: Graphic from Photo by Donnie MacGowan

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Saddle Road takes off into the sky at Wai'iki Ranch, Hawaii: Photo by Donald B. MacGowan

Crossing the spectacular saddle between the towering bulk of the volcanoes Mauna Kea and Mauna Loa at about 6600 feet, The Saddle Road runs through brush, grass and forest lands, over lava fields and through some of the wildest and most breath-taking scenery on the Island. From this roadway, four of the 5 principal volcanoes that form The Big Island may be seen: Hualalai, Kohala, Mauna Loa, and Mauna Kea. Because the western half of the road is in notoriously poor condition and consists, in reality, of only one operable lane for much of its descent from the saddle to the Mamalahoa Highway.

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Looking from Saddle Road to Hualalai Volcano, Hawaii: Photo by Donnie MacGowan

However, this road provides the only road access to the Mauna Kea Summit Area and Visitor Information Center, Mauna Kea State Park, Pohakuloa Training Area, Mauna Kea Astronomical Observatory Complex, Waiki’i Ranch and the Kilohana Girl Scout Camp. The Saddle Road also provides the only access to thousands of acres of public forest and open grass lands. Connecting Hilo from about milepost 7.8 on the Hawai’i Belt Road to the Mamalahoa Highway approximately 6 miles south of Waimea, the Saddle Road is widely used by island residents for cross-island travel, despite its somewhat poor condition and undeserved, evil reputation.

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Mauna Loa from Kipuka Pu'u Huluhulu, Hawaii: Graphic from Photo by Donald B MacGowan

The Saddle Road frequently has perfect weather, but also fairly routine are patches of intense rain, fog and high winds. It’s takes about 2 ½ to 3 hours straight driving time, depending upon weather, to make the full traverse from Kailua Kona to Hilo; however, one should be sure to leave time in the schedule to drive up to Mauna Kea Visitor Information Station or hike the Pu’u Huluhulu nature trails.

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Looking from the Saddle Road to Kohala Mountain, Hawaii: Photo by Donald B MacGowan

Along its entire 53 mile length between the turn-off from the highway just 6 miles west of Waimea and where it meets Hawaii Belt Road just north of Hilo, there is no gas and there are no services available; plan accordingly. Some food, water and restrooms may be available at the Mauna Kea Visitor Information Station which is a 30 minute drive up a side road off the Saddle Road about half way.  More information about the Saddle Road is available here.

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Hualalai Volcano from Saddle Road, Hawaii: Photo by Donnie MacGowan

Leg 3) Off a Spur road at the jct of John Burns Way and Hwy 200, on the south side, is Kipuka Huluhulu (“Shaggy Hill”) Nene Sanctuary.

Pu’u Huluhulu Nature Trails/Kipuka Aina Hou

Frequently described as simultaneously the most noticeable and the most overlooked landmark along the Saddle Road, Kipuka Pu’u Huluhulu rises more than 200 feet out of the surrounding lava flows. It’s name meaning “furry hill”, this forested cinder cone has multiple trails winding up through rare native koa trees to breathtaking 360° views of Hualalai, Mauna Kea and Mauna Loa at the top, where you can also wander a meadow of native Hawaiian plants recently reintroduced in this protected natural habitat. By whatever trail, the summit of Kipuka Huluhulu is only about 20 minutes walk from the car.

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Morning light on Kipuka Pu'u Huluhulu, Saddle Road, Hawaii: Photo by Donnie MacGowan

Owing to the encapsulated nature of the kipuka, bird watching here is particularly fabulous; the Ā’akepa, Nene and the Ā’akiapola Ā’au, as well as the Kalij pheasants, pueo, i’o and turkeys are among the rare, endangered or just plain beautiful birds you will see here. The numerous roads and trails through the hundreds of square miles of adjacent lava flows makes for interesting, if hot and dry, mountain biking and hiking.  More information about Kipuka Huluhulu is available here.

Parking and a unisex pit toilet are the only amenities available at Kipuka Pu’u Huluhulu.

Leg 4) Go north on John Burns Way to Mauna Kea Visitor Information Station.

Mauna Kea Visitor Information Station

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The rare, endangered and exotically beautiful Silver Sword plant grows along a nature trail behind the Mauna Kea Visitor's Center: Photo by Donald B. MacGowan

The Visitor Information Station is open daily from 8 a.m. to 5 p.m. During the day there are interactive computer exhibits about Mauna Kea, the observatories and astronomical research, plus there are video presentations and nature trails to hike. Many evenings after dark National Park personnel and astronomers put on public programs and discuss what the latest astronomical findings tell us about the nature of our universe. The souvenir shop has some food items, including hot chocolate, coffee and hot soup, for sale.  More about exploring the Visitor’s Center and the summit of Mauna Kea is available here.

Leg 5) John Burns Way to Mauna Kea Summit

Mauna Kea Summit

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Pu'u Weiku Summit Heaiau and Astronomical Observatories, Mauna Kea Summit, Hawaii: Photo by Donnie MacGowan

Before you decide to go to the summit of Mauna Kea, stop, think, plan. Are you prepared for cold and high altitude? Do you understand the nature and dangers of altitude sickness and UV radiation? Are you experienced at traveling icy dirt roads? Is you car safe for the trip (many car rental agencies on the island forbid you to drive this road)? The Rangers at the Visitor’s center can brief you on altitude sickness, UV radiation preparedness, the condition of the road and all other information you need to decide whether to visit the summit (see a video here).

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From Mauna Kea Summit to Mauna Loa, Hawaii: Photo by Donnie MacGowan

The summit of Mauna Kea is truly an amazing place. Beautiful, awe-inspiring, 360 degree views of the entire Big Island, the summit is also culturally and religiously important to the native Hawai’ians and is home to several, world-class astronomical observatories and their support buildings. Because of the extremity of the altitude and the poor quality of the road above the Visitor’s Center, it is advised that extreme caution be exercised in deciding to visit Mauna Kea’s Summit. From the road’s end very near the summit, a short, 10 minute trail leads up Pu’u Weiku cinder cone to the actual mountain top and a Hawaiian religious shrine. Also near the summit is the 1-mile hike to Lake Waiau, the 7th highest lake in the US, as well as numerous archeological sites. Moving at altitude is strenuous, so conserve energy. Do not over-tax yourself, be sure to drink plenty of fluids and protect yourself from the sun, wind and cold. Leave the summit area and return to the paved road long before you are tired.  More very important details about visiting the summit of Mauna Kea are available here.  Some ruminations on the Hawaiian Snow Goddess, Poliahu, and personal reflections about the summit of Mauna Kea can be found here.

Leg 6) Return John Burns Way to Hwy 200; take Hwy 200 east to Kaumana Caves

Kaumana Caves

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Looking Kaumana Cave, on the outskirts of Hilo Town, Hawaii: Photo by Donnie MacGowan

A skylight opening to 25-mile long Kaumana Cave is located at the county park near the 4-mile marker on the Hilo side of the Saddle Road. Concrete stairs take you down through the rain forest jungle to the bottom of a collapse pit forming two entrances to the cave. Most people are drawn to the entrance on the right, a large, opening leading to cavernous rooms. In this entrance, graffiti from hundreds of years ago to the present is preserved, scratched into the rocks. The entrance on the left, however, is more interesting, leading through squeezes and low spots to numerous rooms with fascinating speleo-architecture and cave formations. Both caves go to true dark in fewer than 300 feet in either direction. There are more than 2 miles of easily accessible, wild cave to explore here, but if you intend more than just a cursory inspection near the entrances, bring a hard hat, water and at least 3 sources of light. A quick tour of the caves takes fewer than 20 minutes.

Parking for the caves is located across the highway from the park; extreme care should be taken when crossing he road. Public restrooms, water and picnic tables are available at the park. As you approach Hilo from Kaumana Caves, Hwy 200 becomes variously called Kaumana Drive, then Waianuenue Avenue.  More about Kaumana Cave is available here.

Leg 7) Take Hwy 200 into Hilo Town. At the intersection of Kaumana Drive (Hwy 200) and Lele Street, turn left and go 1 block to Waianuenue Ave; go left on Waianuenue a short distance to the entrance to Rainbow Falls and Wailuku River Park

Rainbow Falls

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Rainbow Falls, Hilo Hawaii: Photo by Donnie MacGowan

The subject of recent and ancient legend, Rainbow Falls is the lovely emblem of Hilo town. The characteristic wishbone shape of Rainbow Falls is best seen at moderate river flows…too little water and only a single drizzle remains, too much runoff and the falls merge into a single, roaring flume. At any time, however, it’s a beautiful place and worthwhile to visit. The rainbows within the falls are best seen in the mid to late morning. Follow the trail to the left along the river bank to delightful swimming and wandering; please note, however, that swimming in rivers and near falling water is dangerous. Don’t go in if the current is swift or if recent rains have swollen the river.

Restrooms are by the parking lot and a souvenir shop is located across the street. For more information on Rainbow Falls and the Wailuku River Park, please go here.

Leg 8) Take on right on waianuenue Ave exiting Rainbow Falls and follow it into downtown Hilo Town.

Hilo Town

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Hilo's east side is famous for it's numerous, lovely, if tiny, beach parks, Leiiwi Beach, Hilo Hawaii: Photo by Donnie MacGowan

Beautiful but wet, metropolitan but decrepit, bustling but laid back, Hilo is a lovely, maddening, heartbreaking, addictive study in contrasts. In can rain all day long for 50 days in a row, yet when the sun does shine, the views of Mauna Loa and Mauna Kea from the Liliuokalani Gardens, or of Hilo Bay as you drive down from the mountains, or the rain-forest and waterfall choked gulches with lovely beaches along the highway north of town, make Hilo one of the most truly, achingly-lovely spots on earth.

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Liliuokalani Gardens, Hilo Hawaii: Photo by Donnie MacGowan

More laid back and sleepier than bustling Kailua Kona, Hilo is the largest town on the island, and the county seat. The Imiloa Astronomy Center of Hawaii, Tsunami Museum, Lyman House Missionary Museum and the Panaewa Rainforest Zoo are all wonderful places to learn about various aspects of Hawaii. There are numerous shopping districts, two large malls and the Historic Old Hilo downtown shops to browse through, a variety of sprawling green parks, a fabulous tropical arboretum right downtown and a mile-long black-sand beach fronting the bay to explore. Hilo’s Farmer’s Market is a “must see” for any visitor who is spending time on this side of the island. A more complete tour of Hilo Town is available here; a darker vision of Hilo is available here.

Leg 9) Take Highway 19 north out of Hilo along the Hamakua Coast to Waimea.  At Waimea, get on Highway 190 and follow it west to Kailua Kona.

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Looking toward Waimea from the Waikoloa Road, Hawaii: Photo by Donald B MacGowan

This return route is safer and easier to drive in the afternoon and at night, and routes you through fabulous, scenic Waimea Town, where there are interesting shops, fabulous restaurants and gasoline available late into the night.  More about Waimea can be found here.

New at iTunes: Hawaii Dream Vacation iPhone/iPod Touch App Puts the Magic of Hawaii in the Palm of Your Hand. Interactive maps, GPS and WiFi enabled, dozens of videos…available at iTunes or www.tourguidehawaii.com.

Mauna Kea Full Moon, Hawaii: Photo by Donald B MacGowan

To see the new iPhone/iPod Touch App, please visit http://www.tourguidehawaii.com/iphone.html. The best of Tour Guide Hawaii’s free content about traveling to, and exploring, the Big island, can be found here. For more information on traveling to Hawaii in general and on touring the Big Island in particular, please also visit www.tourguidehawaii.com and www.tourguidehawaii.blogspot.com.

New at iTunes: Hawaii Dream Vacation iPhone/iPod Touch App Puts the Magic of Hawaii in the Palm of Your Hand. Interactive maps, GPS and WiFi enabled, dozens of videos…available at iTunes or www.tourguidehawaii.com.

Hualalai Sunset on Highway 190, Mauna Loa-Mauna Kea Saddle area, Hawaii: Photo by Donnie MacGowan

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New at iTunes: Hawaii Dream Vacation iPhone/iPod Touch App Puts the Magic of Hawaii in the Palm of Your Hand. Interactive maps, GPS and WiFi enabled, dozens of videos…available at iTunes or www.tourguidehawaii.com.

Kamehameha Statue, Wailoa Park, Hilo Hawaii: Graphic from Photo by Donnie MacGowan

by Donald B. MacGowan

New at iTunes: Hawaii Dream Vacation iPhone/iPod Touch App Puts the Magic of Hawaii in the Palm of Your Hand, available at iTunes or www.tourguidehawaii.com.

Kolekole Beach Park: Graphic from Photo by Donnie MacGowan

There are many wondrous, enigmatic and fascinating attractions on the Big Island of Hawaii, some better known than others, many out of the way and generally off the beaten track.  Tour Guide Hawaii has produced an encyclopedic collection of the most up-to-date information, presented as short GPS-cued videos, in an app downloadable to iPhone and iPod Touch that covers the entire Big Island, highlighting the popular and the uncrowded, the famous and the secluded, the adventurous and the relaxing.

Kolekole Beach Park

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Stormy surf at Kolekole Beach, Hilo Hawaii: Photo by Donnie MacGowan

Surprising, wild, lovely, peaceful Kolekole Beach Park is the jungle gem of the Hamakua Coast beach parks. The river you saw magnificently jumping with such abandon off the cliff at Akaka Falls ends its journey to the sea by sluicing down through this Koa and palm tree filled gulch and smashing into the surf at Kolekole Beach Park. Neatly hemmed on three sides by dense jungle canyon, Kolekole features lawns, picnic facilities, and a water-fall festooned swimming hole, all leading the visitor to the pounding, cobble beach in the furious surf.

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The rope swing over the falls and lovely swimming hole are popular with everybody, Kolekole Beach Park, Hilo Hawaii: Photo by Donnie MacGowan

Kolekole Beach park is located just north of mile marker 14 on Highway 19; the narrow access road turns sharply uphill just before the massive bridge over Kolekole Gulch. Kolekole means “raw” or “scarred” in Hawaiian suggestive of the raw gash of Kolekole Gulch, but the term has come to mean “talk story” in pidgin and that is what locals come here to do, “talk story” with friends and family as the fish, surf, barbecue and relax.

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Kolekole Jungle from the Old Mamalahoa Highway, Hilo Hawaii: Photo by Donald B MacGowan

The lovely, jungle-draped access road tumbles down the steep slopes of Kolekole Gulch to the side of Kolekole Stream, which rises at about 8000 feet on eastern slope of Mauna Kea, flows over Akaka Falls and then down to Kolekole Beach. In addition to the koa trees, varieties of palm, banana, fern and liana vine and lots of orchids can be found along this road, growing down to the river. A remnant of the Old Mamalahoa Highway turns off from the access road at the bridge over Kolekole Stream, and runs through the incredible jungle all the way to Hakalau Gulch. This section of road used to be a very scenic drive until the earthquake of 2006 rattled the depression-era bridges.

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Highway 19 Overpass at Kolekole Beach Park, Hilo Hawaii: Photo by Donald B MacGowan

That huge, 100 foot high bridge that spans Kolekole Gulch, running over the park at the mouth of the stream, was originally built by the Hawai’i Consolidated Railway Company as a railway bridge. Debris from major damage to the bridge by the tsunami of 1946 are visible underneath, even today. Damage to this, and the other bridges up and down the Hamakua Coast forced the closure of the railroad line. The bridges had been repaired and rebuilt for automobiles by 1949, opening the connection between Honoka’a and Hilo once again.

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The wild surf at Kolekole Beach is generally too rough to swim in, Hilo Hawaii: Photo by Donnie MacGowan

Although locals surf and swim unconcernedly here, the visitor is advised to admire the water, but not go in. Not only are the currents and tides lethally treacherous here, but stream mouths and murky water are prime hunting grounds of Hawai’i’s own tiger, Mano, the shark. Remember that most all Hawai’i streams are infected with leptospirosis and giardia; do not drink from the streams, do not allow stream water to get into your mouth and do no attempt swimming in the stream if you have any open cuts or scratches.

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Kolekole River from the road, Hilo Hawaii: Photo by Donnie MacGowan

Facilities at Kolekole Beach Park include picnic pavilions and tables, pit barbecues, showers, restrooms. There is no drinking water at the park; remember to bring your own. Camping is available by permit only; details are available here.  The park can be crowded on weekends but is generally deserted during the week.

New at iTunes: Hawaii Dream Vacation iPhone/iPod Touch App Puts the Magic of Hawaii in the Palm of Your Hand, available at iTunes or www.tourguidehawaii.com.

Picnic Grounds at Kolekole Beach Park, Hilo Hawaii: Photo by Donnie MacGowan

To see the new iPhone/iPod Touch App, please visit http://www.tourguidehawaii.com/iphone.html. The best of Tour Guide Hawaii’s free content about traveling to, and exploring, the Big island, can be found here. For more information on traveling to Hawaii in general and on touring the Big Island in particular, please also visit www.tourguidehawaii.com and www.tourguidehawaii.blogspot.com.

New at iTunes: Hawaii Dream Vacation iPhone/iPod Touch App Puts the Magic of Hawaii in the Palm of Your Hand, available at iTunes or www.tourguidehawaii.com.

The Old Mamalahoa Highway Crosses over Kolekole River, Hilo Hawaii: Photo by Donald B MacGowan

For independent reviews of our product, written by some of our legions of satisfied customers, please check this out.

All media copyright 2009 by Donald B. MacGowan. All rights reserved.

New at iTunes: Hawaii Dream Vacation iPhone/iPod Touch App Puts the Magic of Hawaii in the Palm of Your Hand, available at iTunes or www.tourguidehawaii.com.

Everett Maynard at Kolekole Beach, Hilo Hawaii: Graphic from Photo by Donnie MacGowan

by Donald B. MacGowan

New at iTunes: Hawaii Dream Vacation iPhone/iPod Touch App Puts the Magic of Hawaii in the Palm of Your Hand, available at iTunes or www.tourguidehawaii.com.

Lava enters the sea at Waikupanaha: Graphic From Photo by Donnie MacGowan_edited-1

There are many wondrous, enigmatic and fascinating attractions on the Big Island of Hawaii, some better known than others, many out of the way and generally off the beaten track.  Tour Guide Hawaii has produced an encyclopedic collection of the most up-to-date information, presented as short GPS-cued videos, in an app downloadable to iPhone and iPod Touch that covers the entire Big Island, highlighting the popular and the uncrowded, the famous and the secluded, the adventurous and the relaxing.

Trip 5: Hawaii Volcanoes National Park and Lava Viewing Approximate minimum time start to finish (to see every site): 14 hours (return drive in the dark).

New at iTunes: Hawaii Dream Vacation iPhone/iPod Touch App Puts the Magic of Hawaii in the Palm of Your Hand, available at iTunes or www.tourguidehawaii.com.

Many natural hot springs surround Ahalanui Hot Pond at Pu'ala'a County Park in Puna Hawaii: Photo by Donald B MacGowan

From Kona, connect to Highway 11 south 2 1/2 hours to Ka’u Desert Trail. A 40 minute round trip hike leads to footprints of ancient warriors who where caught in a sudden, ferocious eruption. Continue on Highway 11 to Hawai’i Volcanoes National Park. Park Rangers at the Visitor Center will have the latest lava information. Chain of Craters Road has numerous craters, tons of hiking trails and several breathtaking vistas for great photographs. Upon exiting the Park, continue through Puna to Kea’au and Highway 130 (food stop). Proceed to Pahoa and the junction to Highway 132 and Lava Trees State Park. Here trees were inundated with fast flowing lava. When the trees rotted, it left these Lava Trees. Then on to Highway 137, following the coast past Ahalanui Hot Spring to Kalapana and a 20 minute hike to the lava viewing area at Waikupanaha. (Arrive about dusk for optimal viewing.) From Kalapana back to Kona is a 3 1/2 hour drive (after dark).

Leg 1) Start at north end of Keauhou Historic District on Ali’i Drive, head south on Ali’i Drive to jct with Kamehameha II Hwy; east on Kamehameha III to Hwy 11. Take Hwy 11 south to Ka’u Desert/Warrior Footprints Trail.

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Vog-Tinged Sunset at the Reconstructed Hapaiali'i Heiau, Keauhou Historic District, Kona Hawaii: Photo by Donnie MacGowan

Keauhou Historic District and Kona Coffee

For almost 400 years, temples and palaces along the Kona coastline served as a kind of “Rome of the Pacific”, a great political, religious and cultural center in Polynesia, until the capital was moved to Honolulu in 1850 by Kamehameha III.

The most important, interesting and best preserved historical and cultural sites lie within the Keauhou Historic District, between Kahalu’u Beach Park in Kailua running south 6 miles to Kuamo’o Bay in Keauhou. The District contains perhaps a dozen fascinating sites that are easy to walk to, well maintained and quite interesting. To see the numerous fascinating and important archaeological sites in the Keauhou Historic District, it is necessary to park your car in the free parking at either Kahalu’u Beach Park or the Keauhou Beach Resort and explore on foot.

Just uphill from the Historic District is the Kona Coffee District. Hawaii is the only state in the union which produces coffee, and Kona coffee is perhaps the finest in the world. Over 2 millions pounds of coffee a year are produced on about 600, 2-3 acre farms; tours of coffee farms and roasteries are available.  More about Kona Coffee can be found here.

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Frank Burgess hiking on the Ka'u Desert Trail, Hawaii Volcanoes National Park: Photo by Donnie MacGowan

Ka’u Desert Trail and Warrior Footprints, Hawai’i Volcanoes National Park

Just where Hawai’i Belt Road enters Hawaii Volcanoes National Park from the West, is a small parking strip that is the gateway to a host of wonders within the Ka’u Desert section of Hawaii Volcanoes National Park. Although eruptions here are generally characterized by leisurely outpouring of lava, it is not unknown for Kilauea to violently erupt in a blast of steam and ash. It is this ash that preserves some human footprints, believed to have been formed in 1790 when enemies of Kamehameha the Great were caught by one such massive, explosive eruption. Perhaps as many as 400 men died in this eruption. An emergency phone is available here; there are no other services. Do not venture from your car here without carrying water. More about the Warrior Footprints and the hike can be found here.

Leg 2) Continue south on Hwy 11 to Hawaii Volcanoes National Park Entrance and jct with Crater Rim Drive; Crater Rim Drive west to Kilauea Visitor’s Center to Jagger Museum, then back around Crater Rim Drive to Kilauea Iki Crater.

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Kilauea Crater and Eruption at Halema'uma'u, Hawaii Volcanoes National Park: Photo by Donnie MacGowan

Hawai’i Volcanoes National Park

Hawai’i Volcanoes National Park is a magical, spiritual, wondrous, strange and beautiful place comprised of great contrasts and contradictions: dry as dust desert to teeming tropical jungle; frigid sub-arctic wasteland to steaming black sand beaches to rivers of flowing lava.

The star attractions in the Park are a pair of active volcanoes; Mauna Loa is the largest mountain on earth and Kilauea is most active volcano on earth. However, there are numerous other wonders from lava tubes to crawl down, black sand beaches with sea turtles to watch, mysterious petroglyph fields to explore, tropical jungles to hike through, endangered bird species to find, happy-face spiders to amuse and an otherworldly volcanic landscape so fresh it’s still steaming.

Hawaii Volcanoes National Park is open 24 hours a day, 365 days a year. During daylight hours, an access fee is charged. The Visitor Center has a 24-hour information line at 808.985.7017 and there is a 24-hour eruption hotline at 808.985.6000. Within the Park tune to A.M. radio 530 for continuous information broadcast. There tourist items available for sale and one restaurant and in the park, however generally shopping, restaurants and gasoline are only available in the nearby village of Volcano.

Kilauea Visitor Center

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Fran Burgess peruses Kilauea Visitor's Center Book Shop at Hawaii Volcanoes National Park: Photo by Donnie MacGowan

Newly remodeled and updated, the Kilauea Visitor’s Center is an outstanding resource of information on Hawaii’s volcanoes and the National Park; the not-to-be-missed first stop in the park you must make. The Center is run by enthusiastic and knowledgeable staff that has the most up-to-date information on viewing the eruption, hiking and camping, bird watching, stargazing and just about any other topic of interest to Park visitors.

Available for sale in the Center are maps, guidebooks, books and videos about the volcanoes, Hawai’iana, history, plants and every topic you can imagine pertinent to the Park, even souvenirs. There are free brochures and pamphlets on various trails, attractions, hiking safety and lava viewing hazards and precautions. The Visitor Center is open daily from 7:45 a.m. to 5 p.m.; there are public restrooms, water and pay phones available. Starting at 9 a.m. and showing every hour on the hour is a 20 minute informative movie about the Park; the film changes from time to time, but always contains spectacular footage of eruptions, information on volcanology and the natural and human history of the Park.

Jagger Museum and Hawai’i Volcano Observatory

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The Eruption at Halema'uma'u Crater, as seen from the Jagger Museum, glows sickedly at night, as if someone had left the door to Hades propped ajar...Hawaii Volcanoes National Park: Photo by Donnie MacGowan

Famed for its fabulous views of Mauna Loa and Kilauea as much as for its interesting exhibits, The Jagger Museum (named for geologist Thomas A. Jagger) is open daily from 8:30a.m. to 5:00p.m. Exhibits include murals by Herb Kawainui Kane, seismograph charts of eruptions and earthquakes, geological displays and display about the natural and human history of the Park.

When entering the parking lot of the Museum/Observatory, be especially careful of the Federally-protected Hawaii Goose, the Nene, who seem to congregate here. The Nene is the State Bird of Hawai’i, and this parking lot and its surrounding area constitute one of the best places for viewing them.

Kilauea Iki Trail

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Looking from the rim down on hikers in the crater on Kilauea Iki Trail, Hawaii Volcanoes National Park: Photo by Donnie MacGowan

Perhaps the finest short day hike in the park, a four-mile, 2-3 hour trip down into, across and back out of Kilauea Iki Crater gives one an intimate feel for volcanoes, Hawaiian-Style. Along one side, thick fern and ohi’a forest skirts along the rim and on the other, lush tropical rainforest crowds to the very brink of the crater; bleak volcanic desert lines the crater walls and covers the floor. The start and finish of the hike are along well marked, wide trails. The remainder is an easily followed, well marked trail with stone ahu (cairns) over the crater floor. As always when hiking in the Park, it is wise to avoid the noonday sun, and to remember that afternoon showers are common, especially near where this hike meets the crater rim. More about hiking the Kilauea Iki Trail can be found here.

Leg 3) Crater Rim Drive to intersection with Chain of Craters Road; Chain of Craters Road to End of Road.

End of Chain of Craters Road

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Most years, it is possible to hike to see flowing lava from the end of Chain of Craters Road in Hawaii Volcanoes National Park: Photo by Donnie MacGowan

The end of Chain of Craters Road is currently at the 19 mile marker near the Holei Sea Arch. This is where the road was cut off by flowing lava and destroyed the 2 million dollar visitor center. When the lava is near the road, one can walk right up to it. There are displays about the volcano and natural history of the area, as well as a wealth of information on hiking to, and viewing, the lava, available here.

Hiking all the way out to the active flows is one of the most spiritually rewarding, awe-inspiring, curiosity quenching and amazing things one can do anywhere in the world—but it is neither for the physically unfit nor the meek of spirit. It is a long, hot hike (currently seven miles) over broken ground and glass-sharp rocks; the heat from the volcano is savage; the weather, if clear, is sweltering…frequent squalls blow in off the ocean and the rain and wind can get pretty wild out on the lava plain where there is absolutely no cover or shelter to protect you. No water or shade is available anywhere along the hike.

Leg 4) Follow Chain of Craters Road back uphill to Crater Rim Drive, follow Crater Rim Drive back to Park Entrance and then to Hwy 11. Go east on Hwy 11 to jct with Hwy 130 at Kea’au; take Hwy 130 south to Pahoa.

Puna District and Pahoa Town

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Remember...Puna is wet! The Malama Market sign is reflected in a rain puddle in downtown Pahoa, Puna Hawaii: Photo by Donald B MacGowan

Uncrowded, off the beaten track and largely undiscovered by tourists, Puna District is a magnificent wonderland; from incredible tree-tunneled roads, geothermal fields of steam vents, lovely beach parks, hot ponds, hikes on raw lava flows and jungle trails, and unequaled snorkeling, the land cries out for the visitor to explore a little bit.

At the center of Puna is Pahoa Town; wild, untamed and even a bit unruly, with its false-front, western-style buildings and raised wooden sidewalks, Pahoa looks more like it belongs in Wyoming. But Wild West isn’t the only subculture evident here…tie-dye banners and the general “flower-power” ambiance some businesses and citizens lend Pahoa give it a decidedly “’60’s” feel.

It has been said of Pahoa that if it weren’t for counter-cultural influences, it would have no cultural influences at all. The charm and allure of this way of living is evident when you consider that the region around Pahoa is the fastest growing portion of the island. Pahoa has some of the best restaurants on the island, THE best natural foods store and a great public pool.

Remember that the return leg of this trip to Kona will be made at night .  There is no food or gas available between Kea’au in Puna and Kailua Kona, so be sure to fill-up the tank and buy plenty of food while you can.

Leg 5) At Pahoa, get on Hwy 132 to Lava Trees State Park.

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A lava cast of an ohi'a tree at Lava Trees State Monument in Puna, Hawaii: Photo by Donnie MacGowan

Lava Trees State Monument

Under a lacy canopy of monkeypod trees, casts of ohi’a trees stand as monuments to a fast-moving pahoehoe lava flow that passed through here in 1790. When the lava hit the water-saturated ohi’a trees, it cooled and began to congeal around them. The original ohi’a trees burned away but the quickly cooled lava around them stands here today, hollow, with imprints of the tree bark inside. Lava Trees Park offers trails to hike and a restful, bird-filled jungle to sit and listen to. You can spend between 20 minutes to an hour wandering the trails, here, exploring and discovering. Be careful, however, the area is riddled with hidden cracks in the ground which can make exploring hazardous. You may wish to avail yourself of the restrooms here; they are the last public facilities for some distance. You can find more about the Lava Trees Monument and the famous, lacy, canopied roads of Puna here and here, respectively.

Leg 6) From lava Trees State Park take Hwy 132 to jct with Hwy 137 at Kapoho; take Hwy 137 southwest to Ahalanui Pond then to Kaimu Black Sand Beach and Kalapana Disaster of 1990.

Ahalanui Pond

Also called “Secrets Beach”, this spring and ocean-fed, man-made pool was initially constructed when the springs ran chilly cold. Eruptions in Puna during the ‘50s and 60’s reworked the subterranean waterworks and now the springs run hot and the pool is a comfortably warm 90-95 degrees. The open connection to the ocean, keeps the water fresh. With the gentle aloha breezes, swaying palms and surf whooshing against the, it can be really hard to drag oneself out. Soak for a while. Picnic tables, pavilions, pit barbecues, showers, lawns and all the pleasantries of a civilized park are available at Ahalanui Pond. Leave no valuables in your car and be vigilant if you stay soaking here, after dark.  There is more about Ahalanui Hot Spring and pool here.  You can find information about nearby Issac Hale Beach Park and Pohoiki Bay here.

https://lovingthebigisland.wordpress.com/2010/01/03/discovering-puna-explore-isaac-hale-beach-park-at-pohoiki-bay-puna-hawaii/

The Big ISland's newest Black Sand Beach, Kaimu Beach, at Kalapana, Puna Hawaii: Photo by Donnie MacGowan

Kalapana Disaster of 1990/Kaimu Black Sand Beach

In 1990 the volcano goddess Pele determined it was time for some serious housecleaning in Puna. Lava flows from Kilauea’s East Rift engulfed the villages of Royal Gardens, Kaimu and Kalapana, destroying virtually everything.

Buried were a centuries old fishing village and a world famous black sand beach. When the lava came, it wiped out not just material possessions; it wiped out a way of life and a landscape cherished by generations. The Big Island’s newest black sand beach, Kaimu Beach, is a lovely if barren crescent of sand at the end of an unforgiving expanse of lava from the 1990 flows. The trail to the new black sand beach is marked with hundreds of young palms, numerous lava casts which include palms, pandanus fruit and even some fish that were caught in tide pools.

From the lava hillocks along the trail you can get nice views of the eruption plume at Pu’u O’o, up on the flank of Kilauea, as well as the steam clouds down a few miles along the coast where the lava enters the sea. Restrooms and fast food are available at the end of the road. More about Kalapana and Kaimu Black Sand Beach can be found here.

Leg 7) From Kalapana, take Hwy130 (Ahia Road) just a tweak to the jct with old HWY 130; go west on old the highway to Waikupanaha Lava Viewing.

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Streaming lava at Waikupanaha, Puna Hawaii: Photo by Donnie MacGowan

Lava Viewing Near Kalapana

Nowhere else can you see lava flowing from a volcano into the sea; no Big Island visit is complete without seeing this awe-inspiring show. Currently lava is only flowing into the sea outside the Park. Drive south on Highway 130 through Pahoa to the 20 mile marker and take the right branch about two miles to the parking area. Port-a-potties are available here. The road is open from 2 p.m. until 10; no cars allowed in after 8. Lava viewing information is available from Hawaii County at 808.961.8093; check conditions before you go.

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Littoral explosion plume at Waikupanaha lava ocean entry, Puna Hawaii: Photo by Donnie MacGowan

The easy trail, a 20 minute stroll to the viewing area, is well-marked. The viewing varies as lava flows nearer or farther from the trail. Viewing is best at dusk so bring flashlights for the hike out. Take close-toed walking shoes and a hat, long pants and long-sleeved shirt, at least 2 liters of water and sun block and a rain jacket and camera. Remember food and gas are not available anywhere nearby after dark, so fill up BEFORE you park, bring snacks and drinks. There are port-a-potties available at the parking lot.  Much more about lava viewing at Waikupanaha can be found here.

Leg 8) Return to Hwy 130; Hwy 130 north through Pahoa to Kea’au and jct with Hwy 11. Hwy 11 west to Kailua Kona. Take Hwy 11 west to Kailua Kona.

Remember that this leg of the journey takes about 3 1/2 hours, you will be driving it in the dark and there is nothing in the way of gas or food available between Kea’au and Kailua Kona at night.  If you find yourself low on gas and hungry at the end of the trip, the best bet is to drive into Hilo (about 1/3 hour away through Pahoa, get gas and eat there, then drive back to Kailua Kona on Highway 19 through Waimea.

New at iTunes: Hawaii Dream Vacation iPhone/iPod Touch App Puts the Magic of Hawaii in the Palm of Your Hand, available at iTunes or www.tourguidehawaii.com.

Waikupanaha ocean entry, Puna Hawaii: Photo by Donnie MacGowan

To see the new iPhone/iPod Touch App, please visit http://www.tourguidehawaii.com/iphone.html. The best of Tour Guide Hawaii’s free content about traveling to, and exploring, the Big island, can be found here. For more information on traveling to Hawaii in general and on touring the Big Island in particular, please also visit www.tourguidehawaii.com and www.tourguidehawaii.blogspot.com.

New at iTunes: Hawaii Dream Vacation iPhone/iPod Touch App Puts the Magic of Hawaii in the Palm of Your Hand, available at iTunes or www.tourguidehawaii.com.

Lae`apukii Ocean Entry Lava Flow Hawaii Volcanoes National Park: Photo by Donald B MacGowan

For independent reviews of our product, written by some of our legions of satisfied customers, please check this out.

All media copyright 2009 by Donald B. MacGowan. All rights reserved.

New at iTunes: Hawaii Dream Vacation iPhone/iPod Touch App Puts the Magic of Hawaii in the Palm of Your Hand, available at iTunes or www.tourguidehawaii.com.

Helicopter and Explosion Plume, Lava Ocean Entry at Waikupanaha, Puna Hawaii: Photo by Donnie MacGowan