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Geology of the Hawaiian Islands

Story of the origins, presents state and the future of Hawaii

by Marcin Smok


haleakala crater

The Hawaiian archipelago is a very unique landmass on Earth. A magnet for geologists, volcanologists, botanists and countless other scientists, this chain of volcanic islands has always been a place of wonder, an unanswered question in the history of our planet. Discoveries made here helped us understand the geological processes that shaped Earth and continue to do so, influencing our very existence and reminding us that humanity's rule over the globe is nothing but temporary, a short chapter in the story of the blue planet.

To understand how Hawaiian Islands commenced to exist is to learn about the land forming mechanism our planet implements from the dawn of time, the most fundamental and violent of all Earth's forces- the power of a volcano erupting unimaginably hot lava from the depths of planet's liquid interior. Before we go back in time to when Hawaiian island were still forming, let's fast forward to present day and summarize what we know about them from one quick glimpse at the map...

  Satellite composition of the Hawaiian island chain. by  NASA/Goddard Space Flight Center  

Satellite composition of the Hawaiian island chain. by NASA/Goddard Space Flight Center  

Hawaii is a chain of volcanic islands situated in the middle of the Pacific Ocean, the most isolated archipelago on Earth that remained untouched by humans for thousands of years, discovered only a mere millennium and a half ago by mighty Polynesian sailors searching for a new place to expand their civilization. The closest landmass is Kiritimati atoll, at over 1300 miles to the south, while the nearest continent lays 2400 miles away, in today's state of California. The island chain consists of eight major islands- at its northernmost tip lays Ni'ihau and Kauai, then O'ahu with the state's capitol Honolulu, followed by the group of four islands- Maui, Lānaʻi, Moloka’i and the uninhabited Kaho'olawe in the center of the chain and finally, at its southern end, the largest and youngest- the island of Hawai'i, commonly known as the Big Island. Each of the eight tropical islands is different from another in terms of geological features, climate zones and volcanic activity. When scientists first discovered the uniqueness of each individual island in the chain, they ultimately knew Hawaii would be a perfect place to study the Earth's origins. What they've learned through decades of observations and by collecting and analyzing scientific data revolutionized Earth sciences and laid foundation for a number of fundamental theories, like plate tectonics, hot spot and mantle plumes, which I will talk about in details later in the article.

Hawai'i always played the role of the most intriguing to scientist island in the chain, simply because it has something other islands lack- an erupting volcano (es). The enormous Mauna Loa erupted in regular intervals for more than 200 years (the last documented eruption occurred in 1780), with latest taking place in 1984, meanwhile Big Island's youngest volcano, Kilauea, spills lava continuously since its formation, which is estimated to be between 300,000 to 600,000 years ago!!! The latest lava flow from Kilauea's vent Pu'u 'O'o started in 1983 and continues to this day.

The enormous Mauna Loa volcano as seen from the slopes of Mauna Kea.

Scientists in the 19th and early 20th century tried to answer questions of the volcano's role in island building and the origins of lava that surfaced in this remote location. The breakthrough came with an invention of gravimeter by a Dutch geophysicist and geodesist Felix Andries Vening Meinesz. His ingenious apparatus allowed for precise measurement of Earth's gravitational forces, which in turn enabled to determine a given landmass’s size. He took his device to the Big Island and his calculations shocked the scientific community- what was visible above the ocean surface was only a tip of an enormous, incredibly massive mountain- when measured from the ocean floor, Hawai'i tallest peak, Mauna Kea summit, reach 33,100 ft. (10,100 m) in height, making it the tallest mountain on Earth (almost twice the size of Mount Everest in the Himalayas). Besides that, Mauna Loa, Hawai'i second largest volcano, is so massive it bends the Earth's crust towards the mantle. The numbers are so large it is beyond imagination how much lava flew from planet's interior to form the island. To give a point of reference, geologists found a method to measure the amount of lava that is currently produced by Kilauea and the amount is staggering- as much as 100 million cubic yards (around 76,500,000 cubic meters or 76.5 billion liters) of liquid rock surfaces on Big Island every year. According to my calculations, that would be 640 gallons (2423 liters) of glowing red lava per second!!! Some of it flows on the surface, but majority gets to its final destination- the ocean- through a "volcano plumbing system", a system of underground tunnels called lava tubes. A lava tube forms when a top layer of surface flowing lava hardens and forms a thick, solid cap that enables the still liquid lava beneath to travel larger distances without cooling down. A great example of a lava tube accessible to explore is Thurston Lava Tube in Volcanoes National Park on the island of Hawai'i.

Lava from Kilauea volcano By Hawaii Volcano Observatory (DAS) [Public domain]

Flowing lava is an extremely powerful natural occurrence, a liquid fire swallowing everything on its path and leaving a permanent scar in the surrounding landscape. However powerful it might be, Kilauea volcano's lava meets its match when the land ends- a fierce battle of fire and water always ends with the same outcome -from a cloud of water vapor and toxic mix of carbon dioxide, sulfur dioxide, hydrogen sulfide and other gases, a new land emerges. Solidified lava forms a new patch of island, just like it did for eons of time before. Just to give you a perspective of how amazing the land-forming ability lava possess, for the last 20 years eruption from Kilauea vent Pu'u 'O'o created 540 acres (219 hectares) of new ground. That would be a little over 408 American football fields of knife sharp, jet black rock.

Seeing a river of lava entering the ocean with her/his own eyes, a person would assume that this process is the sole source of the formation of Big Island. Scientists, using a method of calculating lava rocks' age called radiocarbon dating, found out that the island of Hawai'i is about 400,000 years old. That might be long in our lifetime perspective, but in geological history, Big Island is a "newborn baby". The five volcanoes- the active Kilauea and Mauna Loa, dormant Mauna Kea and Hualālai, as well as extinct Kohala- make up what today is the biggest island in the chain (it is so large all the other major Hawaiian Island could fit into it and there still would be some room to spare).

When people realized the island of Hawai’i is essentially one huge lava field with volcanoes looming over the landscape, they've compared this knowledge to other islands in the archipelago. Each of the 8 major island yield evidence of a volcanic past, yet they are so dissimilar to one another, it's hard to believe they all formed in the same way. Besides that, while all Hawaiian islands have volcanic origins, only Big Island has active volcanoes. These confronting facts had scientists come to a conjecture that something is missing in the theory of the archipelago's past...

  Felix Andries Vening Meinesz  By Woodwalker at en.wikipedia

Felix Andries Vening Meinesz By Woodwalker at en.wikipedia

To continue with the story, we have to return to Mister Felix Meinesz and his gravimeter. The instrument was used to measure gravity at sea level and below the ocean surface, so when Meinesz took measurements aboard submarines, he found some gravity anomalies at the ocean floor. He attributed these anomalies to prove a theory formed earlier in 1912 by German geophysics Alfred Lothar Wegener, called "continental drift". The hypothesis Wegener put forward posited that continents move about each other, "drifting" on the ocean floor. His idea, albeit uncompleted, sparked a race to find solid evidence of continental movement. The next piece of the puzzle was delivered with the technological advancements brought into the World War I Theater. The invention of sonar enabled the military to draw a virtual map of the ocean floor. The results of these surveys were shocking- instead of a vast, flat plain, as was believed before, the bottom of the seas is full of features, just like continents it surrounds- valleys, canyons and even enormous mountain ranges are all present underwater. The most interesting find emerged in form of undersea ridges that run parallel to continents' coasts (we call them mid-ocean ridges). They couldn't form as a coincidence, in fact more and more scientists were agreeing that continents move, however the ultimate evidence was still missing.

The mid-ocean ridges puzzled geologist until an American ocean geologist Harry Hess proposed a theory stating that under these ridges hot magma rose closer to the surface, pushing the ocean floor apart, hence the continental movement. His hypothesis began to make broader sense when US Navy published a report of seafloor magnetism they've prepared during the Second World War. They've found that basalt rocks (basalt is a type of lava that is abundant on the ocean floor) have magnetic minerals in them that are "locked” with the alignment of Earth's magnetic field. Interestingly, these magnetic rocks showed that Earth's magnetic field reversed its polarity (so the magnetic north flipped and became magnetic south and vice versa) many times during the past. Scientists took this new knowledge to a Mid- Atlantic ridge and made a remarkable finding- at the crest (the area center of the ridge), the polarity was normal (same as now), but moving away in either direction, they've found rocks with reversed polarity at approximately the same distance from the crest. That proved the theory of magma pushing the ocean bottom away and creating new seafloor as it cools down. They named these places divergent boundaries. Continued research yielded another discovery- there are also places called subduction zones, where ocean floor seems to be sinking down to the Earth's interior, one part of the crust sliding under the other. Those places are called converged boundaries. The third type of boundary was discovered later and called transform-fault boundaries, where two crust "plates" are sliding horizontally past one another (this kind of plate boundary is responsible for earthquakes in California, for example). The outcome of this research can be seen in the below picture:

Global tectonic activity of the Earth . Picture by NASA

A map of the world, complete with mid-ocean ridges and subduction zones. The visualization of these ocean features formed a revolutionary theory, a discovery that changed geology forever and helped to understand how our planet changed in the past, explained how many of the natural features on land came to be and gave a clue about origin of earthquakes and volcano eruptions.

The theory of plate tectonics is the widely accepted to be the best model of our planet's geology. According to its principals, the Earth's crust (our planet's outer, solid layer) is broken up into pieces called tectonic plates. There are 8 major and several smaller tectonic plates in the world and they all seem to "drift" or "slide" on Earth's next layer, the upper mantle. The constant movement of tectonic plates re-shaped the size and amount of continents our planet had in the past, but also created some of the most amazing natural wonders we admire these days. The creation of Himalayas, for example, happened when ancient Indian continent, drifting north as part of Indo-Australian Plate, collided with the Eurasian plate. The "forehead" of Indo-Australian plate, in form of the ocean crust, got uplifted, turning into a new mountain range- Himalayas. The same kind of plate collision remnants can be found all over the world.

Another result of plate boundaries interaction are frequent earthquakes (when plates slide against each other, sometimes the energy absorbed by the rocks reach a certain point where it can no longer be held, the rock fractures and that energy is released in a form of seismic waves, creating earthquakes on the surface of our planet (it is called an elastic rebound theory). In addition to that, plate boundaries are regions of intensive volcanic activity. In fact, when geologists mapped the most active volcanoes on Earth, it turned out most of them follow plate boundaries. A string of 452 volcanoes, oceanic trenches, volcanic arcs and volcanic belts form a horseshoe shaped line extending from the Pacific coasts of South and North Americas, north to Bering Strait and then south around the coast of Japan, Philippines, Indonesia and other South Pacific islands, reaching the southern tip of New Zealand. This imaginary line is called Pacific Ring of Fire and it encompasses the most seismically and volcanically active regions in the world. An impressive 75% of planet's most active volcanoes lays on the Ring of Fire, the sites along the line are also epicenters of 90% of all earthquakes occurring around the globe. The discovery of Pacific Ring of Fire and its relationship to plate tectonics brought answers to centuries’ old questions about volcanism and the destructive force of earthquakes. This new knowledge applied to vast majority of regions with high volcanic activity, but one place was different...

Pacific Ring of Fire Image by USGS

Hawaii lays right in the middle of the Pacific plate, thousands of miles from nearest boundary. There is no crack in Earth's crust through which lava could come up to the surface. Knowing that the theory of plate tectonics is likely correct, Hawaii volcanic origins remained a mystery. Scientists had to turn somewhere else for clues. Once again, American Navy came with a possible solution when they've mapped seafloor north of Hawaii with sonar. The result revealed a chain of seamounts, underwater mountains made of volcanic rock that stretches for 3,105 miles (4,997 km), all the way to Aleutian Trench off the coast of Alaska. Beside seamounts, the chain also contains numerous islands, atolls and reefs. The southern part of the chain consist of the Hawaiian Island themselves, followed by the Northwestern Hawaiian Islands (also called the Leeward Isles) and in its northern boundaries, a seamount range called the Emperor Seamounts. Together, they form the Hawaiian-Emperor seamount chain, one of the longest on the planet. What is even more interesting about them, though, is that when you look at a 3-D model of the seafloor, seamounts and islands of the Hawaiian-Emperor chain form two, straight lines. No other seamount range is aligned with that level of geometrical precision.

Hawaiian-Emperor Seamount Range By Ingo Wölbern (own work, created with GMT Software) [Public domain], via Wikimedia Commons

The existence of Hawaiian-Emperor seamount range made the case of Hawaii origins even more complicated. Scientific community could not produce a valuable argument until a Canadian geophysicist and geologist John Tuzo Wilson proposed an unorthodox idea, basing his thoughts mainly on a simple observation- looking at the geological features of the major Hawaiian Islands, Wilson found that the northern the island was, the older it appeared to be (more erosion features, more vegetation). He was especially fascinated by the extensive erosion on the island of Kauai, with its dramatic Na Pali coast, a lush tropical jungle as far as eye can see and a deep ravine that tore a bruise through the island- the Waimea Canyon. Radiocarbon dating validated Wilson's assumptions- each following island, starting with Hawaii going north, was older than the previous. It is now estimated that Big Island is 400,000 years old, Maui from 1.3 million (West Maui) to 750,000 years old (Haleakala), Oahu around 3 to 4 million years old and the oldest, Kauai, dated at 6 million years old. However, continuing to date the other formations in Hawaiian-Emperor seamount chain and ending at its northernmost underwater mountain- Meiji Seamount- its estimated age is astonishing 82 million years old. The two very unique occurrences (sequentially rising age of islands and the straight lines Hawaiian- Emperor Seamount chain) led Wilson to formulate an incredibly interesting idea- theory of a hot spot. Wilson proposed that under Pacific tectonic plate lays a region of extremely hot magma, which rises through a system of canals within the lithosphere and surfaces at the ocean bottom, slowly forming an island. The volcanic activity continues for around a million years and then fades out as the island drifts away from the fixed hot spot with a tectonic plate it sits on. If this theory would prove to be true, the southeastern tip of Big Island is currently in the epicenter of the hot spot.

 Kamila holding sand that contains olivine

Kamila holding sand that contains olivine

John Tuzo Wilson theory of a hot spot was not only brilliant, but also highly believable, because it provided answers to previously unsolvable case of Hawaiian Islands geology. On the other hand, it also came with a new set of problems- what is a hot spot? How did it form? Why does it stay in the same place for millennia? An American geophysicist named William Jason Morgan proposed an answer to at least some of these questions by presenting a theory of mantle plumes. Mantle plume is "a posited thermal abnormality where hot rock nucleates at the core-mantle boundary and rises through the Earth's mantle becoming a diapir in the Earth's crust"-source Wikipedia. In plain English, mantle plume is sort of like a lava lamp, where a heavier liquid absorbs heat from a light bulb (in this case the Earth’s outer core), expands and rises to the top of the lamp (crust-mantle boundary). The magma that rises to the Earth's crust from the core-mantle boundary forms a dome under the crust and releases the pressure through a narrow "tunnel"- a hot spot. To find a proof of the mantle plume hypothesis, scientists literally cracked open lava rocks to examine their mineral content. They've soon found what they were looking for- locked in a lava rock sample from the island of Hawai’i was a mineral called olivine. This dark green mineral is known to originate deep inside our planet and seeing it on the surface validated Morgan's theory. To see olivine yourself, head to Papakōlea Green Sand Beach  on Big Island.

The theory of a hotspot not only explained how the island chain formed, but also provided an ultimate proof of plate tectonics. Today, the network of sensors allocated throughout the world is monitored by satellites using the GPS system, allowing for precise measurements of continental plates. The image below shows the direction of these minute changes in plate dynamics. The alignment of Hawaiian Islands corresponds to the movement of Pacific Plate, which drifts in the north-west direction at a speed between 2-4 inch (5-10 cm) per year. Once the hot spot hypothesis was widely accepted to be a reasonable explanation of Hawaiian island formations, scientists started looking for other island chains that might have been formed in the same way. We are almost certain that the Galapagos island chain as well as Iceland and some islands in the Indo-Pacific region were all formed by a hot spot.

  Plate tectonic movements measured by GPS devices. Image by NASA

Plate tectonic movements measured by GPS devices. Image by NASA

With Hawaii origins explained, a set of new questions arose: What happened to the older islands in the chain? What is the future of Hawaii? What happens when Big Island moves out of the hot spot? For answers to those and other questions about Hawaii archipelago geology, we need to go back to sea floor mapping...

 Aerial photo of Nihoa island. By George H. Balazs, NOAA

Aerial photo of Nihoa island. By George H. Balazs, NOAA

Magma, in form of a mantle plume, that accumulates below Hawaii generates an extreme pressure on Earth's crust- the map of sea floor around the island chain shows that the crust is bowed upward around 500 feet from the surrounding seafloor, creating a gently sloped underwater "hill". As the islands move away from the hot spot, they slide off this "hill", slowly sinking into the ocean. It is estimated that Kauai, the oldest of the major Hawaiian Islands, will be reduced to merely a rock sticking out from the Pacific Ocean, resembling the current state of Nihoa, the tallest island of the Northwestern Hawaiian Islands, located 140 miles (240 km) from Kauai.

Plate tectonics is not the only cause Hawaiian Islands disappear. The archipelago is constantly shaped through wind and water erosion. One look at the landscape of Kauai reveals the sheer power of erosion that takes place there- geological features like Waimea canyon or Na Pali coastline make an impression of an island made out of limestone that's dissolving rapidly. That would surely make sense, only if the entire island wasn't made out of one of the hardest rocks on Earth- tholeiitic basalt. How could water do so much damage in so little time (in geological perspective, that is)?

As hard as tholeiitic basalt may be, it has one flaw- high iron concentration in its structure. On the other hand, Kauai owe it's amazing greenery to the high annual rainfall (in fact, Mount Wai-‘ale-‘ale is the wettest spot on Earth with 450 inches (11,430 mm) of rainfall annually). Combine the two and tholeiitic basalt flaw becomes its nemesis- the rock literally rusts away when it's wet. The incredibly beautiful red color of Kauai mountains and canyons is due to oxidization of iron present in ancient basalt lava. When the rock "rusts", it becomes soft to the point where it breaks easily when handled. This erosion process slowly dissolves Hawaiian Islands one by one, until their ghostly remains are swallowed by the Pacific Ocean. This phenomenon can be observed on every island in the chain- the Big Island's Waipi'o Valley is in the initial phase of cliff erosion, while Maui's Olowalu Valley shows a more severe weathering.

Iao Valley on the island of Maui. From our 2013 trip 

A closer study of Moloka’i resulted in yet another island shaping event. In the late 1980's, vastly improved sonar technology allowed for creating a detailed map of the ocean floor. United States Geological Survey mapped the area around Hawaii using Gloria side-scan sonar, an aperture designed specifically for sea topography scanning. They've found a large accumulation of undersea boulders 200 miles north of Moloka’i. When geologists started measuring these pieces and took rock samples to find out where they originated, the outcome turned out to be quite shocking- the debris scattered on the ocean floor, if put back together, fit like a jigsaw puzzle back into Moloka’i north shore. Radiocarbon dating estimated the rock samples to be 1.5 million years old and consist of exactly the same element composition as rocks on the island. There is no doubt a cataclysmic landslide occurred on Molokai- virtually half of the island slid at once into the ocean in an event that lasted only few minutes. The result- a mega tsunami, with waves that could have reached 1,000 feet (300 meters) in height, swept through the Hawaiian islands and reached as far as the coast of Australia to the west and US Pacific coast to the east. Aftermath of this natural disaster left Moloka’i with a new coastline, its cliffs reaching 3013 ft. (1010m), the highest in the world. Later research confirmed that landslides occurred many times on Hawaiian Islands, most recent one around 100,000 years ago. They occur because the land sits on an unstable, sandy surface layers sandwiched between volcanic rock. When fresh lava flow reaches the ocean, it solidifies on a sandy beach, a weathered lava rock from past eruptions. The new land, sitting directly on top of that weak foundations is prone to give away and slide into the ocean.

 Debris field from Molokai and Oahu landslides. Image from Google Earth

Debris field from Molokai and Oahu landslides. Image from Google Earth

Hawaii landslides are a real threat not only to the archipelago, but also to the entire Pacific Northwest, New Zealand and New South Wales. Particularly alarming is current condition of part of the island of Hawaii called the Hilina slump. This chunk of land, 5,000 cubic mile (20,000 km³) in size, located in Kilauea east rift zone, is literally breaking away from the rest of the volcano and sliding towards the ocean at a rate of 4 inches (10 cm) a year. This displacement can (and did in the past) create earthquakes and it is not ruled out that this massive chunk of land can suddenly slip at a much faster pace. If that would happen, the outcome would be catastrophic to millions of people living near Pacific coast. Scientists take this threat seriously and the many faults created by Hilina slump displacement are closely monitored and studied.

Through the amazing work of scientists from all over the world, we discovered how Hawaiian Islands came to be, what forces shaped them to how they look today and we learned the chain's ultimate fate in the depths of the Pacific Ocean. One remaining question still awaiting answer was- What's next? We know Kauai will mostly likely disappear completely in 1-1.5 million years, Oahu will take place as the oldest Hawaiian island, Maui will continue to reshape its landscape and Big Island volcanoes will eventually finish their eruptive phase. What will happen when Kilauea move away from the hot spot? The answer: it will be time for Lōʻihi to shine...

  Pillow lava from Loihi volcano, Public domain photograph by A. Malahoff, University of Hawaii, 1980. Figure 6.8-C, U.S. Geological Survey Professional paper 1350.

Pillow lava from Loihi volcano, Public domain photograph by A. Malahoff, University of Hawaii, 1980. Figure 6.8-C, U.S. Geological Survey Professional paper 1350.

When geologists looked at the topographical map of the seafloor around Big Island, they've located a number of seamounts surrounding the sea south of Hawai’i. They've assumed them being extinct volcanic cones from ancient eruptions, until in 1952, a swarm of earthquakes centered in one of the seamounts rocked the ocean floor. This event sparked a series of observations on this distinctive underwater mountain, named Lōʻihi (Hawaiian word for "long"). Scientists mistakenly attributed these earthquake swarms to be characteristics of an extinct volcano. It wasn’t until 1978, when USGS submarine took pictures of Lōʻihi and collected rock samples, that the understanding of this seamount shifted. The rock that geologists examined turned out to be pillow lava, a heavy kind of lava associated with an active volcano. The now heavily studied Lōʻihi shook the earth on few separate occasions during the 80’s, further indicating that the underwater volcano was very much active. The breakthrough came in 1996- a greater magnitude earthquake indicated an ongoing eruption. The University of Hawaii gathered a dive team to document the event first hand and even though they came late, the discovery was still remarkable. Lōʻihi’s summit partially collapsed upon itself, forming a new crater, named Pele’s Pit. Since that time, Lōʻihi remains fairly active, but it doesn’t erupt continuously like Kilauea. As of now, we know much more about Hawaiian Islands newest volcano- it sits 22 miles south of Big Island, has a summit area with three pit craters, highest of them standing 10,000 ft. (3000 m) above the surrounding landscape. Radiocarbon dating of rock samples from Pele’s Pit determined Lōʻihi to be around 400,000 years old. Lōʻihi is currently 3,000 ft. (975 m) below sea level and with an estimated 0.1 inch (2.5 mm) of yearly growth, it may surface as Hawaii new island anytime between 10,000 to 100,000 years from now. However, it may as well stop erupting entirely and never reach its island phase, moving away from the hotspot and giving away for a new volcano to “race up” to the sea level. Nobody really knows which of the two will happen, nevertheless Lōʻihi gives scientists an amazing opportunity for studying the volcanic island building process all the other islands in the Hawaiian chain went through. Since 1996 eruption, the seamount acts as an underwater laboratory and site of numerous experiments. The University of Hawaii installed an ocean bottom observatory nicknamed HUGO (Hawai’i Undersea Geological Observatory) in 1997, which provided 5 years of continuous monitoring of volcano’s chemical and seismic activity (the fiber optic cable connecting HUGO broke twice, shutting it off for the second time in 2002). Moreover, many other expeditions has been funded, resulting in video footage and collection of rock and water samples. Lōʻihi will probably “wake-up” and start erupting again in the near future, providing years of data for Earth’s volcanic past studies.

 Location of Loihi Volcano. Image taken from Google Earth

Location of Loihi Volcano. Image taken from Google Earth

Learning about Hawaii geological history is like reading a piece from one of humanity’s great mythologies. A story of origins, death and rebirth, driven by an inescapable fate. With passing time, each island in the Hawaiian-Emperor Seamount chain went through, or currently is going through, a great transformation: from a harsh, uninhabitable landscape of jet-black lava, through a period of life spreading its seeds to dominate the land, shifting its appearance to an Eden like scenery and finally succumbing to the unforgiving depths of the Pacific Ocean. A story that will repeat itself for eons, long after we humans perish, until the mantle plume fueling the hot spot drain all the magma, finalizing this unbelievable act of creation. Knowing when any of that may happen is still beyond the realm of our imagination. Nevertheless, we can witness the land forming force first hand by visiting the island of Hawai’i and, with a little bit of luck, seeing the glowing red river of liquid rock engaged in a fierce battle with the ocean.

Geology of Hawaiian Islands fascinate and help with understanding of elemental forces that shape Earth and ultimately, the whole universe we’re part of. I hope you enjoyed reading this article as much as I did writing it. Please share with your friends and leave comments below, we really appreciate you visit IBN travel.

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