Hawaiian cultural traditions and scientific theory together help us to understand how the Hawaiian Islands have formed and changed over time. Mo‘olelo of Papa and Wākea, and Māui describe the birth of our islands. Through mo‘olelo of Pele we discover how specific volcanic forms found throughout our islands were created. Science teaches us about the Hot Spot theory, the incredible and ever-changing life cycle of Hawaiian volcanoes, and more.
Sensational Sinkholes
Student Reader
Imagine a magical place known only to a few. A place with stories, history and wonder. A place filled with amazing secrets that have been gradually revealing themselves over the years. Keep imagining. Allow yourself to dive beneath the surface of the earth to discover new and unexpected treasures.
What might you find “beneath the surface of the earth?” SINKHOLES! — naturally eroded gaps in the earth’s surface where a whole new world exists! Read on to learn more!
Take yourself back 120,000 years to a time when the ocean was about 25 feet higher than it is today! Back then, this flat land wasn’t even land at all. It was a living, underwater coral reef. Sharks, eels, crabs, seals, and seaweeds populated this rich, shallow sea.
With the dead coral reef above sea level, it became land. (Check out the sample accompanying this reader.) Then another gradual process began. Rain falling on the mountains of Waiʻanae and Koʻolau brought dirt down to the old dead reef, filling in gaps and covering it. This created a broad, flat area known as the ‘Ewa Plain. Here, seed by seed, a dryland forest began to form. In place of eels and seals, sea birds, forest birds, and even tiny tree snails made this habitat their new home.
Changes continued. The dead coral reef – so obvious in some spots today – was affected by rainfall. Rainwater containing small amounts of acid began dripping slowly and steadily through the dead reef. This decayed the calcium in the reef, forming large holes. Some are several feet across! Some are 10 feet deep! And some expanded into bell-shaped underground caverns!
Why bell-shaped? Rainwater that collects beneath the surface evaporates slowly. Where it ponds, the acidic water keeps eating away at the lower walls of the sinkholes, making them much wider at the bottom than they are at the top. This continues until the holes become about 10 feet deep, where they come in contact with underground fresh water stored in rock. When acid rainwater combines with underground fresh water, it becomes diluted and stops eating away at the old coral reef. This is how sinkholes form in Hawaiʻi over thousands of years.
Now, let’s go back to the surface. Imagine an animal scampering along the plain looking for its next meal, when suddenly it tumbles down into one of the many deep sinkholes. Running around with no possibility of escape, how could it survive? It simply couldn’t. And hundreds of years later, long after its body had decomposed, its bones remain to tell the story of how this creature had become trapped, then slowly starved and sadly passed away.
As you may already know, Hawaiʻi has always been a special place. From goddesses and gods, from volcanoes to rainforests, and from seagoing wayfarers to chiefs and chiefesses, these islands offer much for explorers young and old. So, continue investigating your island home, and Hawaiʻi will become more fascinating every day. For proof, read on!
Birds developed in ancient Hawaiʻi where predators such as cats and rats were absent.
Who knows what else is out there waiting to be discovered? Keep your thinking caps on. Continue exploring what Hawaiʻi has to offer. With a little imagination, you can make the past spring to life! But be careful. As you’re springing around, don’t fall into a sinkhole – no matter what may be awaiting your discovery!
Lelekamanu Program
Kaʻena, Oʻahu’s First Shield Volcano!
It’s old news that the island of Oʻahu was formed by 2 gigantic shield volcanoes. Old news indeed!
Right off the press, the latest reports speak of a third volcano, unknown until recent time. Updates are certain to follow.
Just as Kīlauea’s explosive, fiery surprise of 2018 opened our eyes to new, exciting, and scary eruptions on the island of Hawaiʻi, now evidence has surfaced that paints a new picture of the geologic history of the island of Oʻahu. The news just keeps rolling in!
Long before Waiʻanae and Koʻolau became significant parts of Oʻahu, the great shield of Kaʻena slowly built but remained submerged for much of its life. When it finally appeared and when it sank again into its watery home, no one knows. But it became the firm foundation from which Waiʻanae and Koʻolau later erupted.
And while we previously wondered why Waiʻanae erupted so distant from its closest neighbor, Kauaʻi, we find that mystery solved. Kaʻena formed between the two! And the mass of the island that we once thought belonged to Waiʻanae was a mistaken assumption. Almost half of the material that we believed was Waiʻanae actually belongs to Kaʻena!
So, 62 miles northwest of Kaʻena Point – home to native seabirds, turtles, and coastal native plants – lie the sunken remnants of a lost piece of history – a shield that once rose more than 3,000 feet above sea level – the height reached today by Koʻolau.
It would have been impressive to be able to see Oʻahu in all its glory – 3 stupendous massive shields on display – perhaps hard to imagine after lifetimes of viewing the island through incorrect lenses.
Who knows what other surprises await our discovery? Life is filled with mystery – some just beneath our feet!
Images courtesy of Dr. John Sinton, University of Hawaiʻi, Department of Earth Sciences