Kohala Volcano Essay

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Introduction
Kohala Volcano is the oldest of five volcanoes in hawaii. Kohala is estimated of 1,000 years old and it emerged above sea level over 500,000 years ago. The most recent eruptions were 120,000 years ago. That was a long time ago! I wonder when it were to ever erupt again! Hopefully it won't erupt soon! Kohala volcano is extinct. Kohala is so old, that it experienced, and recorded a reversal of magnetic field 780,000 years ago. Kohala is a shield volcano cut by multiple gorges. Between 250,000 and 300,000 years ago, a huge avalanche consumed a slice of the volcano’s northeast flank more than 12 miles wide at the shoreline. The debris spilled more than 80 miles out and onto the ocean floor. The lasting effects can still be seen today …show more content…

An international group of scientists led by University of Hawaii researchers revisited a fossil deposit first found high on Kohala’s flanks in the 1930s. And, there’s much more to learn about Kohala’s past in the future.

Big Island Hawaii Volcanoes
All Hawaii volcanoes have their own distinct features. While the entire chain of Hawaiian volcanoes extends more than 3000 miles nearly 5000 km across the Pacific Ocean, most have been quiet for hundreds of thousands, even millions of years. Six Hawaii Island volcanoes coalesced, or joined, to form the Big Island: Mahukona Volcano, Kohala Volcano, Mauna Kea Volcano, Mauna Loa Volcano, Hualalai Volcano and Kilauea. While Kilauea may be the most famous of the Hawaii Island volcanoes, Mauna Loa and Hualalai are also active volcanoes. To be considered active, a volcano will have erupted at least once in the last 10,000 years, and there continues to be sufficient seismic activity below the surface to suggest that another eruption may occur in the next 1000 years or less. Kohala was devastated by a massive landslide between 250,000 and 300,000 years ago. The Hawaiian …show more content…

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. In geologically recent times, a new volcano, Loihi, 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 Loihi, whose summit lies approximately 3,178 feet below the surface of the ocean today, will begin

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