The following pictures are from my trip to Hawaii in June of 2022
How Hawaii Was Formed: Understanding Plate Tectonics
Hawaii is located in the middle of the Pacific Ocean, but did you know it's not sitting on the edge of two tectonic plates like most volcanoes? Hawaii is actually on the Pacific Plate, which is the largest of Earth's tectonic plates. The Pacific Plate is constantly moving, but Hawaii's islands were created by a special process that doesn't happen at plate boundaries like earthquakes or many volcanoes do.
Earth's outer layer, or crust, is made up of large pieces called tectonic plates that float on the soft, hotter layer beneath them, called the mantle. These plates are always moving, but very slowly. Most volcanic activity happens where plates are colliding or pulling apart, but Hawaii’s volcanoes are different. They were formed by a hotspot—a place deep in the Earth where hot, molten rock (magma) rises up through the crust and forms volcanoes.
Hawaii sits right on top of one of these hotspots. Over millions of years, as the Pacific Plate moved northwest, the hotspot stayed in the same place, causing new islands to form as the plate slowly moved over it. That’s why Hawaii is made up of several islands that stretch in a line! The oldest islands, like Kauai, are further away from the hotspot and are no longer active. The youngest, like the Big Island, is still sitting over the hotspot, which is why it has active volcanoes like Kilauea and Mauna Loa.
Map from: Butler, Rob. Volcanoes and tectonic plates: Ring of Fire - tectonic journeys in E Asia:.” YouTube, 9 April 2024, https://www.youtube.com/watch?v=nI04nTzBtV0. Accessed 30 September 2024.
The Pacific Plate itself is surrounded by different types of plate boundaries. To the east, it is bordered by the North American Plate, while to the south, it meets the Antarctic Plate. These are all part of the Pacific Ring of Fire, a horseshoe-shaped zone where lots of earthquakes and volcanic activity happen because the plates are either colliding, pulling apart, or sliding past each other.
Though Hawaii isn't on the edge of a plate boundary, its creation is still deeply connected to the movement of the Pacific Plate. As the plate moves, new islands form, and older ones slowly erode and shrink. This process of island formation will continue as long as the hotspot remains active, and the Pacific Plate keeps moving.
The movement of tectonic plates and the existence of hotspots like the one under Hawaii show us how dynamic and constantly changing Earth’s surface is. Hawaii is a perfect example of how powerful forces beneath the ground can create something as beautiful as these islands!