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Yet again we see the big island of Hawai'i being "under construction". All the Hawaiian islands are made of lava from a single active magma hot spot. As the pac
by dreamcompiler 4y ago
Yet again we see the big island of Hawai'i being "under construction". All the Hawaiian islands are made of lava from a single active magma hot spot. As the pacific plate moves northwest over this stationary hot spot, new islands are formed.
The Big Island (Hawai'i) is the youngest as it's over the hot spot now. The other islands have moved off the hot spot and no longer have active volcanoes. Among the oldest islands is Midway (yes that Midway) which is geologically part of the Hawai'i archipelago even though it's not politically part of it.
- gangstead 4y agoIs the big island the biggest just because it is the newest? Were the other islands bigger and have eroded over time?
- deleted 4y ago[deleted]
- dreamcompiler 4y agoGood question. I expect so but I'm not a geologist.
- ouid 4y agoThey're pretty young geologically, <5 mya. Hawaii gets insane amounts of rain, but its hard to imagine that being enough to fully erode an islnd the size of mauna kea, and i think you would expect to see similar volume between the islands if it were just erosion, since it would mainly just be flattening them, rather than dissolving them, but i'm also not a geologist.
- vikingerik 4y agoThe volume from an eroded island is still there, it's just flattened below sea level, ultimately down to a wider base at the sea floor.
- RajT88 4y agoMy wife and I go to Hawaii some winters to celebrate our anniversary (it was our honeymoon spot, of course it was). We've taken a few tours there to learn about the place. What I recall from those tours is that the islands are all slowly sinking. Indeed Big Island is the biggest because it's the newest - the older ones are smaller because they have had more time to sink / erode.
- s1artibartfast 4y agoKeep in mind that the exposed area and volume of the Hawaiian islands is a very small portion of their overall volume. It is also worth noting that most of the volcanos in the Hawaiian chain are part of a single ridge which connects bellow the surface. [1] The depth of the ocean also differs significantly along the emperor seamount chain. With all that said, This paper suggests that the rate of magma has increased recently. [2] https://www.researchgate.net/publication/222958454_Calculated_volumes_of_individual_shield_volcanoes_at_the_young_end_of_the_Hawaiian_Ridge https://www.researchgate.net/publication/222958454_Calculate... https://www.researchgate.net/profile/Michael-Garcia-15/publication/282070552/figure/fig4/AS:668448883478535@1536382041330/Multibeam-bathymetry-map-of-the-Hawaiian-Islands-illuminated-from-the-NW-grid-available.png https://www.researchgate.net/profile/Michael-Garcia-15/publi...
- saiya-jin 4y agoCold magma gets relatively quickly weathered by elements, so volcanic islands tend to go through process of creation and destruction on multiple levels. Only when foliage creates thick and cohesive enough layer to slow down weathering they become more long term (till new eruption swallows that foliage and here we go again). Ie Iceland get from time to time new small islands created and they disappear by same process usually within few years.
- msworddebugger 4y ago> 1.2 million years ago, Maui Nui was 14,600 square kilometres (5,600 sq mi),[1] 40% larger than the present-day island of Hawaiʻi. Sea levels were lower than today's, due to distant glaciation locking up the Earth's water during ice ages, thus exposing more land. As the volcanoes slowly settled by subsidence, due to the weight of the shield volcanoes and erosion, the saddles between them slowly flooded, forming four islands: Maui, Molokaʻi, Lānaʻi, and Kahoʻolawe by about 200,000 years ago. Another former volcanic island lying west of Molokaʻi was completely submerged, and covered with a cap of coral; it is now known as Penguin Bank. https://en.m.wikipedia.org/wiki/Maui_Nui https://en.m.wikipedia.org/wiki/Maui_Nui