Week 4 - Phase 2 Intro and The Geology of Seamounts
- Sidhhant Girhotra
- Oct 22, 2019
- 2 min read
Updated: Oct 30, 2019

What's my plan?
I started off phase 2 with a theme that I wanted to take forward and do some in-depth research on. Week 4 and 5 would be all about visualizing, reading and researching into Seamounts and the life around it. I would also try to get in touch with Southampton Oceanography society and the research team to get some insight into the world of underwater.
Things I wanna look into regarding my theme:
Geology of undersea Mountains
Deep ocean currents and their relationship with the Seamounts
Deep Sea corals and how they grow all around seamounts
Life around Seamounts
Conservation of Seamounts
Geology of Seamounts
Seamounts are large submarine volcanic mountains rising at least 1,000 meters above the surrounding deep-sea floor. Smaller seamounts are called sea Knolls and flat-topped seamounts are called Guyots. Seamounts tend to be elliptical possibly because the lavas are extruded from linear rifts in the seafloor.


As submarine lava flows, it forms oceanic basalt that is dredged from the seamounts, whereas, the summit and flanks of seamounts are generally covered with a thin layer of marine sediment. They are extremely abundant and occur in all major ocean basins. Thousands of seamounts have been reported from the south Pacific ocean basin alone. A linear cluster of seamounts may result when several are fed by lava extruded from a single linear rift. Most Pacific seamounts occur in linear clusters or elongate groups of 10 to 100.
Article - Geology of Seamounts

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