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7.10 The Mid-Ocean Ridge - Part 1 (Chapter 7: Plate Tectonics) £2.99   Add to cart

Lecture notes

7.10 The Mid-Ocean Ridge - Part 1 (Chapter 7: Plate Tectonics)

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This document contains detailed notes on The Mid-Ocean Ridge - Part 1 from Chapter 7: Plate Tectonics of the A Level Geology course. It includes all the information required to secure a top grade in this part of the course. These notes took me many hours to complete and are how I revised for my exa...

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  • May 28, 2020
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  • 2018/2019
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Danny139
The Mid-Ocean Ridge –
Part 1

, The Mid-Ocean Ridge
• The MOR is a 60,000km long chain of mainly submarine volcanoes,
ridges, rifts, fault zones and hot springs which encompasses the
Earth.
• The average depth of the MOR is 2,500m, ranging from 1,800m
above sea level in Iceland, to 4,000m below sea level in the Cayman
Trough in the Caribbean.
• Every 50 to 500km, the MOR is offset by transform faults which divide
the MOR into many sections.
• MOR’s are the principal means of transferring of mass and energy
from the upper mantle to the surface by advection and partial
melting.

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