Study Guides (390,000)
CA (150,000)
McGill (6,000)
EPSC (40)
Final

EPSC 201 Study Guide - Final Guide: Plagioclase, Mantle Wedge, Oceanic Trench


Department
Earth & Planetary Sciences
Course Code
EPSC 201
Professor
Anthony Williams- Jones
Study Guide
Final

This preview shows page 1. to view the full 4 pages of the document.
EPSC201 2004 Final Exam Review Section 3&4
1. Using a sketch, describe the formation of the Hawaiian islands?
Hot spots – stationary
Plate – dynamic
This causes lines of islands to be formed. This
can tell you the past movement of the plates,
and how it changed direction if the line
segments change directions.
You can also tell how fast the plates are
moving, by looking at the spacing in between
the islands and the age of the islands by rock
samples.
India definitely went over a hot spot while it
was migrating north. We know this by identical
rocks found at the hot spot and rocks in India.
The hot spots give a lot of information about
plate trajectories.
Hot spots don’t exist forever. They come and
go over a time period of tens of millions of
years.
2. Explain the statement “Silicate minerals comprise covalent and ionic bonds.”
The size of an ion has a big effect on the geometry of elements.
Ionic Bonds – the transfer of electrons from one atom to another, which forms charged ions.
Covalent Bonds – the bond shares electrons between the atoms, to fill the outer shell of each
atom, making it stable. The bonds are much stronger then ionic bonds.
Most rocks are formed through silicate mineral in which silicon bonding to oxygen is one of the key
building blocks.
In the simplest form, silicon is bonded to four oxygens in the form of a tetrahedron through covalent
bonding. What we see in the diagram is an arrangement of silicon tetrahedron. If you add up all the
charges of silicon and oxygen, you end up with -4 (SiO4). (Si has charge of +4, oxygen has charge of -2)
You're Reading a Preview

Unlock to view full version