Physical Geology: Chapter 1&23 (introduction to geology & earths companions) Flashcards
1
Q
geology
A
is a science that studies the origin and evolution of Earth and solar system bodies
2
Q
geocentric model
A
model that places Earth at the center of the solar system
3
Q
heliocentric model
A
model that places the Sun at the center of the solar system
4
Q
differentiation
A
- the process through which the Earth transformed into a different planet with a zoned interior (the crust, the mantle, and the core)
- partial melting or complete melting of earth allowed heavier more dense minerals and elements like: iron (Fe) & nickel (Ni) to sink to down a produce the core; also allowed the reverse, lighter less dense minerals and elements like: silicates, and plagioclase feldspar
- the energy to partially/completely melt the earth came from:
1) impacts; and 2) radioactive decay
5
Q
The Core
A
- inner most zone of the Earth
- gravity, seismic, and geochemical data strongly suggest its mostly made up of iron
- core molten on outside (ouster-core) and solid on the inside (inner-core) where the pressures are highest (5200 to 6400 km in depth)
6
Q
The Mantle
A
- is material in the middle zone
- makes up the bulk of solid earth
- seismic and geochemical data strongly suggest is has an intermediate density and is formed mostly of compounds of O2 with Mg, Fe, and Si
- about 40 to 2900km in depth
7
Q
The Crust
A
- materials that floated toward the surface of magma ocean formed Earths solid crust
- thin outer layer up to about 40 + Km thick
- contains relatively light materials with low melting temperatures
- most easily melted compounds are Si, Al, Fe, Ca, Mg, Na, and k
8
Q
Earth has two heat engines
A
- internal: (comes from the initial formation of Earth and form radioactivity)
- external: (comes from sun a.k.a. solar energy)
9
Q
Internal Energy
A
- drives volcanism and other interior processes
10
Q
External Heat
A
- energizes the atmosphere and oceans which are responsible for climate and weather
11
Q
Earths surface: 1) the continents
A
- its not clear what caused the initial formation of the continents; hypothesis :
1) repeated melting and solidification of initial cooled surface: allowed lighter elements to become separated form heavier ones and float to surface
12
Q
2) oceans and atmosphere
A
- origin traceable to water and gases that boiled off during initial heating/ differentiation of earth (water, H, N, C initially bound in minerals , then freed by partial melting, carried to surface by magmas and then released through volcanic activity)
- gases released from volcanos in early Earth history are believed to have been the same as those released today in modern volcanoes
- today the atmosphere is mostly made up of N and O, but O apparently only persisted in atmosphere after photosynthetic algae developed and began releasing substantial O was a waste product
13
Q
Earth is composed of a system of interacting components
A
1) heat from interior drives mantle convection
2) solar energy drives most of biosphere and atmosphere
3) interactions between atmosphere, hydrosphere, biosphere, geosphere
14
Q
Lithosphere
A
- (crust and upper mantle): strong, solid, outermost shell; 100-200 Km thick; cool and brittle with roughly a dozen of plates
15
Q
Asthenosphere
A
- weak layer upon which lithosphere rides; weak because its almost at melting point; 100 to 200 Km thick and can also flow