• Shuffle
    Toggle On
    Toggle Off
  • Alphabetize
    Toggle On
    Toggle Off
  • Front First
    Toggle On
    Toggle Off
  • Both Sides
    Toggle On
    Toggle Off
  • Read
    Toggle On
    Toggle Off
Reading...
Front

Card Range To Study

through

image

Play button

image

Play button

image

Progress

1/41

Click to flip

Use LEFT and RIGHT arrow keys to navigate between flashcards;

Use UP and DOWN arrow keys to flip the card;

H to show hint;

A reads text to speech;

41 Cards in this Set

  • Front
  • Back

Geology

science of the Earth; study of materials, processes, products and history of the Earth

geoscientists

study the whole earth system - all parts of planet and their interactions

geophysics

prediction of earthquakes and volcanic eruptions, petroleum exploration etc

hydogeology

*exploring groundwater reserve and managing drinking water supplies

mineralogy

investigating the composition of minerals in rocks

structural geology (4)

plate tectonics, mapping, petroleum exploration, ore deposits,

geochemistry (4)

assessment of soil contamination, pollution, mineral exploration, climate change

paleontology

*history of life and ancient life; change through time

geoscientists need (5)

1. strong background in physics, chem, math, bio, commsci


2. solid knowledge of geological language


3. logical thinking


4. understanding of spatial and temporal scales


5. communication

spatial scales (3)


a) atom


b) mineral


c) rock


d) mountain


e) continent


f) earth

a) fraction of mm


b) mm to cm


c) cm to m


d) >1000 m


e) 100 - 1000 km


f) radius = 6370 km

times scales


a) age of earth


b) atlantic to open


c) rocky mountains


d) humans


e) glaciation


f) Mt St. Helens


g) earthquakes

a) 4.6 billion


b) 200 million


c) 60 million


d) 2 million


e) 10 thousand


f) 6 min


g) seconds

stars and galaxies

immense balls of incandescent gas, binded by gravity into galaxies (>100 billion), solar system arm of Milky Way

nature of our solar sytem (4 entities)

- sun = 99.8% of solar mass


- planets


- moons


- asteroids (belt between Mars and Jupiter)

planet

large solid body orbiting a star, spherical, cleared neighbourhood of objects

moon

solid body orbiting a planet. all planets but Mercury and Venus have moons

2 types of planets

terrestrial and giants

terrestrial planets

small, dense, rocky, closest to sun (Mercury, Venus, Earth, Mars)

giant planets

large, low density, outermost orbit , gas (jupiter, saturn) or ice (uranus, neptune)

Earth system

- interaction of components


- atmosphere (gaseous envelope), hydrosphere (blue liquid water), biosphere (life), lithosphere (solid earth)

internal and external processes fueled by ?

internal - radioactive decay, external - sunlight

atmosphere components (3)

nitrogen (78.08%) and oxygen (20.95%), other (0.7%)


sea level atmospheric pressure

14.7 psi

with increasing elevation

pressure decreases, density decreases, oxygen content decreases

Earth's surface components (2)

land (30%) and water (70%)

topography

land, defines plains, mountains, valleys

bathymetry

sea floor variations, defines mid-ocean ridges, abyssal plains, deep-ocean trenches

what is earth made of? (5)

- iron (32.1%)


- oxygen (30.1%)


- silicon (15.1%)


- magnesium (13.9%)


- other (8.8%)

minerals

naturally occuring crystalline solid

glasses

non crystalline solids, form by rapid cooling too fast for crystal growth

rocks (+3 types)

-aggregates of minerals


- igneous - cooled from liquid


- sedimentary - debris cemented from preexisting rock


- metamorphic - altered by T and P

sediment

accumulation of loose mineral grains, weathered and eroded from rocks, precipitated

metals

solids composed on metal atoms, high density, conduct electricity

melts

rocks that have been heated to a liquid, magma, lava

volatiles

materials that turn into gas at the surface, released from volcanic eruptions

what is the key to understanding the Earth's interior and why

density, average density of earth >> average density of surface rocks

crust

- outermost skin (from 70 to 7 km)


- base called the Moho where seismic celocity changes between crust and upper mantle


- upper part of tectonic plate

crustal composition

- oxygen most abundant


- 98.5% is 8 elements

mantle (4)

- 2885 km thick


- 82% of earth's volume


- convection mixes it and aids in plate motion


- upper and lower

core (3)

- iron rich


- outer and inner


- outer generates magnetic field

lithosphere (4)

-outermost 100 to 150 km of earth


- behaves rigidly


- crust and upper mantle


- makes tectonic plates

asthenosphere

upper mantle below the lithosphere, flows as a soft solid