ch. 8 test Flashcards
Structure of Earth
Crust
Lithosphere
Asthenosphere
Mantle
Outer Core
Inner core
why is earth hot
- remnant heat from formation
- pressure from gravity
- decay of radioactive isotopes
Oceanic Crust
- made of basalt
-greater density than granite
Continental Crust
- made of granite
Examples of Convergent Boundaries
- Cont-Cont
-Ocean-Cont
-Ocean-Ocean
Cont-Cont
-Collision boundary
-Mountains get pushed up
Earthquakes, Landslides, Avalanches
-Ex. India into China
Ocean-Cont
-Ocean plate subducts under the continent
-plate melts under the continent, forms volcanoes
- trench forms at the boundary
- earthquakes
-Ex: Andes Mountains, Cascade Mountains
Ocean-Ocean
-One plate subducts under the other
- melts and forms island arc of volcanoes
-volcanoes, earthquakes, deep sea trenches
- Aleutian Islands, Japan, Philippines
Subsurface mines
- Coal and rich metals
- Hazards: Mine collapse, Dust+debris, methane
-acid mine drainage- sulfuric acid into water
Placer mine
- hydraulic mining of stream gravels (gold)
- destroys habitat
open pit mine
- quarry
-small open pit used for stone gravel and sand
strip mine
remove soil+rock, mine coal, replace soil+rock
-go strip by strip
-Ex: Montana/Wyoming coal mines
Mountain top removal
- commonly done in WV
-remove top of mountain then mine what’s below
igneous rocks
- formed from the cooling and crystallization of magma/lava
- Ex. Basalt, granite
sedimentary rocks
-rocks made of sediments
- sediment: broken down pieces of rock
- Sand, silt, clay
-pressed+glued together
-Ex. sandstone, limestone, shale
metamorphic rocks
- rocks that are chemically or physically altered by heat or pressure
- sandstone to quartzite
- limestone to marble
-shale to slate
-granite to schist/gneiss
physical weathering
-ice water wedging
-tree roots cracking rocks
- thermal expansion+contraction
chemical weathering
-mineral oxidation
-dissolving of minerals by acid rain
-salt corrosion
-plant secretion
erosive agents
water
wind
glaciers
Why are soils important
foundation for terrestrial ecosystems
90% of the world’s food
easily erodible, not quickly replaced
3 components of soil
-detritus
-inorganic mineral matter (sand/silt/clay)
-Critters (Fungi bacteria insects)
soil texture
% composition of sand, silt and clay in a given soil
Soil horizons (in order)
O horizon
A horizon
E horizon
B horizon
C horizon
Ohern asks everyone bring cookies
O horizon
- detritus/organic matter
-nutrients/food for critters
-retains moisture
-reduces erosion
A horizon
-topsoil (sand silt clay humus)
- home of critters
- where roots live and get nutrients
E horizon
eluviation- zone of leeching
- mineral nutrients deposited down
B horizon
- deposition of minerals/nutrients in clay form
-subsoil
C horizon
- weathered parent material
-bedrock
what do plants get from soils?
-mineral nutrients
-gas exchange
- water
-proper pH
organic fertilizers
-composted leaves/manure/plant remains
-adds detritus/humus to promote soil health
inorganic fertilizers
- add NH4+ or NO3- or PO43-
-can be unhealthy