Exam 2 Flash Cards
Continental crust on both sides, divergent motion, breaks continents apart, makes deep rift valleys and narrow new oceans
Rifting zone
Oceanic crust on both sides, divergent motion, makes oceans wider and releases heat at a mid-ocean ridge (MOR)
Spreading zone
Oceanic crust on both sides, convergent motion, recycles ocean crust, makes a deep-sea trench and an island arc
Oceanic subduction zone
Oceanic crust on one side, continental on the other, convergent motion, recycles old ocean crust, makes a deep-sea trench and volcanic mountains
Continental subduction zone
Continental crust on both sides, convergent motion, joins small continents into larger ones, makes huge non-volcanic mountains
Collision zone
Any kind of crust, transform motion, connects other types of plate boundaries, makes a strike-slip fault with lots of earthquakes
Transform zone
Most powerful physical weathering process, requires lots of freeze-thaw cycles = wet climate that is sometimes hot and sometimes cold
Frost-wedging
Most powerful chemical weathering process, requires a wet climate, turns feldspar into clay and makes saprolite (clay that looks like rock)
Hydrolysis
Combines metals with oxygen in air, makes colorful minerals
Oxidation
Both water and oxygen combine with iron in rocks to make rust
Limonite
Rocks dissolve away completely to make caves
Dissolution
Rotting organic matter, provides nutrition for plants
Humus
Pure organic layer at the top of soil
O-Horizon
Mix of humus, sand, clay and oxides; also known as topsoil
A-Horizon
Mix of sand, clay and oxides, also known as subsoil
B-Horizon
Weathering rock just starting to break down at the bottom of soil
C-Horizon
Individual rocks fall over time to form talus piles
Rockfall
Many rocks move downhill as a jumbled mass
Rockslide
Rock and soil moves downhill in one intact block
Slump
Soil layer slides over rocks very slowly
Creep
Rocks and soils move downhill like soft pudding
Earthflow
Water mixes with clay to make a slurry that can flow for long distances
Mudflow
Internal layers all slant the same way, usually formed by rivers
Unidirectional cross-beds
Internal layers slant in different directions, formed by wind or waves
Bidirectional cross-beds
Very large layers, formed by desert dunes
Meter-scale cross-beds
Thin layers formed by channels or storms
Small-scale cross-beds