mineral
solid orderly material not made from life arranged in a pattern
4 mineral classes
silicates, oxides, sulfides and sulfates, carbonates
aphanitic
small grains, cools fast
phaneritic
large grains cool slow
most common sedimentary
Shale - clay
Limestone - chemical
Sandstone - sand
origins of coal and petrolium
coal-peat from wetlands
petrolium-shallow seas
weathering
process where solid rock is broken apart and desolved
erosion
transportation of rock fragments by water wind and glaciers
denudation
the lowering and wearing away of earths surface
angle of repose
maximum slope angle that a material can be stable. main reason for mass movement.
classifications of mass wasting processes
Soil creep: slow dry rock fall: fast dry debris avalanche: fast damp mud flow: fast wet slump: middle earthflow: middle soliflucation: slow wet