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14 Cards in this Set

  • Front
  • Back

Sedimentary Rocks

The result of deposited material which eroded from other rocks and was cemented and lithified by time, pressure, and sometimes exposure to fluids

Chemical and Biogenic

Result of precipitation from water or biochemical processes



Examples: halite, gypsum, limestone, diatomite

Carbonaceous

Result of organic matter decay



Example: peat

Clastic or detrital

Result of transport



Examples: mustones, sandstones, conglomerates

Altered minerals

Result of leaching



Examples: kaolin, bauxite

Grain Size

Indicative of environment under which sediments were deposited: fine grained material required low energy -> air or water were carriers. Fine grains can also mean particles were transported and eroded for long distance

Stratigraphy

Nearly all sedimentary rocks are layered; this is due to their origins. Layers are almost always deposited horizontally.

Evaporites

Formed by precipitation of minerals from solutions when concentration reaches saturation from water evaporation



Examples: halides, sulphates, nitrates, borates, carbonates

Potash

An evaporite. Refers to all soluble potassium salts.



Sylvinite is the rock that contains NaCl (halite) and KCl (sylvite)

Lithium

LiCl is precipitated and turned into Li2CO3 which is used to make batteries 924% of Li production), lubricants, pharmaceuticals, etc

Cryptocrystalline Silica

Chert, opal, chalcedony (onyx, carnelian, petrified wood)



Chert formed by chemical or biogenic processes

Diatomite

Biogenic. Consists of fossilized remains of diatoms. Used as filtration aid, mild abrasive, various other uses

Pearls

Microcrystalline calcium. Produced by mollusks when irritating microscopic object becomes trapped within the mollusk

Phosphates

Phosphorites



Carbonatites



Guano