unit 3 (sedimentary)
No description yet. This curated deck is ready for daily study.
Card preview (24)
weathering
pre existing rocks break down mechanically or chemically to produce sediment
clastic rocks
formed from mechanical weathering
mechanical weathering
when a material is broken into smaller pieces which still retain characteristics of the original material
lithification
sediment turns into solid rock via compaction and cementation
chemical weathering
material is altered by chemical action resulting in new material
deposition
sediment deposited in lakes, rivers, and oceans, or accumulates in desserts
erosion
erosional agents (wind, rain, ice) transport the sediment to new locations
biochemical
accumulation of living material
chemical rocks
formed from chemical weathering
shale (clastic)
fine particles compacted to form thin layers
breccia (clastic)
poorly sorted angular particles
sandstone (clastic)
well sorted sand size particles
conglomerate (clastic)
poorly sorted round particles
what can we tell from grain size?
• grain size decreases with decreasing current velocity • larger grain sizes are closer to the source of weathering
limestone (CS) forms by
chemical precipitation in shallow water
rock salt forms (CS) by
evaporation of shallow seas and lagoons
High velocity gives us what texture?
coarse
low velocity gives us what texture?
fine
Evaporites (CS)
result of evaporation of water
precipitates (CS)
changes in environmental conditions
gypsum (CS) forms by
evaporation
dolomites (CS)
a precipitate
sylvite precipitates are?
evaporites
travertine (CS)
form of limestone deposited by hot springs or limestone caves