Chapter 7, Test 2 Flashcards
crossbedding
layers of sediment at angles, usually formed from dunes
what sources can sedimentary rocks contain
coal
petroleum or natural gas
iron, aluminum, and magnese
lithification
unconsolidated sediments are transformed into solid sedimentary rocks by compaction or cementation
detrital rocks
made up of solid pieces of weathered rocks
clay minerals, quartz, feldspar, mica
chemical rocks
made up of precipitated ions that were once in a solutuon
organic rocks
made up of material once living
shale
mid sized particles in thin layers that are commonly referred to as lamine
sandstone
composed of sand sized particles
quartz is the predominate mineral
conglomerate
consists of largely rounded gravels larger than 2mm in diametet
breccia
composed of mainly large angular particles larger than 2mm in diameter
inorganic process
no previous life
organic process
life. example, seashells
chemical sedimentary rocks
consists of precipitated material that was once in solution
limestone
most abundant-calcite
coquina
organic limestone
made up of broken seashells
travertine
inorganic limestone
deposited by mineral springs. especially hot springs
example- stalagmites and stactites
oolitic
inorganic limestone
grows like snowballs or like tree rings around fine particles in shallow agitated water
example- antelope island
dolostone
similar to limestone but contains calcite and magnesium. formation is a mystery. found in Logan canyon
chert
made up of microcrystalline quartz
includes Flint and Jasper
lots of arrowheads made of this
evaporites
cause deposition of chemical precipitated
example- salt or gypsum. gypsum is made into drywall
coal
composed of organic material that has been burried for millions of years. (leaves, bark, wood)
stages of coal formation
1-plant material (in a swamp)
2- peat (partly decomposed)
3- lignite (soft brown coal)
4- bituminous (compact black Rock)
continental (sedimentary environment)
dominated by erosion and deposition associated with springs
glaciers
winds
marine (sedimentary environments)
shallow (about 200 meters)
deep (seaward of continental shelves)
transitional (sedimentary environments)
tidal flats
lagoons
Deltas
(shoreline between continents and oceans)
strata/beds
rock layers
bedding planes
flat surface that seperate the strata
graded bed
did sediment that represents decrease in stream transport energy
ripple marks
form alone sea shore or stream bed