Types of rocks Flashcards
Sedimentary Rocks
formed by fluids (air/water)
Only on the surface of the earth
Two groups
- Clastics (pieces of rocks)
- Chemical/ Biogenic (organic compounds or fossilized microbes)
Material rocks come from
weathering (breaking up)
erosion (transport)
Weathering
- breaking down material (exposed to the elements)
Erosion
- plate tectonics
- base level (local or ocean)
Physical weathering
- makes the rocks smaller (sledgehammer breaking apart the rock)
- surface area of rocks (multiplies as it gets smaller)
Chemical weathering
- alter the chemical composition
- Water is exposed to rocks gets transported to a different location
Types of weathering
- Jointing (removing the surface or the pressure of rocks causes the rocks to fracture in crosshatching pattern) (physical)
- Freeze-Thaw wedging (more water enters the cracks to expands more) (physical)
- Root wedging (roots gets into the cracks and expands more) (physical)
- Salt wedging (water dissolved in halite rocks) (chemical)
- Dissolution (combination of physical and chemical combinations)
What breaks down first
edges (get rounded)
surfaces that are exposed
halite and olivine
Clastic sedimentary rock
- getting pieces of rocks and glued together
- clasts and “cement”
- diagenesis (glues sentiments together)
Three categories of grain sizes
- mud/silt
- sand
- gravel/pebble/cobbles
trends in size
source (mix and angler)
sink (well sorted and smooth)
maturity
changes chemically
immature (felsic and matic)
mature (same size and composition)
Large sedimentary rocks
anything larger than 2 mm
- breccia (angler near mountains)
- conglomerate (rounder near mountain streams)
Sand size
anything between 2-1/16 mm
- Lithic (mixed composition and immature) (landslides)
- Arkose ( mix of 2 or 3 materials pink potassium feldspar) (Alluvial fans)
- Quartz (only one mineral and mature) (can be red from iron or other red minerals) (beaches)
Fine grained
less than 1/16 mm (flood deposits or lakes)
- mud stone
- shale
Chemical sedimentary (evaporates)
formed from evaporation
- salts (halite, gypsum)
Biochemical sedimentary
formed from animal shells
- pelagic ooze (calcite, quartz)
- pelagic (limestone (tropic and mid latitude))
- Siliceous (chert-quartz (polar))
What happens when water gets cooler
hold more CO2 causing carbolic acid
- will dissolve calcite
Limestone
warmer oceans
shallow waters
Chert
Quartz/silica
- cold polar areas
- high acid
Coal and oil shale
organic carbon
- swampy
- near a coast line
- warm
- high amount of organic matter
Biogenic Fossils
preserve structures
imprints
petrified wood
Bedding and Stratification
form in layers Grand canyon (strati-graphic)
Stratigraphy (original horizontal)
states that sediment is deposited in a layer that is horizontal and parallel to Earth’s surface