Clastic - Sedimentary Rocks
Rocks made up of other rocks and sediments that have cemented together.
Biochemical - Sedimentary Rocks
Made up of shells and fossils.
e.g. Limestone
Organic - Sedimentary Rocks
Rocks made up of carbon based materials.
e.g. coal
Chemical - Sedimentary Rocks
Rocks that have a lot of salts in them from evaporation.
Rock Beds
Layers of rock. A common formation for sedimentary rocks.
Strata
Several beds of rock layered on top of eachother.
Contact
When two beds of different rock types are layered and touching.
Ripples
These occur in sandy environments and form perpendicular to the flow of water or wind that created them.
Crossbedding
Sediments that flow and roll to create beds of old dune material. Usually seen as dunes are created and move around over time.
Turbidity Currents
Fast moving currents of sediment laden water that move down slope. Often created by underwater movements like marine avalanches.
Turbidite
Are deposits of sediment that end up layered from course grains to fine grains.
Depositional Environments
Locations where sediments accumulate.
Terrestrial - Depositional Environments (4 types)
Where sediments accumulate on land. Still involves WATER processes.
Marine - Depositional Environments
Where sediments accumulate in bodies of water.
Sedimentary Basins
Places where the land has sunk and has been filled up by sediments.
Subsidence
Places where the land has sunk.
Foreland Basin - Sedimentary Basin type
These form at the bases of mountain belts
Transgression - Sea level Rise
When the depositional environment shifts landwards
Regression - Sea level Fall
When the depositional environment shifts towards the basin.
Diagenesis - Post Depositional Procress
The sum total of all the physical, chemical and biological changes to a sediment AFTER it is deposited.
Note: Involves changes in temps and pressure but not to the same extent as metamorphizing.
Replacement Sedimentary Rock
Diagenetic process - when one material in a rock is substituted by another.
e.g. petrified wood
Rift Basins - Sedimentary Basin Type
These sediment basins form at divergent plate boundaries.
Intracontinental Basins - Sedimentary Basin Type
These sedimentary basins form in random places on land that are not near any plate boundaries.
Passive Margins - Sedimentary Basin Type
There sediment basins form at the edges of continents that are NOT tectonic plate boundaries.