8: Sedimentary Rocks & Processes Flashcards
How do sedimentary rocks form?
Deposition: laying down of material by a natural agent (air, water, ice, gravity) or by precipitation of solution
- Often occurs in sedimentary basins
Lithification:
compaction + Cementification = lithification
- Compaction: The process by which pressure reduced the volume of sediments due to a reduction in void space
- The process by which clastic sediments are converted to rock by the precipitation of mineral cement (calcite, quartz, iron oxides) between grains)
What are the three main categories of sedimentary rocks?
- Clastic (detrital)
- starts as clasts, aka fragments or particles
- sandstone, siltstone, shale, mudstone… - Chemical (evaporites)
- Formed by precipitation from solution
- halite, gypsum, some limestones - Organic (biogenic)
- Formed from previously living organisms
- Chalk, coal, and most limestones
Describe Clastic (detrital) sedimentary rock
Composed of fragments of weathered and eroded rocks, grains, and particles
The longer the rocks travel:
- the finer the grains
- the more rounded and less angular due to abrasion from transport
poorly sorted = well graded, you start with this
well sorted = poorly graded
you get this after a long transport
For Clastic Sedimentary Rocks, what are the 4 groups? Give examples for the major 2:
Mudrock
- mudstone: 75% silt and clay, not bedded
- Shale: 75% silt and clay, thinly bedded
- siltstone: More silt than clay
Sandstone
- Quartz sandstone: dominated by sand, >90% quartz
- Arkose: dominated by sand, >10% feldspar
- Lithic wacke: dominated by sand, >10% rock fragments, >15% silt and clay
Conglomerate
- pebbles to boulders, rounded clasts
Breccia
- Pebbles to boulders, angular clasts
Give me some characteristics of Shale, Mudstone, Sandstone, Conglomerate, and breccia:
Shale: splits easily along bedding and lamination
Mudstone: does not break in layers like shale
Sandstone: Dominated by sand sized grains that are cemented together
Conglomerate: rounded grains >2mm in a finer-grained matrix
(only diff is conglomerate is like rounded chocolate chips while Breccia is like chocolate flakes in mint ice cream)
Breccia: Angular grains >2mm in a finer-grain matrix
Describe Chemical (evaporites) sedimentary rocks
Precipitation of minerals from solution
- Often requires restricted basin in warm arid climates
What are some common evaporites?
Halite: NaCl (rock salt)
Gypsum (CaSO_4 2H_2O)
- used in “Gyprock” drywall
Speleothems: CaCO3
- precipitated in caves
Tufa: CaCO3
- precipitated from cold springs
Travertine: CaCO3
- Precipitated from hot springs
Describe Organic (biogenic) sedimentary rocks. Name Some:
They are the remains of living things.
limestone
chalk: Another calcium carbonate from plankton
Coal: Formed from the remains of vegetation, composed mainly of carbon (fossil fuels)
What is coalification?
Conversion of peat (organic soil) to sedimentary rock under pressure and temperature
What are fossils in sedimentary rock? What do they do?
Fossils are the preserved traces of animals, plants, and other organisms,
They help us identify and correlate sedimentary rocks at different sites
Also help us date rocks
What is sedimentary structures? Name all the layers:
Sedimentary structure is a feature formed during deposition that gives clues to the environment and the time and place:
TOP
- Planar bedding
- current bedding showing cross lamination
- ripple marked bedding
- imbricate (overlapping) fossil shells)
- Graded bedding
- Cut-and-fill bedding
BOTTOM
What is Bedding?
A layer of sediment or sedimentary rock with a recognizable top and bottom called a bed
The boundary between 2 beds is a bedding plane
A series of beds that is distinct from beds above and below (and thick enough to be shown on a map) is called a formation
What can ripples in sedimentary structures tell us?
There are symmetric and asymmetric ripples:
symmetric: still water like beach
Assymetric: a direction was prefered, like ripples in a river bed or wind in a desert
What are facies?
They are a distinct rock unit that forms under certain conditions of sedimentation, reflecting a particular process or environment
Here, vertical and lateral differences reflect changes in conditions over time and space