Mass of sedimentary rock which can be defined and distinguished from another by its geometry, lithology, sedimentary structure, paleocurrent patterns, and fossils
facies
Facies
Geometry
Lithology
Sedimentary structure
Paleocurrent patterns
Fossils
Fossils lived where they were buried
Habitat of fossils is deduced by their morphology
Trace fossils are also used to define facies
Terrestrial environments
Alluvial fans
Fluvial (rivers)
Lacustrine (lakes)
Paludal (marsh and swamps)
Aeolian (desert)
Glacial
Transitional environments
Delta
Beach
Lagoon
Tidal flats
Marine environments
Reef
Continental margin (slope, shelf, rise)
Abyssal plain
Alluvial fans
Fan-view shape (top view)
Found in tectonically-active region
Formed by mudflow and debris flow
Alluvium
Freshly-eroded sediments
Size and extent of alluvial fans depends on area of basin, climate, lithologies, and tectonic activity
Alluvialfans
Poorly-sorted, coarse sediments due to proximity from source
Coarser sediments are found in the apex and fining towards the toe
Fluvial
Elongated bodies of water that flow though channels
Fluvial systems are the most active transported of sediments
Fluvial systems are dependent on energy and velocity (Hjulstrom diagram)
Types of river channels
Meandering
Braided
Anastomosing
Straight
Meandering rivers
Consist of a single channel and a thalweg (deepest point in a channel)
Braided rivers
Consist of multiple bars and thalwegs within a single low sinuosity channel
Poorly sorted, coarse-sediments
Anastomosing rivers
Multiple, interconnected, coexisting channel belts on alluvial plains
Laterally stable than braided channel
May consist of individual channels that may be braided, meandering, or straight
Straight rivers
More of a hypothetical end member and not often found in nature
Low sinuosity index
May be produced by tectonic controls
Drainage patterns
Dendritic
Trellis
Radial
Centripetal
Rectangular
Deranged
Ephemeral lakes
Land-locked body of standing water usually formed as a result of water filling depressions
Depressions that form ephemeral lakes may be caused by subsidence, isolation due to sediment deposition, glacial erosion and deposition, volcanic processes, landslides, or meteorite impacts
Lacustrine environments
May be freshwater or salt water
Good paleoclimate indicator
Special stratification - varves (alternating light and dark layers of sediments)
Paludal environments
Constant flooding of water, organic material, and fine sediments
Wet climates near the equator and temperate higher latitudes
High organic content favorable for coal formation
Aeolian
Ability of the wind to shape the surface of the Earth (and other planets) by erosion, transportation, and deposition
Deflation
Removal of loose particle by the wind
Abrasion
Cannonading of rock and other surfaces by particles carried by the wind
Deserts
Generally formed in areas with little to no rain (<250 mm/year)
Low precipitation - scarce vegetation
Scarce vegetation - high wind velocity
Formation of deserts
By-product of global atmospheric circulation
Rain-shadow effect
Coastal deserts
Continental interior desert
Polar desert
Aeolian sediment erosion and deposition
Ventifacts
Lag deposits
Desert pavement
Loess
Sand dunes
Types of sand dunes
Barchan
Parabolic
Traverse
Linear/longitudinal
Star
Glacial
Snow falls greater than which melts during summer
Permanent (on a human scale) body of ice that shows evidence of movement due to gravitational pull
Glacial drift
Sediment deposited as result of glacial erosion
Glacial sediments are usually poorly sorted and varied in size
Tillite
Sedimentary rock formed from glacial till
Transitional environments
Delta
Lagoon
Tidal flats
Beach
Deltas
Formed when rivers empty into larger bodies of water