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Varve
Evidence of lake presence
annual sediment layer: altering silt and clay
forms in any lake that freezes in the winter
the ice makes the water extra calm
melting season: summer layer: light colored silt, variable thickness
non-melting season: winter: dark colored clay, uniform thickness
Turbidity current
Underwater landslide
dense sediment laden flow driven by gravity
flow for considerable distances, slowing and dropping sediment only when they reach gentler slopes
Graded bedding
Results when a sediment laden current (like a flood) begins to slowdown
As transportation begins to slow down, smaller sediments deposit last
the grain size is larger at the bottom and finer at the top
Fossils
Preserved evidence of ancient organisms
indicate types of organisms of the time
Mud cracks
Wet mud dries and then shrinks and cracks
polygonal shape
form when clay/mud is wet, then dry
Indicative of
tidal flats
desert environments
river flood plain
Cross-beds or ripples
Indication of currents (wind or water)
if they are buried, may be preserved and form into rock
the shape/orientation can indicate speed or flow
symmetrical = beach
asymmetrical = rivers, desert, dunes
Glacial deposits
Polished, striated, grooved bedrock surface
striated and flattened cobbles
abrasion smooths rocks and shapes surface to make groves, striation
Dropstones
Stones dropped to the bottom of a lake or ocean from a melting body of ice afloat on the water surface
Glacial erratic
Glaciers can transport very large boulders, but when the glacier melts and recedes, these boulders are left behind
Clastic
Created from broken pieces of source rock from physical weathering
Chemical
Ions dissolved in water from chemical weathering
Biologic
Skeletal debris from organisms
Lithification
The making of a rock
compaction
cementation
Breccia
Base of mountains, angular, large
Conglomerate
In rivers or near mountains, rounded rock clasts
Sandstone
Sand-sized particles, clastic, quartz rich
beaches, deserts, rivers, lakes, deltas
Mudstone/shale
Fine clasts of silt and clay
found in slow water like tidal flats, lagoons, rivers, lakes
Biochemical
Derived from the shells of once-living organisms
deposited as they settle to the sea floor, lithifying
Limestone
Almost entirely calcite, commonly used to make seashells
preserves shells of fossil organisms
organic reefs, warm, shallow oceans
less than 4 km deep
Chert
Made of quartz derived silica, skeletons of certain plankton
deep sea environments deeper than 4km
Evaporites
Derives from evaporation of large volumes
halite and gypsum
Travertine
Precipitated from groundwater
cold springs, hot springs, lakes, caves
layered
Organic
Made of organic carbon and soft tissues
coal
swamps, wetlands