meandering rivers
not choked with sediment be
cause sediment is supplied to them slowly in relation to the
rate at which the water flows
point bar
the current is so weak
that sediment is deposited rather than eroded, and it accu
mulates there to form…..
floodplains
adjacent lowlands where fine settlement is caried to
backswamps
moist vegetated areas
natural levee
a gentle ridge made of sand and silt
Walther’s law
states that when depositional
environments migrate laterally, sediments of one envi
ronment come to lie on top of sediments of an adjacent
environment.
sedimentary cycles
composite units formed when a river migrates back and forth multiple times
delta
The depositional body of sand, silt, and
clay that is formed when a river empties into a body of water.
distributary channels
smaller channels that a larger channel branches into that radiate out into the mainland
barrier islands
composed largely of clean sand piled up
by waves
longshore currents
shallow currents that flow along the coast
Lagoons
lie behind long barrier islands
barrier
island–lagoon complex
A barrier island and the lagoon behind it
tidal flats
depositional environments formed of sand or muddy sand
tempestites
sandy beds that are usually a few
centimeters thick
stromatolites
knobby intertidal structures
sedimentary environments
a location at Earth’s surface that accumulates material through the movement of water, wind, ice, or by chemical process.
cross bed
sedimentary structures that indicate the direction of movement for material
sandstone
coarse, clastic, sedimentary rock
weathering
mechanical or chemical breakdown of rocks and minerals
erosion
removal of weathered material from its source
lithification
process of converting sediments to sedimentary rock
4 types of sedimentary rock
clastic
bits and pieces of pre-existing rock material