Rivers & Fluvial Environment Flashcards
have water in the channel throughout the year
perennial rivers
seasonal rivers
intermittent rivers
have water in the channel after heavy downpour of rains
ephemeral river
rivers in a arid regions
exotic rivers
rivers the loose water in the ground water
influent rivers
rivers that gained water in the ground water
effluent rivers
uncommon and forms in channel with steep gradients
straight rivers
characterized by wandering or meanders rivers that crosses a valley bottom, side to side erosion, fining upward
meandering rivers
characterized by broad channel with multiple sub channels and with eyots and sand bars, coarsening upward
braided rivers
consists of multiple interconnected channels that are separated by areas of a floodplain, high sand/mud ration
anastomosing rivers
streams whose course is a direct consequent of the original slope of the land
consequent river
river whose course have shifted from the original consequent ones
subsequent rivers
river whose course are controlled by factors which are not determinable, notable lack of structural lithologic control of their location
insequent rivers
streams flows opposite to the original consequent drainage
obsequent rivers
drain in the same direction as the original consequent drainage but are at lower topographic levels
resequent
irregular branching of tributary streams in many direction
dendritic pattern
a system of sub parallel streams, usually aligned along the strike of the rock formation
trellis pattern
mains stream and its tributaries display right angled bends
rectangular pattern
have ring like planes, found around dissected domes which have alternating bends of hard and soft rocks encircling them
annular pattern
marked by irregular stream courses which flow into and out of lakes and have only a few tributaries
deranged patteren
shows drainage line converging in to a central depression
centripetal pattern
streams diverging from a central elevated tract
radial pattern
found where there are steep slopes or structural controls which leads to regular spacing of parallel or near parallel streams.
parallel pattern
factors controlling sedimentation of lakes
lake size closed vs. open basin water chemistry amount of sediment entering the basin shape of basin regional tectonics depth of the basin water temperature wind
lakes with low salinity and low rate of dissolution of ions, can be either open or closed
freshwater lakes
lakes with high salinity and higher concentration of ions due to evaporation, hydrologically closed
saline lakes
lakes that occurs in arid regions, temporary lakes that form due to heavy rains
ephemeral lakes
oxygenated lake facies, displays evidence of wave or current processes, traces of plant fossils
epilimnic facies
finely laminated terrigenous biogenic and authigenic materials
hypolimnic facies
dessication cracks and evaporites
ephemeral facies
represents shallow or ramped margins
lake-shore facies