Hydrogeology and Meteorology Flashcards
Streams whose course is controlled by the initial slope of land surface
a. Consequent Stream
b. Insequent Stream
c. Subsequent Stream
d. Resequent Stream
e. Obsequent Stream
Consequent Stream
Streams whose course is dependent on structures and not on topography.
a. Consequent Stream
b. Insequent Stream
c. Subsequent Stream
d. Resequent Stream
e. Obsequent Stream
Subsequent Stream
Streams that develop on flat or structureless rocks.
a. Consequent Stream
b. Insequent Stream
c. Subsequent Stream
d. Resequent Stream
e. Obsequent Stream
Insequent Stream
Streams that develop in response to a new base level and flows in the same direction as the main consequent stream.
a. Consequent Stream
b. Insequent Stream
c. Subsequent Stream
d. Resequent Stream
e. Obsequent Stream
Resequent Stream
Stream that flow in the opposite direction of the consequent stream.
a. Consequent Stream
b. Insequent Stream
c. Subsequent Stream
d. Resequent Stream
e. Obsequent Stream
Obsequent Stream
A measure of a stream’s ability to transport particles based on size
Competence.
The largest river in the world.
Amazon (Drainage: 5,778,000 km2 Discharge: 212,400 cm3/s)
Irregular branching of tributary streams that develop whenever underlying bedrock is relatively uniform, thus forming a pattern influenced by the topography.
a. Dendritic
b. Parallel
c. Trellis
d. Rectangular
Dendritic
A right-angled pattern in which tributary streams are nearly parallel to one another which typically forms in areas underlain by alternating bands of resistant and lesser resistant rocks.
a. Dendritic
b. Parallel
c. Trellis
d. Rectangular
Trellis
A right-angled pattern that develops where the bedrock is crisscrossed by a series of joints.
a. Dendritic
b. Parallel
c. Trellis
d. Rectangular
Rectangular
Pattern that form on areas with pronounced slope to the surface and are also observed on areas with elongated platforms such as resistant rock bands.
a. Dendritic
b. Parallel
c. Trellis
d. Rectangular
Parallel
Streams pattern where streams diverge from a central area.
Radial
Stream pattern where streams flow radially inward into the center.
Centripetal
Stream pattern evolved through the disturbance of an existing drainage system, initially adopting a dendritic pattern that undergoes alteration when overrun by glacial activity.
Deranged
Drainage pattern characterized by a tributary crossing a stream that flows the opposite direction while retraining the original current’s flow.
Barbed
A small glacier that exists in lofty mountain areas and moves a few centimeters per day.
Valley Glacier
Large scale valley glaciers that can flow out in all directions.
Ice Sheet
A mass of ice covering uplands and plateaus. Has an area of less than 50,000 km2.
Ice Caps
Glaciers that occupy broad lowlands at the bases of steep mountains and form when one or more valley glaciers emerge from confining walls.
Piedmont glacier
A method that accelerates and increases the amount of rainfall by adding ice nuclei to supercooled clouds.
Cloud Seeding
A geologic formation, which can absorb water but cannot transmit significant amounts.
Aquiclude