Final Exam Flashcards
the amount of uniformity in the size of rock particles
sorting
Finger lakes form where ___.
moraines block existing streams
What affects the depth of the water table below ground?
surface topography,
permeability of the aquifer,
rainfall
the area where water from the surface can move through permeable rock to reach an aquifer
recharge zone
What are two land features formed by hot groundwater?
geysers & hot springs
the aquifer zone that lies between the water table and the Earth’s surface
zone of aeration
How are wells, springs, and artesian formations similar?
All bring groundwater to Earth’s surface.
A cavern is a natural cavity in rock that forms as a result of ___.
dissolution of minerals
What affects the flow of groundwater through an aquifer?
porosity,
gradient,
permeability
Open spaces in rock must be connected in order for the rock to be ___.
permeable
Pumping water from a well causes a ___.
cone of depression
calcite formations standing on the floor of a cavern
stalagmites
What formation could be produced by hot springs when water mixes with sediment?
mud pot
uncollapsed rock between sinkholes can form arches
natural bridges
Which features are all produced by glacial erosion?
cirque, arête, horn
What is a continental glacier?
A mass of ice that is not confined by local topography.
What are all formed by glacial deposition?
erratic, till, glacial drift, moraine, drumlin
How can an iceberg be formed?
tidal action that breaks a large block of ice from an ice shelf
What explanation is the cause of glacial periods according to the Milankovitch theory?
cyclical changes in Earth’s movement relative to the sun
a bowl-shaped depression in a glacial drift deposit
kettle
the natural steepness of a slope
gradient
the process by which glaciers flow slowly as grains of ice deform under pressure and slide over each other
internal plastic flow
a sloping layer of permeable rock sandwiched between two layers of impermeable rock
artesian formation
the process by which a glacier slides due to the melting of ice at its base
basal slip