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How does ground water fit into the hydrologic cycle
massive underground reservoir that stores, moves and filters water
Belt of soil moisture
groundwater trapped in soil by molecular attractions
used by plants and animals
Zone of aeration
sediment and rock that contains water and air in the pores
pores: space between grains, contains belt of soil moisture
zone of saturation
sediment and rock that contain only water in the pores
upper limit of this zone
What is water table?
underground boundary between unsaturated soil surface and the saturated zone below
level based on rain, drought and pumping
highest under hills, lowest under valleys
Porosity
the total amount (%) of voids and openings between grains in sediment or rock
how much water can be stores
Permeability
the connectivity of pores in sediment and rock
how fast the water flows
Aquitard
impermeable layers that hinder flow of ground water
slow process
water moves through from pore or pore or through fractures
Aquifers
porous and permeable rock that transmit water freely
sand and gravel
Darcy’s Law
states how groundwater moved under the influence of elevation difference between the area of recharge and discharge (head)
Hydraulic gradient
slope of the water table
the greater the gradient, the faster is flows
Everglades Floridan Aquifer
loose sediment over limestone bedrock
series of aquifers and aquitards
water table is shallow or above ground
flow to south west
leads to caves and sinkholes
Everglades watershed
flowing from kissimmee river through lake okeechobee down to florida bay
Everglades problems
50% decline in wading birds, near extinction of florida panther, invasive species, decreased water quality
eroded limestone and decaying plant material
salt water invasion
fertile soil drying up
Speleothem
any secondary mineral deposit in caves
calcite or gypsum
flow stone
made by water flowing over a wall
stalagtites
made by water dripping from the cave ceiling
stalagmites
made by water dripping onto the cave floor
cave column
when stalactites and stalagmites grow into each other
helictites
irregular, twisted speleothems cave sediment, flowing water can deposit sediment in a cave
Mammoth Caves Native Americans
Used caves 3000-4000 years ago
Evidence: baskets, torches, petroglyphs, mummies
How did Mammoth caves form?
when acidic rainwater dissolves through the Mississippian limestone
Surface flow water draining into the caves, flow through and exits
water enters through sinkholes on the surface
How are caves related to ground water
caves are formed and shaped by groundwater
What are sinkholes?
a depression or hole in the ground caused by a collapse of the surface layer
usually when acidic water dissolves underlying bedrock like limestone, dolomite or gypsum
How are caves formed
chemical dissolution of limestone by acidic water over millions of years
carbon diozide gets absorbed by the water to make weak carbonic acid
Why are limestone and carbonate platforms important to the origin on caves?
soluble by mildly acidic water
ground water can dissolve the rock over millions of years
What are glaciers?
thick mass of ice that originates on land from the accumulation and compaction of snow
How do glaciers fit into the hydrologic cycle?
long term freshwater reservoirs
How do glaciers flow?
primarily gravity because of their immense weight
internal deformation and/or basal sliding
Zone of accumulation
zone where snow accumulates and ice is formed
Zone of wastage
zone where more ice is removed than added each year
Firn line/snow line
boundary between accumulation and wastage zones
glaciers flow in response to a balance between accumulation and wastage
how do glaciers pick up sediment?
Picking up rock at the base of mountains (plucking)
when trapped rocks grind the underlying surface (abrasion)
Alpine (valley) glaciers
relatively small glaciers that exists in the valleys of high mountains
Alaska, Alps, Himalayas, Pyrenees
Ice Sheets
great accumulations of ice that occur in polar regions
cover 10% of land today
Antarctica, Greenland
Ice Shelves
Large, flat extensions of ice sheets that float on oceans
U shaped valleys
wide, u shaped valleys created by alpine glaciers
Fjords
glacial valleys partially filled with sea water
Hanging Valley
valleys cut by smaller tributary glaciers that enter the main valley at a considerable height
Roche moutonnée
elongated hills of bedrock, eroded, scoured, and smoothes by glaciers
Glacier striations
“scrape marks” left on rocks from a glacier
Moraines
elevated ridges of sediment that are deposited at the sides and front of glaciers
End Moraine
Moraine deposited in front of a glacier
Ice sheet landscape
tend to smoothed the landscape by eroding high areas and filling in low areas
Till
unsorted, sediment deposited as glaciers melt
Stratified Drift
sorted and layered sediment deposited by flowing melt water
terminal moraine
outermost end moraine, marks advance of ice
Drumlin
asymmetric hills of till that were smoothed and elongates as ice moved over them
outwash plain
sediment laid down by melt water in front of glacier
kettles
little lakes or ponds on outwash plains
chunk of ice gets left behind by glacier, water flowed around it and deposited sediment to leave a hole
Eskers
rivers of water under the ice
has sediment too
erratic boulder
massive boulders transported and deposited by glaciers
Glacier Nat park history
Montana
natives lived here for many years
1892 tourists came from railroad built
1910 nat park established
Glacier nat park sed structures in belt supergroup
mudcracks, ripples, abundant stromatolites
mostly shallow marine for layers
Glacier park creatateous depositions
shallow sea flooded N.A.
thick shale deposits
mountain building in late cretacaous
ooids
small spheres of calcite, indicates shallow tropical marine water
Igneous sill
layer of unsolidified lava that was injected into the Helena Formation
Sheppard formation
glacier park, limestone and siltstone with mud cracks and ripples
lewis thrust
the rocks of the belt supergroup pushed over the cretaceous rocks
Glacier park sculpting
alpine glaciers in the last 2 my created most features in the park
gradual retreat over last 10k years
Ice ages
periods of time in which glaciers and ice sheets are more widespread than today
two causes of glaciations
plate tectonics: large landmasses at poles, large continents
orbital controls: variation of heat from sun, Milankovitch cycles
Carlsbad formation difference
the cavers were formed through sulfuric acid dissolutions, rather than typical carbonic acid
How is Carlsbad cave related to surface flow?
modern day seepage of rain and snow melt that drips into the cave
helps form stalactite and stalagmites
How was Yosemite valley found?
Natives in the area for millennium
gold rush and military conflicts led to settlers coming over
what are batholiths?
massive underground bodies of igneous rock formed by cooled magma
How are batholiths related to yosemite
major uplift and erosion in last 65 my
up to 6 km of rock eroded and batholiths were exposed
What did ice do in yosemite
glaciers form in valley 70k years ago
recede in last 10k years
some small mountain glaciers left
shaped features like half dome, yosemite valley and el capitan
Who were the first people in Acadia
red pain people several thousand years ago
other natives later
Portuguese find shoreline in 1529
french find this too and begin to trade
Acadia geological terrane
Avalonia terrane
Acadian orogeny shaped the park
second of three orogenies that made Appalachians
N.A. collided with Avalonia
sed rocks were metamorphosed and intruded by granite
How did waves and ice sculpt acadia
shaped by continental glaciation of igneous and metamorphic rock
waves modify the shoreline
what glacial features are preserved in acadia
maine rising since the ice lifted, since there is less weight
glacial erratics and till
cadillac mounted (rounded)