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1 inch
2.54 cm
1cm
10mm
shape of earth
oblate spheroid
1 m2
10,000 cm2
1 ft
0.3048 m
ocean covers what
70% earth
The time scale based on the history and formation of the Earth is referred to as
geologic
The largest reservoir, by volume, of water on the Earth is:
oceans and sea ice
The mean depth of the ocean is approximately:
3800 meters
how many major ocean basins
5
The distance between the center of the Earth and the equator is___ than the distance between the center of the Earth and the north pole.
greater
Plates move horizontally past each other along:
transform faults
The reservoir size for water in the atmosphere is ______ than the reservoir size of water in the oceans.
greater (2)
Hot spots and their volcanic island chains can be used to trace the movement of oceanic lithosphere
true
Continental crust is thicker and denser than oceanic crust
False
Oceanic crust
cools and becomes more dense
latitude
parallel from equator
longitude
right angle to the latitude
0 degrees
equator
90 degrees N
North pole
90 degrees S
South pole
23.5 degrees N&S
tropic of Cancer and Capricorn
66.5 degrees N&S
Artic and Antarctic circle
Residence time formula
volume/flow rate
water budget
Takes 38,000 years to evaporate the volume of the oceans, pass it through the atmosphere to the land and back to the oceans
5 major ocean basins in order of size
Pacific, Atlantic, Indian, Artic, South
P waves
compressional, first to arrive, solid, liquid, gas (104-140 degree)
S waves
shear, second to arrive, solid (104-180 degree)
avg density of the whole planet
5.51 g/cm³
Lithosphere
Crust and upper material fused together
Asthenosphere
deformable region in the mantle
mesosphere
solid lower layer of the mantle
isostacy
buoyant support of lithosphere by asthenosphere
Physiographic mapping revealed what?
underwater mountain ranges
trenches
narrow and steep sided, 6k-11k deep
divergent boundaries
mantle upwelling, layers of oceanic crust
convergent boundaries
subduction, thickness and age of oceanic crust, associated with volcanic activity
transform boundaries
offset segments of ocean ridges, changes in speed and direction, can joint up different combos of divergent and convergent boundaries.
topographic relief
variation of elevation across a landscape