esocean Flashcards

1
Q

Wegener’s continental drift theory findings:

A

fit of continents
matching of rock units across ocean basins
distribution of fossils
paleoclimate evidence

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
2
Q

the study of the “beds” or “floors” of water bodies. foundation of the science of hydrography

A

Bathymetry

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
3
Q

bathymetry refers to:

A

the ocean’s depth relative to sea level,
although it has come to mean “submarine topography”, or the depths and shapes of
underwater terrain

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
4
Q

methods of measuring ocean depth

A

sounding line, echo sounding, satellite altimetry

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
5
Q

method of weighted rope lowered overboard until it touched the ocean
bottom; this old method is time-consuming and inaccurate

A

sounding line

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
6
Q

sonar is used by emitting high frequency sound and listening of the echo from the seafloor. deeper water means longer time for the echo to reach the receiver

A

echo sounding

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
6
Q

profiles the shape of the sea surface by measuring the travel time of a radar pulse from a satellite to the ocean surface and back to the receiver. the shape of the sea surface approximates the shape of the sea floor

A

satellite altimetry

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
7
Q

evidences of seafloor spreading

A

distribution of seafloor topographic features
sediment thickness
composition of oceanic crust
high heat flow along mid-ocean ridge axes
distribution of submarine earthquakes
magnetic stripes on the seafloor
deep sea drilling results

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
8
Q

contemplated that oceans grew from their centres, with molten material
(basalt) oozing up from the Earth’s mantle along the mid ocean ridges, this created new
seafloor which then spread away from the ridge in both directions. one of the “founding fathers” of the unifying theory of plate tectonics.

A

Harry Hammond Hess

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
9
Q

two types of lithospheric crust

A

continental and oceanic crust

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
10
Q

thickness of continental and oceanic lithosphere

A

continental: 150km
oceanic: 100km

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
11
Q

what is plate tectonic theory

A

proposes that the lithosphere is made up of seven large plates and numerous smaller segments. These plates rest upon the soft layer of asthenosphere. They move relative to each number.

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
12
Q

3mmain types of plate boundaries

A

Divergent, Convergent, Transform Boundaries

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
13
Q

two plates are moving apart

A

divergent boundary

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
14
Q

two plates are colliding

A

convergent boundary

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
15
Q

plates slide past each other

A

transform boundary

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
16
Q

what is the wilson cycle

A

Plate tectonics is cyclic. In 1966, John Tuzo Wilson proposed a cycle that includes continental break-up, drifting, collision and re-assembly of the continent

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
17
Q

main phases of the wilson cycle

A
  1. Rifting within the supercontinent leads to the opening of new ocean basin and formation of oceanic crust
  2. Passive margin cools and sinks, and sediment accumulate along the edge.
  3. Convergence begins, initiating subduction and eventual ocean closure.
  4. Continent-continent collision forms the next supercontinent.
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
18
Q

driving force for plate motion

A

convection in the mantle
gravity driven mechanisms (slab-pull, ridge-push)

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
19
Q

percentage of ocean basin on the planet’s surface

A

70%

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
20
Q

two characteristics of oceanic basin landform:

A

land that exists under the ocean
land that includes all topographical features

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
21
Q

structures of ocean basins

A

mid-oceanic ridge
ocean trenches
abyssal hill/plain
seamounts
guyot
continental rise
continental shelf
continental slope

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
22
Q

structure normally found rising above the ocean floor at the center of the ocean basins

A

mid-oceanic ridge

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
23
Q

long narrow, steep-sided depressions that
contain the greatest depths in the ocean.

A

ocean trenches

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
24
found on the deep ocean floor. are so flat because they are covered with sediments that have been washed off the surface of the continents for thousands of years.
abyssal hill(found deep) abyssal plain(flat)
25
These features can be very large submerged volcanic mountain reaching heights up to 10,000 feet
seamounts
26
similar to a seamount, but it is submerged volcanic mountain with a flat top
guyot
27
s feature found gently sloping area before the ocean floor and at the base of the continental slope and formed by emerging accumulates deposits at the mounts of many submarine canyons
continental rise
28
a shallow, gently sloping part of the continent crust.
continental shelf
29
This part of the ocean basin extends and slopes after the continental shelf. The boundary between the continental slope and shelf
continental slope
30
three major provinces of ocean basins
continental margins deep-ocean basins oceanic or mid-oceanic ridges
31
five ocean basins from largest to smallest
Pacific, Atlantic, Indian, Southern and Arctic
32
includes any change in position, shape/volume of a rock in response to stress
rock deformation
33
force per unit area applied on rock layers. causes strain on rock layers.
stress
34
change in shape or volume of the rock that has undergone stress
strain
35
is not just a function of the amount of stress but also relates to the area over which the force is applied.
magnitude of stress
36
stages of deformation
elastic deformation ductile deformation fracture deformation
37
stage of deformation when the strain is reversible, the material returns to its original shape once the stress that deforms it is removed
elastic deformation
38
occurs when the strain is irreversible – rock layers/material respond to stress by bending or deforming without breaking.
ductile deformation
39
irreversible strain wherein the materials break because they are mostly brittle.
fracture deformation
40
material composition and factors that affects the brittle-ductile transition
temperature confining pressure rate of strain
41
low temperature low confining pressure high rate of strain
increases brittleness of rock
42
high temperature high confining pressure low rate of strain
increase ductile properties of rock
43
formed when rock layers or materials are deforming plastically under compressive stress, most of these materials do not return to their original shape.
folds
44
types of folds
monocline anticline syncline overturned
45
type of fold that occurs when there is a simple bending of rock layers so that they are no longer horizontal.
monocline
46
occurs when a fold bends upward.
anticline
47
occurs when a fold bends downward.
syncline
48
axial plane inclined to such an extent that the strata on one limb are overturned.
overturned
49
occur when too much stress is applied to rock layers.
faults
50
is the energy released during the movement of faults.
earthquake
51
distance that rocks move sideways a fault. can be up or down the fault plane which is relative since there is usually no way to know whether both sides moved or only one.
slip
52
angle that faults lie to the horizontal of the surface of the Earth.
dip
53
type of faults
dip-slip faults (normal fault-reverse fault) strike slip fault oblique slip fault
54
this type of fault is when the fault’s dip is inclined relative to the horizontal surface
dip-slip fault
55
when the hanging wall drops down relative to the footwall
normal fault
56
when the footwall drops down relative to the hanging wall.
reverse fault
57
are the vertical fractures where the blocks have mostly moved horizontally.
strike slip fault
58
fault which has components of dip-slip and strikes slip.
oblique slip fault
59
any process or phenomena associated with the discharge of molten rock, pyroclastic fragments, or hot water and steam, including volcanoes, geysers, and fumaroles.
volcanism/vulcanism
60
a landform that resembles a mountain with an opening (vent) where magma, lave, ash, gasses, etc. are being released.
volcano
61
Area in the Circum-Pacific where most of the world’s active volcanoes are found.
Pacific Ring of Fire
62
mafic to intermediate intrusives
plutonism
63
mafic to intermediate extrusives
volcanism
64
materials released during volcanic eruption
gasses (water vapor, CO2, toxic gases such as carbon monoxide, sulfur dioxide, hydrogen sulfide and hydrochloric acid) liquid(lava) solid/pyroclastics (volcanic blocks, cinders lapilli, volcanic ash, volcanic dust)