Earths Interdependent systems - Princeton Ch 4 Flashcards

1
Q

Rift volcanoes

A

Occur when plates move away from each other. When a rift volcano erupts, new ocean floor is formed as magma fills in where the plates have separated

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2
Q

Subduction volcanoes

A

Occur where plates collide and slide over each other

A heavy ocean plate is pushed below the other and melts as it encounters the big mantle

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3
Q

Hot spot volcanoes

A

Do not form at the margin of plates.

Found over “hot spots” which are areas where magma can rise to the surface through the plates. (Ex. Hawaiian islands)

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4
Q

How old is the earth

A

Between 4.5 and 4.8 billion years old

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5
Q

What three things interact in the rock cycle and to create basic rocks

A

Time, pressure, and the earth’s heat

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6
Q

This type of rock results when rock is melted (by heat and pressure below the crust) into a liquid and then resolidifies. The molten rock (magma) comes to the surface of the earth, and when it emerges it is called lava; solid lava is this type of rock. Another example is basalt.

A

Igneous

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7
Q

These rocks are formed as sediment (eroded rocks and the remains of plants and animals) builds up and is compressed. One place this can occur is at a subduction zone where ocean sediments are pushed deep into the earth and compressed by the weight of rock above it. An example is limestone.

A

Sedimentary

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8
Q

This type of rock is formed as a great deal of pressure and heat is applied to rock. This can happen as sedimentary rocks sink deeper into the earth and are heated by the high temperatures found in the earth’s mantle. An example is slate. (The product of shale)

A

Metamorphic

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9
Q

Three soil categories from compact particle size to large pores (that can hold more water and don’t easily stick together)

A

Clay, silt, sand

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10
Q

As soil pH gets more _____, ions of heavy metals such as Hg or Al can leach into the ground water and harm plant and aquatic life.

A

Acidic

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11
Q

Soil Layers

A
OAEBCR
O horizon
A horizon
E horizon
B horizon
C horizon
R horizon
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12
Q

O horizon

A

Uppermost horizon; organic material (organism waste, decomposing organism, live organisms); humus

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13
Q

A horizon

A

Weathered rock and some organic material that has traveled down
Topsoil
Zone of leaching

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14
Q

E horizon

A

Eluviated horizon
leached of clay, iron, or aluminum oxides
Sand and silt sized minerals

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15
Q

B horizon

A

Relieved minerals leached out of the A horizon and organic materials
Zone of illuvation (the movement of dissolved material from higher soil layers to lower soil layers due to the downward movement of water caused by gravity)

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16
Q

C horizon

A

Bottommost layer of soil composed of larger pieces of rock that have not undergone much weathering

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17
Q

R horizon

A

Bedrock, below all other layers of soil

18
Q

Loamy

A

Soil composed of roughly the same amount of all three textures (clay, silt, sand)
Best for plant growth

19
Q

Problems of monoculture and prevention

A

Significant decrease in genetic diversity makes crops more susceptible to pests and diseases
Consistent planting of one crop in an area eventually leaches the soil of specific nutrients that the plant needs to grow
Prevention: crop rotation (diff crops are planted in the area in each growing season)

20
Q

Detrimental effects of the green revolution

A

Chemical pesticides result in insects that are pesticide resistant
Over irrigated soils undergo salinization which leads to land degradation

21
Q

Salinization

A

Soil becomes water-logged and when it dries out, salt forms a layer on its surface

22
Q

Erosion has increased significantly caused by humans results from

A

Logging and slash and burn agriculture (deforestation)
Over cultivation of agricultural fields
Overgrazing
Urbanization

23
Q

Best management practices to conserve soil

A

Use of animal waste (manure), compost, and the residue of plants to increase organic matter in soil
Organic agriculture, compost, manure, crop rotation, non-chemical methods
Contour plowing and strip planting
Trees and other wind barriers

24
Q

Soil conservation act of 1935

A

Created the soil conservation service. Passed in response to the dust bowl. Created to conserve soil and restore the nation’s ecological balance. Was led by Hugh Hammond Bennett.

25
Q

Soil and Water Conservation Act of 1977

A

Soil and water conservation programs to aid landowners and users; also sets up conditions to continue evaluating the condition of US soil, water, and related resources

26
Q

Food Security Act (1985)

A

Nicknamed the Swampbuster, this act discouraged the conversion of wetlands to nonwetlands. 1990 federal legislation denied federal farm supplements to those who converted wetlands to agriculture, and provided a restoration of benefits to those who converted lands to wetlands.

27
Q

Layers of Atmosphere (from closest to earth to farthest)

A

Troposphere
Stratosphere
Mesosphere
Thermosphere (Ionosphere)

28
Q

Epilimnion

A

The uppermost, and thus the most oxygenated layer of freshwater

29
Q

Hypolimnion

A

The lower, colder, and denser layer of freshwater

30
Q

Thermocline

A

The line between the epilimnion and hypolimnion, at which the temperature shifts dramatically

31
Q

Littoral zone

A

Begins with the very shallow water at the shoreline. Plants and animals that reside in the littoral zone receive abundant sunlight. The end of this zone is defined as the depth at which rooted plants stop growing.

32
Q

Limnetic zone

A

Surface of open water; the region that extends to the depth that sunlight can penetrate. Organisms that are residents in this zone are short lived and rely on sunlight to carry out photosynthesis

33
Q

Profundal zone

A

Water that is too deep for sunlight to penetrate. Because the Profundal zone is an aphotic zone (a zone that light cannot reach), photosynthesizing plants or animals cannot live in this region

34
Q

Benthic zone

A

The deepest layer in a body of water; characterized by very low temperatures and low oxygen levels.

35
Q

Coastal zone

A

This zone consists of the ocean water closest to land. Usually it is defined as being between the shore and the end of the continental shelf.

36
Q

Euphotic zone

A

The photic, upper layers of water. The euphotic zone is the warmest region of ocean water; this zone also has the highest levels of dissolved oxygen

37
Q

Bathyal zone

A

The middle region of ocean water; this zone receives insufficient light for photosynthesis and is colder than the euphotic zone

38
Q

Abyssal zone

A

This is the deepest region of the ocean. This zone is marked by extremely cold temperatures and very low levels of dissolved oxygen, but very high levels of nutrients because of the decaying plant and animal matter that sinks down from the zones above.

39
Q

Bioaccumulation

A

Fat-soluble molecules accumulate and stay in the fatty tissues of animals since they can not dissolve in water

40
Q

Bio magnification

A

Compounds are passed from prey to predator. Since a predator needs to eat a lot of prey, each of the prey organism gives some of the compound to the predator. The compounds accumulate and the concentration becomes much higher than you would expect to be in the environment