Landforms and Bodies of Water, Exogenic Processes Flashcards

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1
Q

A natural stream of water flowing in a channel to the sea, a lake, or another stream

A

River

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2
Q

An area of land that rises very
high above the land around it
and that is higher than a hill

A

Mountain

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3
Q

An area covered with sand or
small rocks that is next to an
ocean, sea, or lake

A

Beach

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4
Q

A large body of saline water
that separates continents

A

Ocean

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5
Q

An opening on the earth’s crust where pyroclastic
materials, lava, and gases come out

A

Volcano

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6
Q

Why do we have different landforms and bodies of water?

A

There are forces and processes that shape and change the structure of the earth and lead to the formation of these wonders.
- exogenic and endogenic processes

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7
Q

events that occur on the surface of the earth
- affected by external factors like solar energy (wind, water, etc.) and subsystems
- weathering, erosion, deposition, and sedimentation

A

Exogenic Processes

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8
Q

Events that are caused by the movement of materials in the Earth’s inner layer
- driven by Earth’s internal heat (geothermal energy)
- plate movement, magmatism, earthquakes, metamorphism, diastrophism

A

Endogenic Processes

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9
Q

the breaking down & changing of rocks as a result of exposure to the environment

A

weathering

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10
Q

Types of Weathering

A
  • Physical/Mechanical - processes that break a rock or mineral into smaller pieces without altering its composition
  • Chemical - accompanied by changing their chemical composition
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11
Q

Examples of Physical Weathering

A
  • Exfoliation
  • Frost Wedging
  • Abrasion
  • Plant/Root Wedging
  • Animal and Human Activities
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12
Q

Cracking and peeling of the upper/outer rock
layers because it is weakened by:

  • thermal expansion and contraction - repeated heating and cooling of materials cause rigid substances to crack and separate
  • removal of overlying rocks - rocks underneath get exposed; there is less pressure on them, and they
    expand. This causes the rigid layers to crack and sections to slide off
A

Exfoliation

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13
Q

cracking of rock mass by the expansion of water as it freezes in crevices and cracks

A

frost wedging/action

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14
Q

frost wedging in soil

A

permafrost

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15
Q

why does water expand when it freezes

A

When frozen, water molecules take a more defined shape and arrange themselves in six-sided crystalline structures. The crystalline arrangement is less dense than that of the molecules in liquid form which makes the ice less dense than the liquid water. When water freezes, the volume expands by approximately 9%.

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16
Q

Moving sediments or rock sections can break off
pieces from a rock surface they strike.
- The sediments can be moved by wind (in the desert), water, or ice, and the large rock sections by gravity.
- can be both weathering and erosion

A

Abrasion

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17
Q

As plants such as trees send out root systems,
the fine roots find their way into cracks in the
rocks. As the roots increase in size, they force the rock sections apart, increasing the separation and weathering.

A

plant/root wedging

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18
Q

how do human and animal activities cause physical weathering

A
  • Some animals burrow themselves
    on the ground.
  • Mining, construction, and
    agriculture
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19
Q

Examples of Chemical Weathering

A
  • Oxidation
  • Carbonation
  • Hydrolysis
20
Q

Water mixes with carbon dioxide and forms carbonic acid. This dissolve minerals like limestone and calcite.

A

Carbonation/Leeching/Solution (uniform and dissolved)

21
Q

Water mixes with carbon dioxide and forms carbonic acid. This dissolved minerals like limestone and calcite.
- results to the formation of majestic limestone
features in caves (stalagmites and
stalactites) and beaches, as well as, the development of dangerous sinkholes.

A

Carbonation/Leeching/Solution (uniform and dissolved)

22
Q

a type of rock formation that rises from the floor of a cave due to the accumulation of material deposited on the floor from ceiling drippings.

A

stalagmite

23
Q

an icicle-shaped formation that hangs from the ceiling of a cave and is produced by the precipitation of minerals from water dripping through the cave ceiling

A

stalactite

24
Q

Minerals may combine with oxygen to form
new minerals that are not as hard.

  • When iron is exposed to oxygen forming iron oxide
  • pyrite to limonite
A

Oxidation

25
Q

When minerals chemically react with water to form new minerals. The newly formed minerals are not as hard as the original material

-Water splits the ion of the mineral usually resulting in clay, acidic solution, and
free ions or salts.
- feldspar to kaolinite (source of clay)
- silicate rich minerals

A

Hydrolysis

26
Q

Factors affecting Weathering

A
  • climate
    a. hot and dry - less weathering (some wind abrasion)
    b. hot and moist - more weathering (strong)
    c. colder - frost action (more if more water)
  • mineral hardness - harder, less quick
  • surface area - how much of an area is going to be exposed
    e.g.sugar granules vs. sugar cubes
27
Q

These water compositions enable what kind of weathering

  • alkaline (>7)
  • acidic (<7)
  • w/ dissolved salts
A
  • hydrolysis
  • carbonation (carbonic acid)
  • oxidation
28
Q

the transportation of sediments that have been broken down by weathering
- Removal of rocks, sediments, and soil from their original location
- Usually occur after or together with weathering

A

erosion

29
Q

Agents of Erosion (different processes that move sediments)

A
  • gravity (mass wasting/movement)
  • water
  • wind
  • ice/glaciers
30
Q

What is it called when gravity moves sediments downhill

A

mass wasting/mass movement

31
Q

erosion by gravity can be classified according to

A

speed, materials involved, and type of movement

32
Q

mass movement

gradual downhill movement of soil
- slowest and most tame
- can take for weeks, months, years, decades, etc.)

A

soil creep

33
Q

mass movement

gradual downhill movement of soil
- slowest and most tame
- can take for weeks, months, years, decades, etc.)

A

soil creep

34
Q

mass movement

the rapid downslope flow of debris (anything)

A

debris flow/landslide

35
Q

mass movement

the downward flow of fine particles (mud) & a large amount of water
- often associated with storms and rains
- fairly quick
- can engulf entire villages and communities

A

mud flow/slide

36
Q

mass movement

  • rapid falling of pieces of rocks from cliffs/steep slope
  • violent
  • solution - wrecking loose rocks off for control using wrecking ball
A

rock fall/slide

37
Q

rock = ?
small rocks + big rocks = ?
small rocks + big rocks + plants = ?

A

rock
regolith
debris

38
Q

difference of slide, fall, creep, flow

A

slide - move along a smooth surface while maintaining continuous contact with it (on a slope, leaves scar)
fall - move downward, typically rapidly and freely without control, from a higher to a lower level.
creep - slow
flow - with water

39
Q

erosion by water

(Can happen during surface run-off or along the surface of riverbeds and/or sea floors)

A

surface run-off
- sheet erosion
- venous/stream flow erosion
- stream bank erosion

river transport systems/stream load
- traction (rolling of big rocks = smooth)
- saltation (bounce, smaller sediments)
- suspension (float, fine/light sediments)
- solution (dissolved, soluble materials)

40
Q

erosion by water through surface run-off

occurs as a shallow ‘sheet’ of water flowing over the ground surface, resulting in the removal of a uniform layer of soil from the soil surface. (even removal of upper layers)

A

sheet erosion

41
Q

erosion by water through surface run-off

  • creates a channel
  • small - rill
  • big - ephemeral
  • too big - gully
  • areas where rocks and soils have less resistance to water
A

venous/stream flow erosion

42
Q

erosion by water through surface run-off

a natural process that occurs when the forces exerted by flowing water exceed the resisting forces of bank materials and vegetation.

A

streambank erosion

43
Q

erosion by wind

A
  • creep (roll, big rocks)
  • saltation (bounce, smaller sediments)
  • suspension (float, fine/light sediments)
44
Q

erosion by ice/glacier (nature’s bulldozer)

(thick deposition if new)

A
  • freeze-thaw (frost wedging)
  • plucking (removal)
  • abrasion (scraping by moving rocks)
  • transportation (downward movement)
  • deposition (collection of rocks at the bottom of the hill/mountain)
45
Q

the sediment deposited by a glacier. It blankets glacier forefields, can be mounded to form moraines and other glacier landforms, and is ubiquitous in glacial environments.

A

glacial till

46
Q

the dropping off of sediments that have been weathered and eroded

A

deposition