U2L2 Flashcards

1
Q

how does wind speed affect the movement of sediment?

A
  • wind erodes soil, sand, and rock particles
  • stronger wind allows it to carry more/larger sediment pieces
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2
Q

define desert pavement and explain its formation

A

rocky ground that forms when wind carries soil and fine sediment away leaving only pebbles and small rocks behind

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3
Q

define dune

A

mound of wind-deposited sand common in deserts and on shores of lakes and oceans

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4
Q

define loess

A

thick deposits of windblown, fine-grained sediment that forms fertile soil for growing crops

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5
Q

how is a glacier formed?

A

snow is compacted and turns to ice, forming a large mass of moving ice

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6
Q

how do glaciers shape the land?

A

gravity pulls them downhill and they cause erosion, scraping into the ground
when a glacier melts, it releases glacial drift (the material it’s carrying)

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7
Q

describe the processes of erosion and deposition by gravity

A

gravity influences the movement of water and ice and pulls rocks and soil downslope

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8
Q

define mass movement

A

shifting of material due o gravity

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9
Q

define creep

A

the extremely slow movement of material downslope

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10
Q

define rockfall

A

loose rocks falling down a steep slope

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11
Q

define landslide

A

sudden and rapid movement of a large amount of material downslope

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12
Q

define mudflow

A

a rapid movement of a large mass of mud

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13
Q

define abrasion

A

The grinding and wearing down of rock surfaces by other rock or sand particles

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14
Q

define deflation

A

The removal of fine sediment by wind

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15
Q

what depositional pattern was formed in the Moving Sediment experiment?

A

alluvial fan

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16
Q

connect each step of the scientific method to part of James Balog’s Chasing Ice experiment.

A

problem: glaciers are melting & people are unaware
gather information: he took photos of different glaciers over a few years
hypothesis: glaciers are melting faster than ever before
experiment: compare glacier melting rates & evidence to glacier history
collect & analyze data: analyze how current melting is faster than historic melting
conclusion: glaciers are melting too quickly and ocean levels are rising