Chapter 1.3 Physical Environments - Rivers and Valleys Flashcards

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1
Q

A V-shaped valley is fromed when a

A

river erodes vertically by hydraulic action and corrasion.

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2
Q

The first step in the formation of a v-shaped valley is

A
  • A small valley begins to form, weatherng of the land besides the river produces loose pieces of soil and rock.
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3
Q

The second step in the formation of a v-shaped valley is

A
  • The soil and rock roll down the sides of the valley and into the river. The river then carries it away.
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4
Q

The third and final step in the formation of a v-shaped valley is

A

The beds and banks of the river are further eroded by rocks as they bounce and scrape along the river bed by corrasion.

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5
Q

If a river flows over hard rock and then over a band of soft rock, the soft rock will be worn away leaving the hard rock. This can lead to the formation of a

A

waterfall

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6
Q

The first part of the formation of a water fall begins: Water flows over areas of

A

hard and soft rock, eroding the soft rock more quickly by hydraulic action. Overtime the hard rock sticks out over the soft rock to form an overhang.

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7
Q

The second step in the formation of a waterfall is:

A
  • The Bottom of the waterfall has lots of energy so it erodes the soft rock even further by hydraulic action.
  • The water wears away a pluge ppol underneath the waterfall
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8
Q

The third step in the formation of a waterfall is:

A
  • Over time the overhang above the plunge pool becomes unstable and collapses.
  • The pieces of the heard rock help to erode the plunge pool further by corrasion and are themselves eroded by attrition.
  • The waterfall continues to move upstream forming a gorge.
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9
Q

A bend in a river is known as a

A

meander

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10
Q

Step 1 in the formation of a meander is:

A

The course of the river is not as straight as the upper course so the river flows towards the outer bank.

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11
Q

Step 2 in the formation of a meander is:

A
  • The river’s energy is concentrated on the outer bank so by hydraulic action and corrasion it is able to erode the bottom of the bank.
  • Over time the bank will collapse forming a steep slope called a river cliff.
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12
Q

Step 3 in the formation of a meander is:

A
  • On the opposite inner bank the river is much slower it has little energy so deposits some of its load to form a river beach. (deposition)
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13
Q

Step 4 in the formation of a meander is:

A
  • Over time the bend becomes more pronounced and is called a meander.
  • The river is also eroding sideways (lateral erosion) and widens the valley.
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14
Q

Step 1 in the formation of an oxbow lake is:

A
  • The river continues to erode at the outer banks of the meander until the neck of land between them becomes very narrow
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15
Q

Step 2 in the formation of an oxbow lake is:

A
  • During a flood when the river has more energy it cuts through the neck and makes a new straighter channel
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16
Q

Step 3 in the formation of an oxbow lake is:

A
  • The meander becomes cut off from the new course of the river and is left as an ox-bow lake. Without a water supply it soon dries up.
17
Q

Step 1 in the formation of a levee is:

A
  • When floodwaters spread across the floodplain the spread of the water slows and is no longer able to transport sediment
18
Q

Step 2 in the formation of a levee is:

A
  • As a result coarser sediments such as sand and gravel are deposited at the channel edge, gradually building up into natural ridges or levees after successive floods.
19
Q

Step 3 in the formation of a levee is:

A
  • Levees act like natural embankments and are often strengthened as part of flood rpevention measures.
20
Q

The floodplain is the area of

A
  • allurial (sand&Silt) deposits found beside the river in its lower course.
  • When the river floods it deposits the alluvium.
  • The smallest particles found at the edge of the floodplain and the largest next to the river.
21
Q

Braiding is the process by which rivers

A

divide into seperate channels through material being deposited by the river mid-stream.

22
Q

An estuary is the mouth of a

A

river where it meets the sea

23
Q

A u shaped valley is a valley with very

A

high, steep sides and a wide flat bottom formed by a glacier flowing through the original valley.

24
Q

On a map a v-shaped valley can be indentified because the contour lines go

A

right up to the edge of the river

25
Q

Tributaries are

A

small streams that join onto the main river

26
Q

A confluence is the point where a

A

tributary meets the main river