Geography Theme 2 Flashcards

1
Q

Characteristics of a river:

A
  • width
    -depth
    -speed of flow
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2
Q

The hydrological cycle

A

-the hydrological cycle is a closed (no inputs and no outputs) system
-water is constantly recycled through the system
- within the hydrological cycle, there are stores and transfers (flows)

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3
Q

Go to photos and do the activity

A

1,precipitation
2,condensation
3,evapotranspiration
6, overland flow
7,infiltration
8,percolation
9,throughflow
10,evaporation
11,groundwater flow

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4
Q

Explain : Precipitation

A
  • Any form of water, such as rain, snow, sleet, or hail, that falls to the earth’s surface
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5
Q

When can precipitation only happen?

A

-when the air is saturated
-there is a nucleus to form around =for heavy drops
-temperature below dew point

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6
Q

State the three types of precipitation

A
  • cyclonic (frontal)
    -orgraphic (relief)
    -conventional
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7
Q

Evaporation

A
  • is the process by which a liquid or a solid is changed into a gas.
    -Evaporation increases under warm, dry, windy conditions
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8
Q

Factors of evaporation (7)

A

-temp= if hotter evaporation will increase
-humidity
-wind speed= the higher, the more evaporation decreases because wind blows water vapour
-water quality= the clearer and fresh the more evaporation
-depth of water = shallow+wide surface are the more evaporation
-size of water body
-vegetation cover

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9
Q

Interception

A

-water intercepted and stored by vegetation
- There are 3 main components, ways of interception; interception loss, through fall,

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10
Q

Explain the three main ways of intercepting

A

1, interception loss= water that is held by a plants surface—> later evaporated/absorbed by plant
2,throughfall= water that falls through Thais I’m vegetation/ drops from leaves
3,stemflow= water that twinkles along twigs+branched down to the trunk

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11
Q

Evapotranspiration

A

-combined effects of evaporation and transpiration
-water moves outside, plant down a concentration gradient
-most important aspect of waterloss

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12
Q

Infiltration

A

-process which water soaks into the ground, soil layer

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13
Q

What’s the infiltration capacity

A
  • is the maximum rate at which rain can enter the soil/ground.
    -it varies according to time raining, type of soil, how often vegetation occurs…..
  • infiltration capacity decreases with time through a period of rainfall
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14
Q

Percolation

A
  • it happens one infiltration happened
    -it’s the downwards movement of water from the soil to the rock beneath
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15
Q

Surface runoff- overland flow

A

-water moving over the surface

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16
Q

When does surface runoff occur?

A
  • when soil becomes saturated
  • precipitation exceeds infiltration rate
    -Impermeable soil rock
    -high suspended flow
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17
Q

Throughflow

A

-water flowing through the soil, on natural pipes and between soil horizons

-once infiltration happens= water flows downhill through soil

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18
Q

Groundwater flow

A

-subsurface water in soil
-once infiltration happens= water flows slowly through rock towards the sea

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19
Q

Characteristics of a river and drainage basin
-source

A

The place where a river begins

20
Q

Tributary

A

A small river that joins the large river

21
Q

Confluence

A

The point where the tributary joins the main river channel

22
Q

Mouth

A

The point where the river enters the sea

23
Q

Estuary

A

The part of the mouth that is tidal

24
Q

Watershed

A

The high ground separating one river basin from another

25
Q

Downstream characteristics of a river that increase

A

-discharge
-occupied channel width
-channel depth
-average velocity
-load quantity

26
Q

Why does the discharge increase downstream

A

-as a river moves downstream, additional discharge is added to the main river by tributaries, surface flow and ground water

27
Q

Why does the load quantity increase as you go downstream?

A

As a river moves downstream, erosion occurs along the river banks and bed, eroded particles are added to the river’s load.

28
Q

Energy in a river (kinetic and potential)

A

1, overcome friction with the bed and banks (95% of it’s energy is used this way )
2,transport it’s load (when it loses energy, it drops/deposits it’s load)
3, erode the channel bed, banks and load

29
Q

Channel shape

A

-The efficiency of the channel is how easily water moves along it without using energy
-efficiency is measured by hydraulic radius
-the most efficent shape is semi-circular

30
Q

Channel roughness

A

Channel roughnesss causes friction, which slows the velocity of the water, friction might be caused by boulders, broken tress and uneven surface.

31
Q

Erosion is

A

This is where the river or sea wears the rocks away

32
Q

Transportation is

A

Where the river or sea carries eroded material, boulders, pebbles, sand, silt and mud eroded by the river are carried downstream

33
Q

Deposition is

A

When a river no longer has the energy to carry the load so it gradually drops it on the river’s bed

34
Q

The 4 types of erosion

A

-attrition
-hydraulic action
- corrasion (abrasion)
-solution (corrosion)

35
Q

Attrition

A

-“rock on rock”
-this is where rock fragments carried by the waves hit against each other and gradually wear down to form sand and slit

36
Q

Hydraulic action

A

“Pressuring”
- as waves break against the cliff face, the pressure of the breaking wave can compress air in cracks p. This compressed air gradually forces open the crack in the rock- as this process continues, the rock becomes increasingly weakened

37
Q

Abrasion

A

“ rock on cliff”
- this is when rock fragments are hurled at cliffs by breaking waves, gradual at scraping away at the cliff face

38
Q

Solution

A

“Rusting, dissolving”
- this occurs where the salt water is able to dissolve so,e of the chemicals in rocks- for example, limestone cliffs are gradually weakened as the salt water dissolves the calcium carbonate in the limestone

39
Q

Factors that affect erosion (4)

A

-load= the heavier+sharper the load the grater the potential for erosion
-velocity and discharge= the greater the velocity and discharge the grater erosion
-gradient =increased gradient,more erosion
-PH= rates of solution are increased when the water is more acidic
-

40
Q

Transportation

A

-suspension
-solution
-traction
- saltation

41
Q

Suspension

A
  • carrying
  • fine, light material is carried along by the river
42
Q

Solution

A
  • minerals are dissolved in the water, this is chemical change
43
Q

Traction

A

Large boulders and rocks are rolled along the river bed

44
Q

Saltation

A

Small pebbles and stones are bounced along the river bed

45
Q

Deposition

A

Main reason= river loses energy
- as river drops it’s load when the speed or volume of river creases, the load, which is carried gets deposited
-the heavier material is deposited first and the finer material carried further.

Proccess
#depositon occurs:
# decrease in gradient
#decrease in river flow
#the river meeting the sea or lake often creating a delta