The Water Cycle Flashcards

(52 cards)

1
Q

Hydrological Cycle

A

The continual movement of water between the rivers, oceans, atmosphere and land

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2
Q

How the water cycle works

A

1) evaporation
2) warm air rises
3) condensation
4) precipitation
5) interception
6) surface run off or through flow
7) percolates

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3
Q

Major stores of water

A

Ocean, ice caps, land and atmosphere

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4
Q

Transfers

A

Movement of water between stores

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5
Q

River or drainage basins

A

An area of land drained by a river and its tributaries

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6
Q

Edges of drainage basin

A

Watershed

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7
Q

Where the river meets the sea

A

Mouth of the river

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8
Q

Types of erosion

A

Abrasion
Attrition
Hydraulic Action
Corrosion/solution

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9
Q

Abrasion

A

Material carried by the river wears away the bed and banks

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10
Q

Hydraulic action

A

The power of the water forces air into gaps in the banks and weakens them so they eventually collapse

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11
Q

Attrition

A

The particles carried by the river are bashed against one another, making them smaller and rounder

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12
Q

Corrosion/solution

A

Particles are dissolved because of slightly acidic solution

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13
Q

Causes of vertical erosion

A

Swirling currents creating potholes in the river bed

Water falls creating plunge pools

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14
Q

Types of transportation

A

Traction
Saltation
Suspension
Solution

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15
Q

Traction

A

Rolling large stones along the bed of the river

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16
Q

Saltation

A

Bouncing smaller particles along the bed

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17
Q

Suspension

A

Sediment that floats within the river flow

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18
Q

Solution

A

Minerals dissolve in the water

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19
Q

Deposition

A

When the velocity of the river falls, it has less ability to carry its load. The river then starts to drop the material, starting with the largest particles. Loss of velocity can occur for many reasons

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20
Q

Reasons for the loss of velocity

A

River enters the sea or lake
There is less water entering the river
There is more sediment in the river

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21
Q

Competence

A

The maximum size of material the river is capable of carrying

22
Q

Capacity

A

The total actual load transported

23
Q

Levels of energy required to erode

A

Sands require the least energy as their particles do not coagulate
Silt/Clay requires a higher velocity as particles do coagulate
Pebbles are eroded at higher velocities
Boulders require the highest velocities to erode

24
Q

Upper course vs lower course

A

Upper course: Steep gradients lead to rapid-flowing rivers
Middle course: River meanders through gentle gradients
Lower course: River braids over flat land

25
Upper course
- Vertical erosion - Weathering - Headward erosion - Boulders create friction, slowing down the rate of flow - Steep gradient
26
Characteristics commonly found in the upper course of rivers
- V-shaped valleys - Potholes - Interlocking spurs - Waterfalls - Rapids - Gorges - Large boulders
27
Middle course
``` Lateral erosion Transportation Asymmetrical channel Floodplain Truncated spurs Meanders ```
28
Lower course
Transportation Deposition Friction is reduced, so greater velocity
29
Characteristics commonly found in the lower course of rivers
``` Wide smooth channel Braiding Oxbow lakes Large floodplain Terraces Levees Deltas ```
30
V Shaped Valleys
Weathering breaks up material on slopes, which is then deposited into the river. Material is carried by riverbed through abrasion
31
Waterfalls
Soft rock erodes more quickly, undercutting the hard rock Hard rock is left overhanging, because it isn't supported it eventually collapses. Plunge pool is created by the erosion of rocks. Process repeats and waterfall moves upstream, forming a steep sided gorge on either side
32
Meanders
Meanders are formed by erosion and deposition. Centrifugal force causes the water to flow fastest around the outside of the river, creating erosion on the outside and deposition on the inside bend.
33
Oxbow Lakes
When the bends of a meandering river become so large that the water takes a more direct path, often cutting through the land of the bend. This may change the course of the river as more water runs through the alternate route. The old bend of the river eventually gets cut off, leaving an oxbow lake.
34
Braiding
River loses velocity, sediment is deposited and builds up to choke the main channel, causing the river to split in a braiding pattern.
35
Formation of a delta
- River carrying sediment reaches sea/lake - Loses energy and deposited material - Heaviest sediment first, more sediment is added - if tides are strong then sediment will be washed away, if not then delta will form
36
Flocculation
When the fresh and salt water meet creating an electric charge causing the clay particles to coagulate
37
Types of delta
Birds foot: Many distributaries Cuspate: Sediment spread evenly on either side Arcuate: Rounded and convex structure
38
Physical causes of flooding
- Heavy rainfall - Snowmelt - Steep slopes - Impermeable rock - Very saturated soils - Compacted or dry soils
39
Human factors that cause flooding
Urbanisation | Deforestation, removing trees reduces the amount of water intercepted and increases runoff
40
Storm Hydrographs
shows how rainfall events change the discharge of a river
41
Factors influencing storm hydrographs
``` Basin size Precipitation type Temperature Land use/ Urbanization Rock/Soil type Drainage density Tides/storm surges ```
42
Drainage density formula
Total length of all streams and rivers in a drainage basin, divided by the total area of the drainage basin
43
Factors affecting drainage density
``` Geology Land use Time Precipitation Relief ```
44
Bifurcation ratio meaning
a LOW bifurcation ratio means a HIGHER risk of flooding
45
Bifurcation ratio
Number of streams of one order in relation to the number of streams in the next order (1st order / 2nd order) then finding the average of all the ratios
46
Hydraulic radius
Ratio between the area of a cross section of a river channel, and the length of its wetted perimeter.
47
Purpose of the hydraulic radius
Determines the efficiency of a river. ...
48
Drainage patterns
Trellised Radial Parallel Dendritic
49
Radial
Streams radiate outwards from a central high point
50
Trellised
Tributaries enter the main river approximately 90 degree angles due to ridges of harder or impermeable rock, causing a trellis-like appearance of the drainage system
51
Parallel
Rivers flow uniformly down steep sloping surfaces
52
Dendritic
Streams join together to form tributaries into the main river. From overhead this makes a tree-like pattern with tributary "branches" and a river "trunk."