Paper 1 review Flashcards

1
Q

How are fold mountains formed?

A

Tectonic plates converge
Driven by convection currents
Results in compression
Upfolding and uplift
Of sediment
To produce fold mountains

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2
Q

How ocean trenches and ridges are formed

A

Ocean trenches formed at converging plate boundaries by the subduction of one plate below the other causing a deep-sea trench. Ocean ridges are formed at divergent plate boundaries leading to the escape of magma which will produce ocean ridges

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3
Q

Conditions for braiding

A

Large input variations
High sediment load
Coarse sediment load
Steep slopes
Opposite for meandering

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4
Q

The Walker circulation

A

Trade winds
Piling of warm water
Upwelling of cold water
Active convection
Pressure
Dry and wet

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5
Q

Increasing slope stability

A

Afforestation: increases internal strength
Netting: contains debris or rocks
Pining: increases strength
Grading: reshaping to a specific slope

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6
Q

The role of water in movement

A

Rainsplash in terms of the kinetic energy of raindrops being enough to dislodge soil particles which, if there is a slope gradient, will move down. Bare surfaces needed. For sheetwash, smooth surfaces are needed where infiltration capacity is exceeded. Similar for rills but surface irregularities mean water flow is concentrated in channels. Soil heave, soil creep, solifluctuation and mudflows by wetting and drying

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7
Q

Factors influencing weathering

A

Temperature: freeze-thaw, insolation, salt crystal
Precipitation
Rock type and structure: greater in well jointed rocks will bedding planes
Pollution

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8
Q

Radiation balance

A

(incoming solar radiation + atmospheric counter radiation) - (reflected solar radiation + outgoing terrestrial radiation)

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9
Q

Daytime energy budget

A

Incoming solar radiation
Reflected solar radiation
Energy absorbed at surface
Sensible heat transfer
Latent heat transfer
Longwave radiation

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10
Q

How ocean currents affect wind belts

A

Winds across the sea cause surface currents
Trade winds pull surface water west-east
Coriolis deflects right so north
Westerlies push east (clockwise)
In southern hemisphere deflects left (counterclockwise)
Gyres due to circular flow
Wind drives these away from coasts
Winds from high to low pressure
Warm surface water in warm area
Exposes colder water

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11
Q

Sensible heat transfer

A

The transfer of heat into or out of an area by convection, conduction or advection changing temperature rather than phase

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12
Q

Latent heat transfer

A

Absorbed ore released by evaporation or condensation by a substance during a phase change

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13
Q

Abrasion

A

The wearing away of the river bed and bank by load
Most effective in upper course
Creates V-shaped channel

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14
Q

Hydraulic action

A

Force of flowing water to dislodge particles or fragments into the channel
Collapse and retreat of banks
Lateral erosion
Widens channel

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15
Q

Attrition

A

Constant collision and grinding of sediment, wearing down bedload
Impacts downstream efficiency and reduces size and friction

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16
Q

Solution

A

Removal of soluble minerals along with transportation
Eroded material dissolved and carried
River energy not important
In humid tropics, chemical weathering is efficient so solution is important

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17
Q

Reasons for different rates of weathering

A

Higher water content is faster
Result of lubrication of failures
Increase of pore water pressure reducing internal cohesion
Faster on steeper slopes
Rapid increase of strength
Particle by particle is slower
Rockfalls are fast due to lack of support
Vegetation influences movement

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18
Q

Suspension

A

Fine particles carried without touching channel
More turbulent means larger particles can be transported

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19
Q

Saltation

A

Skipping of rocks along river bed
Cumulative process

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20
Q

Traction

A

Sliding, rolling or hopping
Only occurs at high energy levels to move coarse bedload

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21
Q

Raindrop formation

A

Coalescence involves the merging of smaller water droplets in warm clouds to form larger raindrops

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22
Q

Hail

A

Updrafts carry water droplets to heights where temperatures are below freezing so they freeze upon contact with ice nuclei, forming hailstones

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23
Q

Dew

A

Formed when objects on the ground cool below dew point temperature causing water vapour in the air to condense

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24
Q

Snow

A

Form due to the direct transformation of water vapour into ice crystals
Temperature and humidity influence shape and size of snowflakes
Areas closer to poles or higher altitudes are more likely to experience snow

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25
Fog
When air near the ground is cooled to dew point leading to the condensation of water vapour Advection fog occurs when warm, moist air moves over a cooler surface, cooling the air to its dew point Radiation fog develops under clear skies and calm winds mainly at night
26
Continental-continental constructive/divergent boundaries
Rift valleys Earthquakes Volcanoes
27
Oceanic-oceanic constructive/divergent boundaries
Ocean ridges Earthquakes Volcanoes
28
Continental-continental destructive/convergent boundaries
Fold mountains Earthquakes
29
Oceanic-oceanic destructive/convergent boundaries
Ocean trenches Island arcs Earthquakes Volcanoes
30
Continental-oceanic destructive/convergent boundaries
Volcanoes Fold mountains Earthquakes
31
Conservative boundaries
Earthquakes
32
Ocean trenches
Large scale features that are long and relatively narrow depressions in the ocean floor and is the point where one tectonic plate subducts beneath at destructive margins either oceanic-oceanic or oceanic-continental
33
Sea floor spreading
The moving apart of ocean plates as a result of convection currents
34
Conservative boundary
Where plates pass sideways at different speeds or angles
35
Subduction
The process where tectonic plates converge with one plate being forced down under another plate and is melted in the subduction zone
36
Slide
The movement of material downhill along a slide plane together with no internal deformation
37
Heave
The lifting of soil particles out of the slope followed by a drop to the surface
38
Fall
The free movement of material, often very fast from a very steep slope of cliff directly to the ground
39
Flow
The movement of often wet material on a slope with internal deformation and no noticeable failure surface
40
Sheetwash
The movement of water on a sloping surface as a uniform layer
41
Vegetation root action
The growth of roots in joints and crevices of rock, forcing them apart as the roots develop
41
Salt crystal growth
Water entering cracks and pore in rock evaporates, leaving salts which expand putting pressure on the rock
42
Hydrolysis
Where rainwater combines with the minerals within the rocks, soluble parts removed by water or decomposition of feldspar to kaolin
43
Freeze-thaw
Where water enters the cracks in a rock and freezes when the temperature is below 0C and expands by 9% of its volume
44
Rainsplash
Where soil is detached by raindrops hitting the surface
45
Hydration
Minerals absorbing water, leading to expansion to create a hydrate
46
Pressure release
The fracturing of rocks or creation of joints, the result of the reduction of pressure upon it
47
Carbonation
Dissolved carbon dioxide in water reacting with carbonate minerals
48
Altitude effects on climate
As altitude increases the pressure on the air is reduced and it becomes less dense and cooler When air is at the bottom of mountains and hills it is under more air pushing down on it making it denser and warmer For every 100m ascent air temperature drops by 1C Air temperature falls with increasing altitude
49
Latitude effects on climate
At the equator the sun shines directly overhead and is therefore concentrated on a small area whereas at the poles the suns energy is scattered over a larger area so it is less concentrated Highest temperatures at low latitudes in the tropics north and south of the equator There is a decrease in temperature between the equator and the poles
50
Distance from the sea affecting climate
Land heats and cools more quickly than the sea In winter, coasts are warmers since the water takes longer to cool Water takes longer to heat in summer so coastal areas are cooled by cold waters Inland is warmer in the summer since the land heats up Inland is cooler in winter due to the land cooling
51
Prevailing winds and air circulations affecting climate
In temperate zones cold air circulates from poles meeting with desert air. Creates rain clouds and mild temperatures Air rises at the equator since it is warm enough. Makes cumulonimbus clouds as it cools. Becomes denser so sinks creating high pressure
52
Ocean currents affecting climate
Warm ocean currents from hotter areas of the globe raise temperatures Cold currents from polar regions can cool temperatures Ocean currents flow in the same direction all year so temperatures are regularly affected
53
Latitude influence on pressure
At equator, warm surface causes rising air At poles, cold surface causes high pressure and sinking air Due to Coriolis force, air rises near equator and deflection produces sinking at 30 degrees Rising air in the Hadley cell produces cloud, thunder and rain in the ITCZ Sinking at at 30 degrees causes high pressure and clear skies
54
Latitude influence on temperature
Temperature affected by angle of the sun and thickness of atmosphere At equator, sun is direct because of earths angle and less atmosphere Opposite for poles where angle is greater so more atmosphere for radiation to penetrate More atmosphere means energy is scattered and less reaches the ground Low sun angle makes it more easily deflected by snow and ice so less is absorbed
55
Latitude influence on wind belts
Winds at ITCZ are light but can be broken by strong westerlies Mid latitude have faster flow than wind belts at equator Trade winds flow west in low latitudes Summer in SH causes cooling in NH so increased differences in polar and equatorial air leading to stronger high westerlies in NH Trade winds are NE in NH and SE in SH Trade winds associated with Hadley, prevailing westerlies with Ferrell and polar easterlies with Polar cells
56
Ocean currents influence on pressure
Oceans store heat better than atmosphere so air can be heated from above by sun and below by ocean. Creates bigger high pressure than usual making wind stronger Warm water evaporated into atmosphere Pressure affects salinity when high pressure leads to clear skies, high insolation, more water converts to vapour and salinity increases in loft over water
57
Ocean currents influence on temperature
The temperature of the ocean will warm or cool the air above it Ocean currents make cold areas warmer and warm areas cooler Warm equatorial currents will warm cool places in winter in tropical areas. Winds must be blowing air from above the currents onto land Oceans absorb much of the suns radiation warming the planet and allowing warm water to be transported
58
Ocean currents influence on wind belts
Winds blowing across the sea causes surface ocean currents Trade winds blow east to west in NH just above equator. Pull surface water causing currents. Coriolis force deflects right so move north. Westerlies at 30 degrees push east so closed clockwise loop In SH Coriolis force bends left so counterclockwise loop These are gyres due to circular flow Winds drive subpolar gyres away from coasts Winds move from high to low pressure. Winds in Pacific push warm surface water to warm region exposing cold deep water
59
Land/sea distribution influence on pressure
At sea level there is the most atmospheric pressure Air warms quickly over land and rises creating low pressure areas while air over water tends to stay cooler and hot air rises creating an area of higher pressure These differences drive weather patterns depending on pressure
60
Land/sea distribution influence on temperature
Land near the sea has less variations in temperature than inland Takes 5x as much energy to raise water by 2C than land Ocean retains heat and radiation longer than land. Especially noticeable in winter when night is longer so land loses more heat The further from the sea the more variation in temperature since not affected by ocean currents
61
Land/sea distribution influence on wind belts
General winds influenced by continents Close to surface, winds over oceans are stronger than over land Land surfaces are rougher, slowing winds Lack of land in SH is the cause of the bank of strong westerly winds Monsoons occur when there is a reversal of a wind system SE trade winds from SH cross equator in July, deflected right to SW winds in NH from Coriolis force