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693280
Physical Geography
Descripción
none (Physical) Geography Mapa Mental sobre Physical Geography, creado por Jazz Young el 30/03/2014.
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geography
physical
geography
physical
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Mapa Mental por
Jazz Young
, actualizado hace más de 1 año
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Creado por
Jazz Young
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Resumen del Recurso
Physical Geography
The Earth's Crust
Plates
Oceanic Plate
made of Basalt
are between 5Km and 10Km thick
'Floats on a very hot mantle
Continental Plate
made of Granite
between 25Km and 90Km thick
'floats' on a very hot mantle
Plate Margins
Destructive
Oceanic and Continental plates are pushed together
Earthquakes occur here due to fault line
Fold Mountains are made
Constructive
Oceanic or Continental plates pull apart
Creates Volcanoes
Conservative
Plates are pushed in different directions
Earthquakes occur here due to a fault line made
Restless Earth
Fold Mountains
formed on destructive plate margins
Geosyncline
A very large downfold in the Earth's crust which fills up over time with sediment
the rocks in the crust are compressed and folded into ANTICLINES (upfolds) and SYNCLINES (downfolds)
Volcanoes
Types of volcanoes
Shield Volcanoes
Found on Constructive plate margins
Basic Lava (1200C)
runny and flows long distances before cooling and soldifying
many eruptions form a coneshaped mountain with gently sloped sides
E.G Mauna Loa, Hawaii, USA
Composite Volcanoes
Acid Lava (800C)
thick and sticky
alternate eruptions cause ash followed by lava to build up a cone shape with steep sides
Found on Destructive plate margins
E.G Mt St Helens, Washington, USA
Supervolcanoes
found on Destructive plate margins
Massive explosions of ash form a sunken crater
ash would fall across the whole Earth killing everything
Yellowstone Caldera, Wyoming, USA
Earthquakes
The Cause
Plates are locked together via friction and pressure builds up over many years
the Crustal rock breaks suddenly underground causing a focus point in the rock
stored energy is released in seconds and travels outwards from the epicentre as shock waves
recorded in SEISOMETER
RICHTER SCALE measures the energy released
MERCALLI SCALE measures the damage done
Coasts
Waves
Destructive Waves
remove beach material
form in strong winds
BACKWASH is STRONGER than SWASH
a frequency of 11-15per minute
Constructive Waves
deposit beach material
form in light winds with calm conditions
SWASH is STRONGER than BACKWASH
frequency of 6-9per minute
Erosion
Hydraulic Power
force of the waves crashing in the cliff
air trapped in the cliff is compressed and fractures the rock
Solution
Rocks containing calcium carbonate slowly dissolve because of acidic water.
Attrition
pebbles are rolled backwards and forwards by waves
as they rub against each other they're slowly worn away
Abrasion
Sand and pebbles are thrown against cliffs by breaking waves and wear them away
Transportation and Deposition
Traction
boulders and cobbles are rolled along by powerful waves
Saltation
pebbles and sand are bounced around
Suspension
silt and clay are suspended in moving sea water
Solution
minerals are dissolved in sea water
Longshore Drift is the movement of material along a beach
Mass movement and Weathering
Sliding
Blocks of rock or loose material slide rapidly down the slope
Slumping
a mass of soil or clay slides downwards a curve slip-pane,
forms a scar on the upslope and a toe on the downslope
Landforms
Headlands and Bays
a headland is an area of land that sticks out into the sea
a bay is a curved coastal inlet
Hard engineering
building structures or machinery to control the natural processes
Sea walls
concrete walls designed to reflect the wave energy
Groynes
wooden built barriers built across the beach to trap the sand and pebbles transported via longshore drift
Rock armour
large boulders or resistant rock placed at the base of the cliff to prevent erosion
Soft engineering
working with the environment to modify or prepare for natural processes
Beach nourishment
beach material lost throughout longshore drift is replaced with material from further along the coast
Dune regenration
sand dunes are damaged by walkers or picnicker. areas of sand dynes are fenced off to allow them to re-grow naturally
Marsh Creation
areas of low economic value allow the sea to erode and flood the land.
this then develops mud flats, salt marshes, and beaches.
Living world
Weather and Climate
Depressions
areas of low pressure formed when air masses of different temperatures meet.
Anticyclones
areas of high pressure formed when an air mass is slowly sinking
Ecosystems
Nutrient Cycles
all living things need nutrients to live and grow.
the nutrients move through the ecosystem in a cycle
Energy Flows
plants and animals need energy to survive.
energy flows through an ecosystem along the food chain
Recursos multimedia adjuntos
plate_boundaries (image/png)
fold_mountains (image/jpg)
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