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809925
Physical geography
Descripción
GCSE Geography Mapa Mental sobre Physical geography, creado por Marie Stevens el 30/04/2014.
Sin etiquetas
geography
gcse
Mapa Mental por
Marie Stevens
, actualizado hace más de 1 año
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Creado por
Marie Stevens
hace más de 11 años
19
1
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Resumen del Recurso
Physical geography
Volcanoes
monitering
quivering in the ground
how close magma is to the surface
any bulges on the side of the volcano
dust clouds
3 types
super volcanoes
shield volcanoes
composite volcanoes
at destructive plate margins
the oceanic plate goes under the continental plate; its more dense
at constructive plate margins
Earth quakes
Tsunami
Japanese earthquake and Tsunami on 11 March 2011
impacts
collapsed roads
destroyed buildings
loss of lives
expensive to fix
increase in homeless people
jobs lost
tropical rainforests
mainly distributed along the tropics of Capricorn and cancer. these are either sides of the equator.
the vegetation has different layers
shrub, canopy
adaptations
become taller to compete for sunlight
flowers adapted to grow up trees to get to the sunlight
bigger roots
grow faster
little shrub area
tourism
reasons for tourist areas
coastline, mountains, citys
transportation links
airports
roads
train stations
busses
income
jobs
Dubai
tectonic plates
plate margins
destructive margins
two plates moving towards each other
where an oceanic plate meets a continental plate.
the denser oceanic plate is forced down into the mantle and destroyed
this often creates volcanoes or deep ocean trenches.
where the two continental plates meet, the plates are destroyed, but no crust is destroyed.
constructive margins
two plates moving away from each other
magma rises from the mantle to fill the gap and cools, creating new crust.
conservative margins
moving sideways past each other, or are moving in the same direction at different speeds
crust isn't created or destroyed
Earth's surface is separated into tectonic plates
inner core
outer core
mantle
Crust
types of crust
oceanic crust
thinner and more dense
continental crust
thicker and less dense
fold mountains
alps
in central Europe
are formed when plates collide at destructive margins
the sedimentary rocks that have built up between them are folded and forced upwards to form mountains
when oceanic and continental plates collide
or where two continental plates collide
uses
farming
higher slopes are used to graze animals like mountain goats
lower slopes are use to grow crops
steep slopes are sometimes terraced to make growing crops easier.
mining
are major sources of metal ores
tourism
activities attract tourists
skiing
snowboarding
ice climbing
forestry
the environment is good for conifer trees
these are used for fuel, building materials and to make things like paper and furniture.
Hydro-electric power (HEP)
steep sided mountains and high lakes (to store water) make fold mountains ideal for generating hydro eclectic power.
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