Formed of small particles that have been deposited in layers
Igneous rocks
Created by volcanic activity, when magma or lava cools
Metamorphic rocks
Formed from other rocks that have been changed by extreme pressure or heat
Upland
Highabove sea level
Lowland
Lowabovesealevel
Erosion
The wearingawayand removal of material by a moving force
Deposition
The dropping of material by amoving force
Weathering
The breakdown and decay of rocks by naturalprocesses
Permeable
Water can pass through
Impermeable
Water can't pass through
Hydraulic action
The sheer force of water crashing against the coastline causing material to be dislodged and carried away by the sea
Abrasion
Fragments of a rock, pebbles and sand are picked up by the waves and thrown against the cliff face, causing pieces of rock to break off
Solution
Thechemicalactiononrocksbyseawater, most effective on limestone rocks, in which calcium is dissolved and carried away
Attrition
Rock fragments and pebbles carried by the waves are reduced in size as they collide against each other and the cliff face, eventually broken down into sand-sized particles
Biological weathering
Roots of growing plants can widen cracks in the rocks, burrowing animals can also cause the rock to weaken and decay
Mechanical weathering
Freeze thaw weathering weakens rocks, caused by repeated freezing and thawing of water in cracks or holes in the rock
Chemical weathering
Rain water is a weak carbonic acid that slowly dissolves alkaline rocks likechalk due to a chemical reaction
Concordant coasts
Have different rock bands that run parallel to the coast
Discordantcoasts
Have different rock angles that run at right angles to the coast
Joints
Cracksthat divide a rock intoblocks
Faults
A large break in a rock
Fetch
Thedistanceover which the wind blows over the open water
Stock
An isolated pillar of rock left after the top of an arch collapses
Arch
Formed when two caves on either side of a headland join up to a single cave eroded through the headland
Spits
A long and narrow ridge of sand or pebble, one end of which is attached to the land
Bars
Formed when a spit reaches the other headland, only when nearby river and sea currents are gentle
Hard engineering
Involves building structures along a coast, usually at the base of a cliff or on the beach
Soft engineering
Designed to work with natural processes in the coastal system, in order to manage erosion
Discharge
Rate of river flow measured in cumecs
Interlocking spurs
Near their source, rivers flow around valley side slopes, called spurs, rather than being able to erode them
Waterfalls and gorges
1. Hard rock cuts across the softer rock
2. The softer rock downstream is eroded more quickly to form a waterfall
3. The softer rock is eroded more quickly to leave an overhang, which then collapses so the waterfall moves upstream
Infiltration
When water sinks downwards into the soil
Hard engineering (rivers)
Involves building structures along a river
Soft engineering (rivers)
Designed to work with natural processes in the river system in order to manage erosion
Distributions and characteristics of the world's large-scale ecosystems
Tropical rainforest
Temperate forest
Boreal forest
Tropical grasslands
Temperate grasslands
Deserts
Tundra
Tropical Rainforest
Hot all year (27-30 degrees)
Wet all year
Variety of broadleaf plants
Trees dominate with other plants competing for light
Tropical Grasslands
Hot all year
500-1000mm rainfall a year, always with a dry season
Tall grasses with scattered drought adapted trees and shrubs
Deserts
Very hot all year
Very low rainfall
Plants have water storing features, spines instead of leaves and extensive root systems
Temperate Grasslands
Hot in the summer
Very cold in the winter
Most of the rainfall in the year occurs in late spring or summer