Yeet Flashcards
Where are the uk’s main upland areas
North and West of the country
Where are the uk’s main lowland areas
South and East of the country
What are the three types of rock
Igneous
Sedimentary
Metamorphic
Igneous rocks formation
Formed when molten rock from the mantle cools and hardens
The rock forms crystals as it cools.
Usually hard (e.g granite)
Sedimentary rocks formation
Formed when layers of sediment are compacted together until they become solid rock
Two main types:
Carboniferous limestone and chalk
Clays and shales
How are Limestone and chalk formed
Tiny shells and dead skeletons of dead sea creatures.
Limestone is hard
Chalk is soft
How are clays and shales formed
Made from mud and clay minerals
Very soft
How are Metamorphic rocks formed
Formed when other rocks are changed by heat and pressure. The new rocks become harder and more compact
e.g shale becomes slate, then slate becomes schist
Characteristics of granite
Very resistant
Forms upland landscapes
Lots of joints (cracks)
Impermeable - doesn’t let water through
Characteristics of Slate and Schist
Forms in layers creating weak planes
Very hard and resistant
Schist has bigger crystals than slate
Form rugged, upland landscapes
Characteristics of chalk and clay
Chalk is harder than clay
Forms hills in the lowlands and cliffs at the coast
Chalk is usually permeable
Clay is very soft and easily eroded
Clay forms wide, flat valleys in lowlands
Clay is permeable
Characteristics of limestone
Rainwater weathers the limestone through carbonation weathering
Limestone is permeable
What physical processes alter the landscape
Weathering
Erosion
Post-glacial river processes
Slope processes
What is weathering
Breakdown of rock into smaller pieces
Mechanical
Biological
Chemical
What is erosion
Erosion wears away rock
Rivers and sea constantly erode landscapes
What are post-glacial river processes
Melting ice at the end of glacial periods made rivers much larger with more power to erode the landscape
What are slope processes
Includes mass movement -
Shifting of rocks and loose material down a slope
Three types of mass movement:
Slides - shifts in a straight line
Slumps - shifts with a rotation
Rockfalls - material breaks up and falls
Three ways humans have changed the landscape
Agriculture
Forestry
Settlement
How have humans changed the landscape through agriculture
Clearing land for farming
Walls mark out fields
How have humans changed the landscape through forestry
Management of areas of woodland
Very little natural woodland left
Trees planted in straight lines, not natural
How have humans changed the landscape through settlement
Land concreted
Rivers diverted
Rivers straightened
What is mechanical weathering
Breakdown of rocks without changing its chemical composition
Salt weathering:
1) seawater gets into cracks
2) water evaporates, forming salt crystals which expand, putting pressure on rock
3) causes rock to break up
What is chemical weathering
Breakdown of rock by changing its chemical composition
Carbonation weathering:
1) seawater and rainwater have carbon dioxide (weak carbonic acids)
2) They react with rock that contains calcium carbonate.
3) rocks are dissolved
What is biological weathering
Breakdown of rock by living things
e.g plant roots grow into cracks, pushing rock apart