Paper 2 - The UK’s Evolving PHYSICAL Landscape Flashcards
coastal zone
changing boundary between land and the sea
hard rock
resistant rocks
soft rock
less resistant rocks
hard rock examples
sandstone, limestone, chalk
soft rock examples
clay
disconcordant coastlines
- strata is at a right angle to the coast
- forms headlands and bays
concordant coastline
- strata is parallel to coastline
- example: Lulworth code
rock strata
stacked-up layers of sedimentary rock
erosion
wearing away the landscape
carbon dating
uses radioactive testing to find age of rocks which contained living material
how has tectonic processes affected the land
- convection current beneath the plate uplifted rocks from below the sea - becoming land
- during uplift, some rocks snapped and moved along faults in earthquakes -> each movement disturbed the strata so that they tilted
- sometimes, the faults form a steep edge (fault scarp) where uplift has raised some parts more than others
how has glaciation affected the landscape
- altering river valleys, making them deeper and widening them into U-shaped troughs
- as they melted, the glaciers left features like Malham Cove with a spectacular waterfall
igneous rocks
the Earth’s oldest rocks, formed from lavas and deep magmas; they were once molten, then cooled and crystallised - most igneous rocks are resistant to erosion
sedimentary rocks
formed from sediments eroded and deposited by rivers, the sea, or on the sea bed - some are resistant while others crumble easily
metamorphic rocks
sedimentary rocks that were heated and compressed during igneous activity - heating and compression harden them and make them resistant
name igneous rocks
granite, basalt
name sedimentary rocks
chalk, clay, sandstone
name some metamorphic rocks
slate, marble
what is your upland landscape
lake district
what is your lowland landscape
the weald
what does discordant coastlines create
headlands and bays
batholith formation
- A large mass of magma intrudes into the ground
- Large masses of magma cools and solidifies
- Large crystals form in the rock
- They are dome shaped in overtime are exposed due to erosion
batholith
a type of igneous rock that forms when magma rises into the earth’s crust, but does not erupt onto the surface
weathering
Physical, chemical or biological breakdown of solid rock by the action of weather or plants
scree
Angular rock pieces created by freeze thaw weathering
features of Lake District (UPLAND)
was once glaciated which left behind U-shaped valleys and misfits (small rivers that flow where glaciers once were)
features of the Weald (LOWLAND)
Post glacial river processes: water in the chalk froze making it impermeable which created a dry valley
What is the geology of the Lake District (UPLAND)
hard igneous
What is a geology of the Weald? (LOWLAND)
Sedimentary
What is the weathering of the Weald (LOWLAND)
Chemical and biological weathering
What’s the weather in in the Lake District (UPLAND)
Physical weathering (freeze-thaw weathering)
What is a slope processes of the Weald (LOWLAND)
slow (soil creep - leaves behind scarp and vale)
What is the slope processes of the Lake District (UPLAND)
Rapid -> Rockfall and landslides
headland
A piece of land jutting into the sea
bay
A broad coastal inlet often with the beach
interlocking spurs
one of any number of projecting ridges that extend alternately from the opposite sides of the wall of a young, V-shaped valley down which a river with a winding course flows
Waterfall formation
- There is Erosion of less resistant rock underneath the more resistant rock continues (undercutting) -> creates a plunge pool
- Pressure and weight causes more resistant rock which overhangs to collapse
- The waterfall continues to road and it takes a new position -> leaves steep Valley
Abrasion
When sand and pebbles are dragged along the river bed