Topic 4-Uks Evolving Physical Landscape Flashcards
How have tectonic processes shaped the UK’s physical landscape?
• Convection currents have caused uplift of some land, pushing it upwards and further out to sea
• Slowly moved to its current position from
Antartica 500 millions years ago
• Between collisions, huge volcanoes occurred erupting masses of lava and forming mountains
How has glaciation shaped the UK’s physical landscape?
• As the Pennines were uplifted, rivers like the Wharfe eroded into them, creating V-shaped valleys.
• But the most recent Ice Age, over 10 000 years ago, brought huge glaciers to the Pennines. They had two effects:
• altering river valleys, making them deeper and widening them into U-shaped troughs using corrosion, abrasion, freze thaw
• as they melted, the glaciers left features like Malham Cove
How has geology shaped the UK’s physical landscape?
• As tropical don amd coral died, skeletons fell to the sea floor, forming horizontal layers
(stratas)
• As skeletons fell, they crushed those beneath them, eventually squeezing out water and compacting them into rock
• Other rock strata deposited on top of limestone- resists erosion so it forms high peaks and protects weaker sands
• Calcium Carbonate crystallises around the fragments, cementing together
What is igneous rock?
Magma cools amd hardens. Rock form crystals as it cools down. Usually hard
What is sedimentary rock?
Layers of sediment are compacted together until they become solid rock:
Limestone and chalk form from tiny shells and skeletons of sea creatures. Limestone is hard, chalk is softer rock
What is metamorphic rock?
Sedimentary rocks that were heated and compressed during igneous activity. Heating and compression harden them and make them resistant - shale becomes slate and limestone becomes marble.
What are the locations of upland in Uk?
North West- Peak District, Lake district
What are the locations of lowland
South East/ Central UK- North and South Downs
What rock types are in upland?
Resistant igneous and metamorphic - Carboniferous limestone, granite
What rock types are in lowland?
Sedimentary-Limestone, chalk, clay
What is an example of sedimentary rock and its properties?
Limestone:
Coral/ sediment and pressure over time. Made up of layers
Permeable, underground rivers
Generally resistant
What is an example of igneous rock and its properties?
Granite:
Magma cools deep underground
Crystals of quartz
Very resistant
What is an example of metamorphic rock and its properties?
Slates:
Heated mud or shales
Very resistant
How does seasonality impact coastal erosion?
Through changing seasons, storm frequency may vary, often highest in winter. Increases in storm frequency result in the erosion and saturation of cliffs through increasing winds and rainfall.
Temperature also varies with seasons. Differences in temperature have an impact on processes along the coast (eg: Increasing rate of salt weathering as water evaporates quickly
How does storm frequency impact coastal erosion?
Storms are very frequent in many parts of the Uk, especially in winter. Stronger winds create high energy, destructive waves which increase erosion pf the cliffs. Intense rainfall cause cliffs to become saturated- thus makes mass movement more likely
How does prevailing wind and fetch impact coastal erosion?
The prevailing winds in the UK are mostly warm south Westerlies which bring storms from the Atlantic Ocean. The Uk’s South is exposed to these winds and storms, further resulting in the erosion of coasts
How does mass movement impact coastal erosion?
Mass movement is the shifting of rocks and loose material down a slope, e.g. a cliff. It happens when the force of gravity acting on a slope is greater than the force supporting it. Mass movements cause coasts to retreat rapidly. Theyre more likely to happen when the material is saturated — it acts as a lubricant and makes the material heavier and unstable. In rotational slumping, the material shifts with a rotation as material closer to the surface is more stable; less of it collapses. Layers of impermeable rock means it can slump. Rock slides occur as it slides quickly along a bedding plane
How does weathering impact coastal erosion?
Weathering is the breakdown of rock. This may occur through mechanical weathering (seawater gets into cracks, evaporates, salt crystals form and expand, widens cracks causing it to break up), chemical weathering (Water have dissolved CO2, making them weak carbonic acids, reacts with rock containing calcium carbonate so rocks are dissolved), biological weathering- living things (plant roots break down rocks by growing into cracks and pushing apart)
What is abrasion?
eroded particles in the water scrape and rub against rock, removing small pieces
What is hydraulic action?
waves crash against rock and compress the air in the cracks. This puts pressure on the rock. Repeated compression widens the cracks and makes bits of rock break off.
What is attrition
eroded particles in the water smash into each other and break into smaller fragments. Their edges also get rounded off as they rub together.
What are the characteristics of destructive waves?
Destructive waves are high, steep, and have a high frequency
• Their backwash (the movement of the water back down the beach) is more powerful than their swash (the movement of the water up the beach). This means material is removed from the coast.
• The backwash flows under the next incoming wave, forming a rip current. These can be strong and drag swimmers out to sea.
• Storms increase the erosional power of destructive waves, which can lead to increased rates of coastal retreat.
What are the characteristics of constructive waves?
Constructive waves are low, long, and have a low frequency
• The swash is powerful and it carries material up the coast, meaning they deposit material along the coast
• The backwash is weaker and it doesn’t take a lot of material back down the coast.
What are joints
Small, usually vertical cracks