Topic 4 - The UK's Evolving Physical Landscape Flashcards
what are the 3 types of rock
igneous
sedimentary
metamorphic
how are igneous rocks formed
when molten rock from the mantle cools and hardens. the rock forms crystals as it cools down. igneous rocks are usually hard
how are sedimentary rocks formed
when layers of sendiment are compacted together until they become solid rock
how are metamorphic rocks formed
when other rocks are changed by heat and pressure. the new rocks become harder and more compact
what are the three main ways that techtonic activity has shaped the UK’s landscape
- active volcanoes
-plate collisions
-plate movements
how have active volcanoes shaped the UK’s landscape
by forcing magma through the earth’s crust which has cooled to form igneous rocks
how have plate collisions shapes the UK’s landscape?
plate collision causes the rocks to be folded and uplifted forming mountain ranges. many areas remain as uplands. the intense heat and pressure caused by plate collisions formed hard metamorphic rocks in northern Scotland and Ireland
how have plate movements shaped the UK’s landscape?
plate movements meant that millions of years ago Britain was in the tropics and higher sea levels meant that it was partly underwater so carboniferous limestone formed in the warm shallow seas. the youngest rocks in the UK are chalks and clays found in southern England. they formed in shallow seas and swamps. chalks and clays are softer rocks and are more easily eroded they form lowland landscapes
what are the characteristics of granite
- granite is very resistant and forms upland landscapes.
- it has lots of joints (cracks) which aren’t easily spread. the parts of the rock that have more joints wear down faster. areas that have fewer joined are worn down more slowly than the surrounding rock and stick out at the surface forming tors
- granite is impermeable - it doesnt let water through. this creates moorlands-large areas of waterlogged land and acidic soil with low growing vegetation
what are the characteristics of carboniferous limestone
- rainwater slowly eats away at limestone through carbonation weathering. most weathering happens along joints in the rock creating some spectacular features.
- limestone is permeable so limestone areas also have dry valleys and resurgent rivers that pop out at the surface when limestone is on top of impermeable rock
what are the characteristics of slate and schist
- slate forms in layers creating weak planes in the rock. it is generally very hard and resistant to weathering but is easily split into thin slabs
- schist has bigger crystals than slate and also splits easily into small flakes
- slate and schist often form rugged upland landscapes. they are impermeable which can lead to waterlogged and acidic soils
what are the characteristics of chalk and clay
- chalk is harder than clay. it forms escarpments in UK lowlands and cliffs at the coast. one side of the hill is usually steep and the other side is more gentle
- chalk is permeable - water flows through it and emerges as a spring where it meets impermeable rock.
- clay is very soft and is easily eroded. it forms wide flat valleys in the UK lowlands. it is impermeable so water flows over the surface - there are lots of streams rivers and lakes
what is weathering
the breakdown of rock into smaller pieces. it can be either mechanical chemical or biological
what is erosion
the breakdown and removal of rock
what are post glacial river processes
melting ice at the end of glacial periods made rivers much bigger than normal with more power to erode the landscape. the ice also leaves distinctive landforms when it is melted