Geology and UK 4.1 Flashcards
Give a definition, approximate age, 3 examples and location in UK of igneous rocks
Igneous :Rocks formed by the cooling and solidifying of molten materials in teh mantel
Age : Earths oldest rock
Examples: Basalt, Granite, Obsidian
Locations : These rock types are found in the uplands in the UK
Give a definition, approximate age, 3 examples and location in UK of sedimentary rocks
Sedimentary : Rock that has formed through the deposition and compression of sediment, and through the process of heat and pressure
Age : depends on rock but between 2 to 600 million years
Examples : Chalk, clay and sandstone
Location : Found everywhere
Compare metamorphic and igneous rock
Metamorphic rocks, formed by temperature and pressure changes inside the Earth / eg. Marble from limestone
Igneous rock , formed by the cooling of magma (molten rock) inside the Earth or on the surface / eg. Obsidian
Compare the formation and characteristics of granite and carboniferous limestone
Granite is a type of igneous rock, formed by magma cooling on the earths surface.
Characteristics : Very hard rock, the minerals (quartz, feldspar and mica) give the rock a pink, red, grey or white colour.
Limestone is a type of sedimentary rock, formed by layers of sediment squashed together, with large amounts of pressure
Characteristics : Easily weathered and eroded due to its soft rock composition.
Compare the formation and characteristics of chalk and slate
Chalk is a type of sedimentary, a purer, younger form of limestone. Layers of tiny shells and skeletons of dead sea creatures are compacted over time to form chalk.
Characteristics : Very porous, Medium resistance but stronger than clays
Slate is a metamorphic, formed by heated muds or shales.
Characteristics : Very resistant
Explain when and how active volcanoes shaped the uplands of the UK
Largely volcanic basalt (igneous) rock which erupted onto the surface 330-450 million years ago such as at Borrowdale. Also, granite (igneous) erupted below the surface at Eskdale. These are both resistant.
Explain how glacial erosion and deposition shaped the UK uplands
During the Ice Age, glaciers, formed in the upland areas, moved down through through the valleys changing them to u shaped from v shaped valleys
Explain when and how sedimentary rock was formed across the UK Lowlands
One such area in the lowlands, called the Weald, was once a dome of folding rocks, forming an arch called an anticline. Erosion has left alternate strata of more and less resistant rock to form a landscape. This happened during the Jurassic and Cretaceous age.
Explain how glacial deposition shaped the UK Lowlands
During and after the last Ice Age, water in the chalk froze, making it impermeable. Then, fresh water formed rivers and valleys. As the climate warmed, water seeped through the chalk once again leaving dry valleys where rivers had once flowed
Explain how scarp and vale topography forms in the UK Lowlands
Erosion has left alternate strata, of more and less resistant rock to form a landscape know as scarp and vale topography.
- Resistant rocks, like chalk, form steep escarpments
- Behind the escarpments, gentle slows follow the angle at which the rocks are tilted (called the dip), know as the dip slope
- Softer clays are lower and flatter, forming the vales