This KS3 Geography quiz takes a second look at limestone scenery. Limestone is a sedimentary rock composed largely of the minerals calcite and/or aragonite, which are different crystal forms of calcium carbonate (CaCO3). Sedimentary rocks are deposited in layers on the beds of oceans, seas, lakes and occasionally on dry land. The breaks between the layers are called bedding planes. They are usually areas of weakness in a mass of rock. Carboniferous limestone is no exception, but not only does it contain bedding planes, it also contains a lot of vertical joints.
Rainwater is slightly acidic and, as you should have learnt in your science lessons, calcium carbonate will dissolve in acids. Rainwater slowly dissolves the vertical joints, widening them and creating a limestone pavement. As the water travels deeper underground, it can still dissolve the limestone, particularly along the bedding planes. This is how caves and caverns are formed. A cave or cavern that is close to the surface of the earth can suffer from a collapsed roof, creating a deep and steep-sided limestone gorge.
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It's approximately 15-16 million years old
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Most sedimentary rocks have bedding planes
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Limestone dissolves in rainwater because rainwater is naturally slightly acidic
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The largest of these can be millions of years old - they grow at a very slow rate
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The rock has many uses e.g. building, in steelworks, making toothpaste
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The Peak District is mainly in Derbyshire but extends into neighbouring counties
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They will only appear when there has been a lot of rain. Some are seasonal and disappear in the summer, like the river Manifold on the border of Derbyshire and Staffordshire
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Because the rock is full of cracks like some brick walls
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The gaps between them are called grykes
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This can happen when a cave or cavern has formed close to the surface
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