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Is London built on bedrock?

The main bedrocks are Chalk and London Clay, with much of the surface geology made up of sands and gravels from the Eocene, till and gravel from glacial activity, and recent non-glacial deposits caused by wind or water action.
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How far down is bedrock in London?

In some places in the south and west of the region, the younger sedimentary bedrock extends to more than 1 km depth. However, in most of the region the older sedimentary bedrock and basement rocks occur within 500 m of the surface, and lie as shallow as 150 m in some north-eastern parts.
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What soil is London built on?

Most properties in the Greater London area are built on London Clay, which is one of the most shrinkable of soil types of all as it's highly susceptible to changes in volume caused by high water content.
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How deep is bedrock in England?

Seismographical research shows that the crust of the Earth below Great Britain is from 27 to 35 km (17 to 22 miles) thick. The oldest surface rocks are found in north west Scotland and are more than half as old as the planet.
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Why is London built on clay?

This is because old quarry holes are generally refilled with waste material and by lining it with London Clay (which is virtually impermeable) it prevents waste and hazardous substances from entering the groundwater.
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What type of rock is London built on?

The main bedrocks are Chalk and London Clay, with much of the surface geology made up of sands and gravels from the Eocene, till and gravel from glacial activity, and recent non-glacial deposits caused by wind or water action.
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What is under London Clay?

Although the Cretaceous Chalk and the London Clay are the thick rock layers immediately under London, these aren't the only rock layers. For instance, older rocks underlie the chalk, and other rock layers are found between the chalk and the London Clay, and also between the London Clay and the surface.
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Where is the oldest bedrock in the world?

Bedrock in Canada is 4.28 billion years old

Bedrock along the northeast coast of Hudson Bay, Canada, has the oldest rock on Earth.
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Was England once tropical?

Some 210 million years ago, Britain consisted of many islands, surrounded by warm seas. Europe at the time lay farther south, at latitudes equivalent to North Africa today. Much of Europe was hot desert, and at this point was flooded by a great sea – the Rhaetian Transgression.
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Where is bedrock in the USA?

Bedrock City is a Flintstones-themed roadside attraction consisting of an amusement park and RV park at the corner of Arizona State Route 64 and U.S. Route 180 in Coconino County, in the U.S. state of Arizona.
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Why is London so hilly?

The hills in the City of London, from west to east, Ludgate Hill, Corn Hill and Tower Hill, are presumed to have influenced the precise siting of the early city, but they are very minor, and most of central London is almost flat. These hills are developed in various gravel terrace deposits of the river Thames.
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How deep is the clay under London?

London Clay, lies up to 433 feet (132 metres) thick under the City of London and supports most of its tunnels and deeper foundations.
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How did London grow so big?

An ever-growing city

From the sixteenth to mid-seventeenth century, London benefited from the centralized politics and the maritime trade expansion developed by the Tudors and continued by the Stuarts. During Henry VIII's reign London had 100,000 inhabitants. In mid-seventeenth century it had over 500,000.
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Is there bedrock under Chicago?

The bedrock layers under the city of Chicago include massive reefs of limestone that are several hundred million years old, but they cannot be seen except in rock quarries such as the giant pit along the Des Plaines River at McCook. At the other extreme are the human-created landforms of the Chicago region.
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How deep is bedrock in New York?

At the southern tip of Manhattan bedrock depths start at about 8 meters below the surface; going north, the bedrock dips down into a kind of bedrock valley, which reaches its greatest depth between City Hall and Canal Street.
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Is there bedrock under San Francisco?

The Jurassic to Eocene Franciscan Complex in the Bay Area is the most widespread bedrock. The local Franciscan can be broken into nine tectonic terranes that represent pieces of seafloor that were accreted to the North American margin in over a 100 Myr period of subduction.
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When was England deforested?

In the middle of the sixteenth century Britain began to run out of wood. By 1700 it had converted almost completely to coal.
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Was England colder 1000 years ago?

Two astronomers have taken a new look at 240 studies of the world's climate and offered a challenge to global warming doom-mongers. Britain was probably warmer for Robin Hood and Richard Lionheart 1,000 years ago, they say.
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Was Britain ever forested?

The first trees began to colonise the tundra of Great Britain and Ireland during the late glacial period from 10,000 BC. They were limited only by high altitude, severe wind exposure and waterlogging. By 3000 BC everywhere that trees would grow was covered with forest, sometimes called the 'wildwood'.
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Can you get past bedrock in real life?

Real-world bedrock is hard, but absolutely breakable - and most large buildings are anchored into the bedrock with structures called "foundations".
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What is the oldest land on Earth?

Dating to around 3.6 billion years ago, the Pilbara region of Western Australia is home to the fossilised evidence of the Earth's oldest lifeforms.
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How far underground is bedrock?

Bedrock is the solid, intact part of the earth's crust, the outer layer 20 to 25 miles thick that rests on the earth's mantle.
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How deep is the London water table?

Cretaceous chalk is the major aquifer, approximately 60m below the surface of central London.
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How thick is London Clay?

In the London Basin the London Clay is as much as 200 metres (600 feet) thick and is brown, bluish, or gray.
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How far underground is clay?

For example, many soils contain a relatively low amount of clay in the surface layer, a higher amount between the depths of 25 to 75 centimeters (10 to 30 inches), and a decreased amount below a depth of 100 centimeters (40 inches).
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