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The Langdale axe industry (or factory) is the name given by archaeologists to a Neolithic centre of specialised stone tool production in the Great Langdale area of the English Lake District. [1] The existence of the site, which dates from around 4,000–3,500 BC, [ 2 ] was suggested by chance discoveries in the 1930s.
The Langdale Pikes and the Langdale Boulders, Great Langdale. Among the best-known features of Great Langdale are the Langdale Pikes, a group of peaks on the northern side of the dale. From below, they appear as a sharp rocky ridge, though they are precipitous only on their southern side; to the north, the land sweeps gently to High Raise , the ...
Blea Tarn is situated in a small hanging valley between Great Langdale and Little Langdale. The tarn itself was shaped by glacial ice moving over the col from nearby Great Langdale, but the ice was cut off as the glacier shrank, leaving "moraines very different from those at the head of the main valley". [25]
The natural landscape of the park, with many movable rocks and boulders left behind after the last ice age, gave humans the easy opportunity to arrange them into many human-made patterns. It is an area where three rivers meet, along the edge of the Canadian Shield , close to the edge of prairie grasslands.
Glacial erratic boulders of King County are large glacial erratic boulders of rock which were moved into King County, Washington by glacial action during previous ice ages.. The Pleistocene ice age glaciation of Puget Sound created many of the geographical features of the region, including Puget Sound itself, [1] and the erratics are one of the remnants of that age. [2]
(The Center Square) – There's millions in federal funds for residential solar installation, if only Pennsylvanians could access it. The House Energy Committee heard testimony last week in ...
From January 2008 to December 2012, if you bought shares in companies when David B. Lewis joined the board, and sold them when he left, you would have a -2.4 percent return on your investment, compared to a -2.8 percent return from the S&P 500.
Big Rock. The Foothills Erratics Train is a 580 miles (930 km) long, narrow (0.62 miles (1.00 km) to 13.7 miles (22.0 km) wide), linear scatter of thousands of typically angular boulders of distinctive quartzite and pebbly quartzite that lie on the surface of a generally north-south strip of the Canadian Prairies.