Pinksey Bottom
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Pinksey Bottom Tranmoor Beck in the lower reaches |
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 The Pinskey Gill |
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| Data | ||
| location | Cumbria , England | |
| River system | River Lune | |
| Drain over | Sandwath Beck → River Lune → Irish Sea | |
| River basin district | North West | |
| source | North slope of Green Bell 54 ° 25 ′ 39 ″ N , 2 ° 27 ′ 57 ″ W |
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| muzzle | in the Sandwath Beck coordinates: 54 ° 26 '22 " N , 2 ° 28' 3" W 54 ° 26 '22 " N , 2 ° 28' 3" W.
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The Pinksey Bottom (alternative spelling also Pinskey Bottom) is a small river in Cumbria , in north-west England . The Pinskey Bottom has its source on the north slope of the Green Bell and flows north to its confluence with the Sandwath Beck .
Soon after its formation, the Pinksey Bottom flows through the incision of Pinskey Gill (alternative spelling Pinksey Gill). The Pinskey Gill is a Site of Special Scientific Interest . The area is known for the paleogeography and environmental reconstruction of northern England in the Carboniferous Period .
Individual evidence
- ↑ Pinksey Gill on SSSI List at Natural England