III.—Formation of Vallies. A Description of Heudeshope
The Heudeshope beck is a small feeder of the Tees, running swiftly down a steep valley into the main stream, at Middleton Teesdale. It is wholly in the lead-measures (Carboniferous limestone), which are here nearly horizontal, undisturbed by trap, and shew only a few faults, so small as not to affec...
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| Vydáno v: | Geological Magazine |
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| Hlavní autor: | |
| Médium: | Článek |
| Jazyk: | angličtina |
| Vydáno: |
Cambridge University Press
1868
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| Témata: | |
| On-line přístup: | https://zenodo.org/record/2022649 https://doi.org/10.1017/s0016756800207668 |
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