Der Fluss entsteht in einem Gebiet nördlich des Hadrianswalls, das aus den für Northumbria typischen Gesteinsschichten von Kalkstein, Sandstein, Schiefer und Steinkohle besteht und von zahlreichen kleinen Wasserläufen durchzogen ist, die zum großen Teil unbenannt sind. Der Caw Burn und der Pont Gallon Burn sind die beiden längeren eindeutig zu identifizierende Quellflüsse des Haltwhistle Burn.
Source: Wikipedia.org
Copyright: Creative Commons 3.0
| | Public | English
Northumberland, United Kingdom
Discover the most beautiful and popular trails in the area, carefully bundled into appropriate selections.
Source: Stephen McKay
Copyright: Creative Commons 2.0
Discover the most beautiful and popular attractions in the area, carefully bundled in appropriate selections.
Source: Stephen McKay
Copyright: Creative Commons 2.0
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Haltwhistle
