The Askrigg Block is the name applied by geologists to the
crustal block forming a part of
the Pennines
The Pennines (), also known as the Pennine Chain or Pennine Hills, are a range of uplands running between three regions of Northern England: North West England on the west, North East England and Yorkshire and the Humber on the east. Commonl ...
of northern England and which is essentially coincident with the
Yorkshire Dales
The Yorkshire Dales is an upland area of the Pennines in the historic county of Yorkshire, England, most of it in the Yorkshire Dales National Park created in 1954.
The Dales comprise river valleys and the hills rising from the Vale of York w ...
. It is defined by the
Dent Fault to the west and the
Craven Fault System to the south whilst to the north it is separated from the
Alston Block by the
Stainmore
Stainmore is a remote geographic area in the Pennines on the border of Cumbria, County Durham and North Yorkshire. The name is used for a civil parish in the Eden District of Cumbria, England, including the villages of North Stainmore and South ...
Trough. It originated as a geological structure during the
Carboniferous Period
The Carboniferous ( ) is a Period (geology), geologic period and System (stratigraphy), system of the Paleozoic that spans 60 million years from the end of the Devonian Period million years ago (Myr, Mya), to the beginning of the Permian Period, ...
as a major element in the Pennine Block & Basin Province.
[Edwards, W; Trotter, F M, The Pennines and Adjacent Areas, British Regional Geology (Third ed.), London: HMSO. Natural Environment Research Council (published 1954)]
References
Geology of the Pennines
Geology of North Yorkshire
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