Appleby Group
From Wikipedia, the free encyclopedia
The Appleby Group is a lithostratigraphical term referring to the succession of Permian Period aeolian and fluviatile rock strata which occur in northwest England and beneath the Irish Sea in the United Kingdom.[1]
TypeGroup
Sub-unitsBrockram
UnderliesCumbrian Coast Group and Roxby Formation
Overliesmid-Carboniferous unconformity
| Appleby Group | |
|---|---|
| Stratigraphic range: | |
| Type | Group |
| Sub-units | Brockram |
| Underlies | Cumbrian Coast Group and Roxby Formation |
| Overlies | mid-Carboniferous unconformity |
| Thickness | variable |
| Lithology | |
| Primary | sandstone |
| Other | mudstone, breccia |
| Location | |
| Region | northwest England |
| Country | England |
| Type section | |
| Named for | Appleby-in-Westmorland |
The Appleby Group unconformably overlies a variety of older rock strata (Carboniferous). It is succeeded (overlain) by the Cumbrian Coast Group[2] Its lowermost sub-unit is the Brockram, a breccia which sits unconformably on a range of older strata.[3]
