Kinnesswood Formation | |
---|---|
Stratigraphic range: | |
Type | Geological formation |
Unit of | Inverclyde Group |
Underlies | Ballagan Formation |
Overlies | Knox Pulpit Formation |
Thickness | up to 400 metres (1,310 ft) |
Lithology | |
Primary | Sandstone |
Other | Limestone, Siltstone |
Location | |
Region | Europe |
Country | Scotland |
Extent | Central Lowlands |
Type section | |
Named for | Kinnesswood |
Location | Kinnesswood Row (partial) |
The Kinnesswood Formation is a geological formation in the Central Lowlands of Scotland. The lithology largely consists of sandstone with interbeds of limestone and siltstone [1]
Geology is a branch of natural science concerned with Earth and other astronomical objects, the features or rocks of which it is composed, and the processes by which they change over time. Modern geology significantly overlaps all other Earth sciences, including hydrology and the atmospheric sciences, and so is treated as one major aspect of integrated Earth system science and planetary science.
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