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in Fife. The rocks of the
Stratheden Group have also previously been referred to as the Upper Old Red Sandstone. It unconformably overlies a variety of other rock sequences including the
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N.H. Trewin. & M.F. Thirlwall The
Geological Society (2002). Trewin, N.H. (ed.).
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306:(4. ed.). London: Geological Society Publishing. pp. 242–243.
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211:. Occasionally pebbly, this red-brown and yellow
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352:Geologic formations of the United Kingdom
347:Geological groups of the United Kingdom
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235:in the east. The name is derived from
7:
281:The BGS Lexicon of Named Rock Units
14:
16:Geological group in Great Britain
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61:Knox Pulpit Sandstone Formation
1:
231:to the northeastern parts of
215:dominated unit also contains
57:Glenvale Sandstone Formation
53:Burnside Sandstone Formation
283:. British Geological Survey
227:in the west and across the
65:Bute Conglomerate Formation
368:
332:Silurian System of Europe
26:
253:Arbuthnott-Garvock Group
89:Arbuthnott-Garvock Group
304:The Geology of Scotland
223:. It is encountered in
342:Geology of Scotland
28:Stratigraphic range
337:Geology of England
277:"Stratheden Group"
251:and Arran and the
194:lithostratigraphic
207:and northernmost
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255:in Fife and the
241:Strathmore Group
199:(a sequence of
187:Stratheden Group
178:Stratheden, Fife
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85:Strathmore Group
75:Inverclyde Group
22:Stratheden Group
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229:Midland Valley
203:) in southern
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130:conglomerates
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285:. Retrieved
280:
271:
186:
184:
169:Type section
201:rock strata
98:up to 1500m
326:Categories
263:References
237:Stratheden
217:siltstones
287:August 8,
245:Dumbarton
221:mudstones
213:sandstone
174:Named for
126:siltstone
112:sandstone
103:Lithology
95:Thickness
71:Underlies
49:Sub-units
249:Stirling
205:Scotland
191:Devonian
136:Location
122:mudstone
81:Overlies
32:Devonian
257:Kinross
243:around
209:England
151:Country
108:Primary
30:: Late
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259:area.
160:
145:Europe
141:Region
225:Arran
197:group
189:is a
118:Other
43:Group
34:epoch
308:ISBN
289:2016
233:Fife
219:and
185:The
39:Type
328::
279:.
247:,
163:UK
128:,
124:,
87:,
63:,
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316:.
291:.
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