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keuper+waterstones Latitude and Longitude:

53°00′N 1°12′W / 53.0°N 1.2°W / 53.0; -1.2
From Wikipedia, the free encyclopedia
Keuper Waterstones
Stratigraphic range: Anisian
~247–242  Ma
O
S
D
C
P
T
J
K
N
Type Formation
Unit of Mercia Mudstone Group
Lithology
Primary Sandstone
Location
Coordinates 53°00′N 1°12′W / 53.0°N 1.2°W / 53.0; -1.2
Approximate paleocoordinates 16°00′N 11°24′E / 16.0°N 11.4°E / 16.0; 11.4
Region England
Country  United Kingdom
Keuper Waterstones is located in the United Kingdom
Keuper Waterstones
Keuper Waterstones (the United Kingdom)
Keuper Waterstones is located in England
Keuper Waterstones
Keuper Waterstones (England)

The Keuper Waterstones is a geologic formation in England. It preserves ichnofossils of Varanopus aff. curvidactylus, Swinnertonichnus mapperleyensis, Deuterotetrapous plancus, Chirotherium swinnertoni, Microsauropus acutipes and Erpetopus willistoni dating back to the Middle Triassic ( Anisian) period. [1]

See also

References

Further reading

  • W. A. S. Sarjeant. 1967. Fossil footprints from the Middle Triassic of Nottinghamshire and Derbyshire. The Mercian Geologist 2:327-341
  • H. H. Swinnerton. 1910. Organic remains in the Trias of Nottingham. Geological Magazine, decade 5 7(5):229

keuper+waterstones Latitude and Longitude:

53°00′N 1°12′W / 53.0°N 1.2°W / 53.0; -1.2
From Wikipedia, the free encyclopedia
Keuper Waterstones
Stratigraphic range: Anisian
~247–242  Ma
O
S
D
C
P
T
J
K
N
Type Formation
Unit of Mercia Mudstone Group
Lithology
Primary Sandstone
Location
Coordinates 53°00′N 1°12′W / 53.0°N 1.2°W / 53.0; -1.2
Approximate paleocoordinates 16°00′N 11°24′E / 16.0°N 11.4°E / 16.0; 11.4
Region England
Country  United Kingdom
Keuper Waterstones is located in the United Kingdom
Keuper Waterstones
Keuper Waterstones (the United Kingdom)
Keuper Waterstones is located in England
Keuper Waterstones
Keuper Waterstones (England)

The Keuper Waterstones is a geologic formation in England. It preserves ichnofossils of Varanopus aff. curvidactylus, Swinnertonichnus mapperleyensis, Deuterotetrapous plancus, Chirotherium swinnertoni, Microsauropus acutipes and Erpetopus willistoni dating back to the Middle Triassic ( Anisian) period. [1]

See also

References

Further reading

  • W. A. S. Sarjeant. 1967. Fossil footprints from the Middle Triassic of Nottinghamshire and Derbyshire. The Mercian Geologist 2:327-341
  • H. H. Swinnerton. 1910. Organic remains in the Trias of Nottingham. Geological Magazine, decade 5 7(5):229

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