The Principles of Stratigraphical GeologyMarr, J. E. (John Edward)
Science
The Principles of Stratigraphical Geology
Marr, J. E. (John Edward)
Geology, Stratigraphic
-----------------+------------------+-------------------+-----------------
Gloucestershire, | South | N. |
&c. | Northamptonshire | Northamptonshire | Yorkshire
| | and Lincoln |
-----------------+------------------+-------------------+-----------------
Cornbrash | Cornbrash | Cornbrash | Cornbrash
-----------------+------------------+-------------------+-----------------
Great Oolite | Great Oolite | Great Oolite Clay |
| (Upper part) | Great Oolite | Upper
| | Limestone |
| | Upper | Estuarine
| Northamptonshire | Estuarine |
............... | ................ | ................. | ................
| | Series | Series
| | Lincolnshire | Scarbro'
| | Limestone | Limestone
| Sands | | Middle Estuarine
| | | Series
Inferior Oolite | | Lower Estuarine | Millepore Oolite
| | Series |
| | | Lower Estuarine
| | | Series
-----------------+------------------+-------------------+-----------------
Upper Lias | Upper Lias | Upper Lias | Upper Lias
-----------------+------------------+-------------------+-----------------
The dotted line shows roughly the division between Bathonian
and Bajocian.
The changes may be explained very simply if we leave out of account
for the moment the development of Lincolnshire Limestone, with its
equivalent the Scarbro' Limestone, and the Millepore series. The beds
in Gloucestershire and other south-western counties are essentially
marine; whilst in Northamptonshire and Lincolnshire estuarine
conditions set in after the deposition of the Upper Lias, and
continued throughout the deposition of the Bajocian and Lower
Bathonian beds, being replaced by marine conditions during the
formation of the Upper Bathonian strata, and still further north in
Yorkshire the estuarine conditions generally prevailed throughout
Bajocian and Bathonian times. These changes point to the existence of
land towards the north. The general simplicity is modified by
temporary prevalence of marine conditions twice over (during the
deposition of the Millepore Oolite and the Scarbro' Limestone) in
Yorkshire, and once (during the deposition of the Lincolnshire
Limestone) in Lincolnshire.
Public-domain text, read in full here on John Shaqi.
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