Northern England in
the Jurassic period (204 to 145 Ma).
Lower Jurassic rocks at Redcar |
By Jurassic times Britain had reached the latitude of the present day Mediterranean. During this period the North York Moors area was a subsiding basin. This factor, together with a eustatic (worldwide) rise in sea-level, led to thousands of feet of sediment being deposited in this basin during Jurassic times. During late Cretaceous- Tertiary times, due to Earth movements, the basin was inverted. The rocks are divided into Lower, Middle and Upper Jurassic. The first marine sediments (Lower Jurassic) that were deposited are known as the Lias Group. They are a thick sequence of richly fossiliferous mudstones (calcareous in part), siltstones, shallow marine sandstones and ironstones, the latter composed predominantly of an iron carbonate, siderite. Abundant ammonites, e.g. Arietites and Dactylioceras allow a very precise dating and correlation of the sequence. It is within this Group that, in addition to the ironstones, the alum shales and jet rock are found all of which were of economic importance historically. |
During Middle Jurassic times, a delta, or coastal plain
spread from the landmass to the north. This deposited a sequence of
sandstones, siltstones, shales and minor
coals. There were, however, at least two marine transgressions during Middle
Jurassic times. Middle Jurassic rocks are famous for fossil dinosaur footprints
which can be seen on the shore in fallen blocks of the Saltwick
(Hayburn) Fm. between Whitby and Saltwick Bay, and also on the shore in rocks of the Scalby Fm. at Burniston, north of Scarborough. |
|
|
A return to fully marine conditions occurred during
Upper Jurassic times and the rocks of this age consist of marine limestones,
calcareous sandstones and mudstones. The resistant calcareous sandstones and
limestones in fact form a distinct north facing scarp in the southern North
York Moors as well as the reef at Filey Brigg. The
steep slope of Newgate Bank on the Stokesley-Helmsley
road, for example, and the slope leading up to the Hole of Horcum are due to this scarp. The youngest Jurassic rocks
in Yorkshire are mudstones, the Kimmeridge Clay
which is the principal source rock for North Sea oil. Unfortunately it is
very poorly exposed. It can be seen at the base of the cliffs near Speeton, S.E. of Filey when
there is not too much sand. |