This report describes the surface geology of the 1:10 000 Series sheet
SD 55 NW, part of the 1:50 000 Series sheet 59 (Lancaster). Detailed
descriptions of the geological sequence encountered in the Wyresdale Tunnel,
which crosses beneath the eastern part of this area, can be found in Johnson
(1981) and Wilson et al. (1989).
The area was first mapped at the 1:10 560 scale by J.R. Dakyns and
R.H. Tiddeman in 1875-76 and published at the 1:10 560 scale in 1880 as parts
of the Lancashire County Series sheets 30, 31, 34 and 35. In 1884 the
geological information was published at the 1:63 360 scale as part of the Old
Series sheet number 59 (Lancaster). During the present survey, the area to
the south-east of the Quernrnore to Garstang road (approximately three quarters
of the sheet) was mapped by Dr A.A. Wilson in 1984, as part of the BGS work
commissioned by the North-west Water Authority in response to the Abbeystead
Explosion Public Enquiry. Several, significant and previously unknown marine
band localities were discovered by Dr Wilson during this survey. The remainder
of the sheet was surveyed by Dr R.A. Hughes in 1988. A limited amount of field
work was carried out by Dr A Brandon in 1990 and parts of the geological
mapped revised.
The area is one of hilly pastureland, marginal to the high, heather covered
moorland of the Bowland Fells to the north-east. The rugged escarpment of
Clougha extends into the north-east corner of the sheet, the highest point
[5492 5939] being 421 m above Ordnance Datum. In the west, the north-east
trending valley of the River Conder is the major topographical feature, and
drains to the south. The lowest point is at the western end of the Conder
valley [579 500], where elevation is less than 45 m above Ordnance Datum. To
the east of the Conder valley the main lines of drainage flow from north to
south along a series of glacial meltwater channels. The only centre of
habitation is the ribbon development of Quernrnore [59 51].
The north-eastern part of the area was mapped by Moseley (1954). A detailed
geological log of the Wyresdale Tunnel, constructed to link the drainage
systems of the Rivers Lune and Wyre, was made by E.W. Johnson, N.
Aitkenhead, J.I. Chisholm, R.S. Arthurton, and D.J.C. Mundy of the BGS,
during construction. The results were published in a sedimentological
synthesis by Johnson (1981), who described the succession in terms of a
prograding delta-front sequence. Following the Wyresdale Tunnel explosion in
May 1984, the BGS surveyed the area in an attempt to identify the source and
the trap of the methane which exploded. A description of the geology as found
during this survey is given in Wilson, Brandon, and Johnson (1989). All
fossils recorded in this report were identified by Dr N.J.Riley.
Subsequent to the preparation of the original draft report the stratigraphy
and geological map of the area has been revised, particularly with regards to
the Roeburndale Formation. This report therefore includes parts revised by Dr
A Brandon in consultation with Or A A Wilson
Is data on this page outdated, violates copyrights or anything else? Report the problem now and we will take corresponding actions after reviewing your request.