Field Trips which took place in 2011
May 8th: Leader: Gordon Liddle. Upper Carboniferous and Permian, Tynemouth. An interpretation of the deltaic sediments of the Upper Carboniferous as seen at the North Tyneside coast.The excursion examined the Tertiary dyke at Tynemouth intruding the Carboniferous material, noting the Permian Unconformity and the interpretation of the sediments. The ballast beach at Tynmouth allowed some exotic material to be seen. The party then moved on to the Cullercoats area, about 1 mile north. Here the 90 fathom Fault was examined together with the effects on the intruded sediment. The coast at Hartley, about 2 miles North was then visited to examine the local effects of faulting. Click here for a full report.         For explanatory photo's, click here.

June 19th: Visit to Whitby - Saltwick Bay, led by Dr. Martin Whyte of Sheffield University. The purpose of the visit was to study the succession and depositional features of the Lower and Middle Jurassic Formations exposed there with the emphasis on identifying dinosaur tracks and other fossils. The party met at 10.30 am in the Whitby Abbey Car Park NZ 905110  (pay and display). Members of the Natural History Society of Northumbria and O.U.G.S. were invited to this field trip. For a full report, click here.

July 2nd: Upper Tees Drumlins: Members of N.E.G.S. were cordially invited to this event organised by the Natural History Society of Northumbria.
Time: 1030am. Meeting place: Cow Green Reservoir Car Park NY811308. Length of visit: 4-5 hours
This trip examined the drumlins that can be observed within the upper Tees valley, particularly around Cow Green Reservoir. These drumlins indicate the former existence of an ice centre over Cross Fell and adjacent parts of the Pennine escarpment. From the presence of a number of superimposed drumlins, this ice divide can be demonstrated to have migrated from a more northerly restricted location over westwards towards Cross Fell and Dufton Fell. Understanding the ice dynamics of such centres has been important in developing more accurate reconstructions of the last ice sheet to cover the British Isles. Leader:  Wishart Mitchell, Honorary Research Fellow, Department of Geography, Durham University.

July 16th: Glaciation and geomorphology around Kisdon, Upper Swaledale. Leader: Jon Barber, Ph.D., University of Leeds.
By kind invitation we joined Craven and Pendle Geological Society for this field trip.
Guide: Jon Barber Ph.D., University of Leeds Joint meeting with the North Eastern Geological Society
Time: 10:00 am at: the Resource and Heritage Centre in Keld,
Purpose: To examine landforms and sediments in the valleys and on the valley-side slopes around Kisdon, upper Swaledale, noting the effects of glaciation and glacier wastage, and how the landscape was later modified by fluvial and slope-forming processes. The effects of 19th century mining activity will be noted also. The area is a SSSI and is located in the Yorkshire Dales National Park.
For a full report, click here.

Aug. 6th.Time:10:00 am. Title:  The Ferryhill Gap.
Leader: Derek Teasdale, Quaternary Geologist
Description:The Ferryhill Gap is a huge incised valley cutting through the Magnesian Limestone escarpment south of Durham. 
It is the largest  glacial meltwater channel in North East England.  Extensive sands, gravels and lake deposits occur to the south. 
This visit examined questions surrounding the gap's formation, whilst exploring this spectacular landscape feature.
Meeting place:  Click here for a report & photo's.

Sep. 17th. Geology South of the Wear. "SUNDERLAND'S SECRET GEOLOGY" Leader Andy Lane
This field excursion took us to see some of the less well-known geological sights of the Sunderland area. That they are less well-known does not mean that they are not spectacular!   For a full report and photo's click here.

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