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Earth Science Conservation Review

Summary Full report
Cumber - site of local interestLondonderry
Site number:721
Locality Type:Inland exposure Status: local interest
Grid Reference: C544074 Approximate
Google maps: 54.91173,-7.15177
County: LondonderryCouncil area:Derry City & Strabane District Council
Period:Quaternary
Site Description
Highlights:
The Cumber delta is bounded by the erosive slopes along the present courses of the Glenrandel and Faughan rivers which limit a relatively flat and extensive surface between the townlands of Binn [C557 061] and Upper Binn [C564 053]. This surface represents the topset surface of the delta. The delta’s large-scale foresets record the former presence of an extraglacial lake occupying the Faughan and Foreglen depression as ice retreated generally southwards from the north coast of Ireland towards the Sperrin Mountains. Large-scale lake formation indicates the presence of ice dams blocking the lower reaches of the Faughan and Roe valleys, forming an association of the deposit with the Ballykelly moraine.
Description:
The Cumber delta consists of two discrete delta fragments, having been dissected along the course of the present day Glenrandel river. It is bordered on its northern and northeastern margins by the River Faughan. The main delta surface at Binn [C557 056] consists of a plateau of low relief (<5m) lying at 126m O.D. An area of low amplitude, hummocky terrain occurs at Tullintrain [C558 053] where small-scale hollows in the surface are occupied by raised bogs and lakes. A large-scale depression in the gravels [C550 053] contains post-glacial alluvium. The hummocky terrain is truncated abruptly on its southern margins by a relatively steep, 6m high slope running parallel to the Longland Road at this location. Further south and southeast, approximately 2km2 of gravels are banked against the rising slopes of Slieveboy Hill [C560 033] and extend southeastwards towards Clagan [C582 048]. The exposure at Robinson’s quarry [C538 061] shows a sequence consisting of conformably bedded sands overlain unconformably by pebble and cobble gravels.



The sediments consist mainly of large-scale foreset sequences which are associated with deposition in ponded water up to 126m O.D. The well-preserved flat top of the plateau represents a topset gravel sequence which prograded over foresets as water levels shallowed. Palaeocurrent directions of the foreset beds to the north and northwest indicate that ice was retreating generally to the south and east along the western part of the Foreglen depression into the Sperrins. The general absence of morainic ridges indicates that the deltas were probably fed from subglacial sources emanating from ice-margins grounded in water. The absence of glaciotectonic activity suggests that the ice margins were halting for short periods with no major ice-marginal re-advances. The foresets exposed at Robinson’s quarry form a typical glaciofluvial delta deposited near a subglacial efflux.
Importance:
The landforms at Cumber are of scientific value as they assist in the reconstruction of late glacial depositional environments along the Faughan Basin depression.
Notes:
The flat-topped delta dominates the skyline topography east to west along the Faughan River valley, especially near Claudy.



See also ESCR Key Site 471 - Cumber Delta, Dungiven Basin and Key Site 504 - Faughan and Dungiven Basins [Sand and Gravel Landscapes Block].
Keywords
Rocks:Gravel, Sand
Relations:Deltaic sediments, Glacio-fluvial sediment, Glaciolacustrine deposit
Geomorph:deltaic foresets, deltas
Paleoenv:delta, glacial
Access
Approach:The Cumber delta is bounded by the erosive slopes along the present courses of the Glenrandel and Faughan rivers just south of the B74 Claudy - Feeny road.
Uses
Educ. Level:The site is of educational value to researchers and students of glaciology.

Record type: SLNCI Report    
Entered by: E M Porter
Last updated:09/10/03

 Enlander, I., Dempster, M. & Doughty, P., 2026. Cumber - site of local interest, County Londonderry, site details. [In] Earth Science Conservation Review.
https://www.habitas.org.uk/escr/site.php?item=721. Accessed on 2026-11-06.

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