Earth Science Conservation Review

Soldierstown Quarry, Moira Clay-with-Flints
Summary Full report
Site Type:
Site Status: ESCR
Council area: Lisburn & Castlereagh City Council
Grid Reference: J156633
Bing maps: 54.50537,-6.21541
Google maps: 54.50537,-6.21541
Rocks
Rock Age: Cretaceous, Tertiary
Rock Type: Chalk, Clay, Flint, Basalt
Interest
Summary of site:
Soldierstown Quarry provides access to an infrequently exposed deposit called the Clay-with-flints (CwF). This deposit is found between the Cretaceous white limestone below and the Palaeogene black basalt above and spans a period of time of approximately 10 million years. Because of its location beneath the basalt, the CwF is usually only exposed at the edge of the Antrim Plateau.
The Cretaceous white limestone formed on the bottom of a sea floor around 75 million years ago, during a time when the island of Ireland was completely covered by a warm, clear, shallow sea. As the sea level eventually dropped, the resulting limestone was exposed and it underwent a long period of weathering. This would have led to the development of a landscape similar to that of the Burren in Co. Clare, with abundant limestone pavement and associated hollows and caves. The Cretaceous limestone contains abundant nodules and layers of flint, a silica-rich material that does not dissolve in rainwater, unlike the limestone. As weathering continued, it left behind the more robust flints that accumulated on the limestone landscape.
At the beginning of the Palaeogene period, about 65 million years ago, volcanic activity began as a result of stretching and thinning of the crust when the North American and European tectonic plates pulled apart. The resulting lava flows covered much of Northern Ireland and preserved the top surface of the Cretaceous limestone, covering the CwF.
As its name suggests, the CwF is made up of two main components, namely flints, held together by varying quantities of clay. The colour of the clay varies greatly, as does the overall thickness of the deposit. Its position between the underlying white limestone and the overlying black basalt provides information on the environment at that time.
The origin of the CwF has been a subject of great debate amongst geologists. It was initially thought to be a result of weathering at the surface to produce the flint, combined with the residue left behind from the dissolution of the white limestone to produce the clay. Whilst this is correct in the case of the flint, the origin of the clay is more doubtful. Another theory is that the clay component came from an explosive volcanic event that would have produced abundant volcanic material including ash. This would have occurred before the main basalts started forming. The most recent theory indicates that the clay probably came from localised mudflows. These would have contained clays derived from the weathering of basalts which would have been plentiful at the beginning of the Palaeogene period.
SITE SPECIFIC SUMMARY INFORMATION TO BE ADDED

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