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| Cushendun - Bay Hotel to Cave House tunnel - Devonian | Antrim |
| Site number: | 307 | File Number: | D23 |
| ESCC: | EC | ||
| Locality Type: | Coastal section | Status: | ESCR |
| Grid Reference: | D252327,D25253254 End(s) of linear site, Not Entered | ||
| Google maps: | 55.12614,-6.03731 | ||
| County: | Antrim | Council area: | Causeway Coast & Glens Borough Council |
| Period: | Devonian | ||
| Stages: | Lower Devonian | ||
| Lithostrat: | Cross Slieve Group, Cushendun Conglomerate | ||
| Site Description | |
|---|---|
| Description: | |
Exposed at Cushendun, east of the Bay Hotel (D252327) and at the spectacular cliff north of Cave House (D25253254) are conglomerates that are typical of the basal unit of the Cushendun Formation. They occur in laterally persistent beds, frequently up to 12m thick, and are interbedded with coarse-grained laminated sandstones. The conglomerates are clast-supported and well sorted, with a lithic arenite matrix and well rounded clasts which consist almost exclusively of quartzite and are attributed to a polycyclic origin. Cross-stratification is absent in the conglomerates. Sandstone beds are commonly eroded by the overlying conglomerates and in places are laterally impersistent. | |
| Notes: | |
For general information and reference list on the Cross Slieve Group see Key Site 1146 - Cross Slieve Group; Cushendun to Port Obe. For general information and reference list on the Devonian System in N. Ireland see Key Site 1147 - The Devonian System in N. Ireland - Introduction. | |
| Keywords | |
|---|---|
| Rocks: | Conglomerate, Sand, Sandstone |
| Structures: | cross-bedding |
| Map(s): | See the 1:50,000 O.S. Sheet 5 (Ballycastle). | ||
| Record type: | Environment Serv. GIS, ESCR report | ||
| Entered by: | Doughty, P.J. | ||
| Last updated: | 31 May 2006 | ||
| Enlander, I., Dempster, M. & Doughty, P., 2026. Cushendun - Bay Hotel to Cave House tunnel - Devonian, County Antrim, site details. [In] Earth Science Conservation Review. https://www.habitas.org.uk/escr/site.php?item=307. Accessed on 2026-11-06. |
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