Loxter Ashbed Quarry Champions Site
Geological overview
Loxter Ashbed is a disused limestone quarry. The geology of Loxter Ashbed Quarry dates to the Silurian period of time, approximately 422 million years ago. The rocks are limestones and belong to the Aymestry Limestone Formation. The site is a wonderful example of an anticline together with offering a few fossils.
Loxter Ashbed Quarry is a Community Conservation Champions site. The ‘Champions’ are a loosely knit group of volunteers who are actively involved in the maintenance and public promotion of 19 geological sites spread across the counties of Herefordshire and Worcestershire. They are engaged in a wide range of activities which vary according to the nature of the site.
Location
Wellington Heath, Herefordshire
Access
The site is on private land. Access available to groups by prior arrangement. Please email or phone Mandy on 01531 634303 to arrange a visit.
Geological Age
Silurian – Aymestry Limestone Formation
Rock Types
Sedimentary – Limestone, shale
Features
Anticlinal folding
Area structural geology setting
Fossils
Interpretation
2 x Interpretation boards
