Geological glossary
| Alluvial fan | A fan-shaped deposit of material deposited at the mouth of a gorge or valley where it emerges onto less steeply sloping terrain. | 
| Anticline | A type of fold, where the rocks are folded upwards into an arch. | 
| Bed | A layer of sedimentary rock. Beds can vary in thickness from a few millimetres to many metres. | 
| Breccia | A sedimentary rock made up of angular fragments of rock in a finer- grained matrix. Similar to cemented scree. | 
| Calcite | A mineral made of calcium, carbon and oxygen — CaCO3; the main (calcium carbonate) component of limestone and marble. | 
| Conglomerate | A sedimentary rock made up of rounded cobbles and boulders of rock in a finer-grained matrix. | 
| Crinoid | A fossil sea lily made up of small ossicles or plates of calcium carbonate. These plates are the major constituent of crinoidal limestone. | 
| Cross-bedding | A feature of sedimentary rocks deposited by flowing water or strong tidal currents, where the sediment is lain down in sloping laminae. | 
| Cryoturbation | Disturbance to the soil caused by repeated freezing and thawing, typically under periglacial conditions. | 
| Diagenesis | A term used to describe the process of how sediment is transformed into rock. | 
| Dolomite | A mineral made of calcium, magnesium, carbon and oxygen — CaMg(CO3)2; also the name given to a rock made up of dolomite. | 
| Galena | Lead sulphide — PbS.A heavy, grey shiny mineral with cubic cleavage. Principal lead ore mined on Mendip. | 
| Gruffy ground | A local term used to describe the uneven ground produced by mining, possibly derived from ‘groovy ground’. | 
| Inlier | A term used to describe an area of older rocks surrounded by younger rocks. | 
| Karst | A term used to describe a limestone landscape. Karst features include caves, sinking streams, closed depressions and dry valleys. | 
| Limestone | A sedimentary rock consisting mainly of calcium carbonate grains such as ooliths, shell and coral fragments and lime mud. Often fossiliferous. | 
|  | A fine-grained, wind-blown silty soil, often derived from rock flour produced by glaciers. | 
| Oolith | A grain of calcium carbonate formed by precipitation of calcium carbonate around a nucleus, much like a pearl. A limestone made of ooliths is known as an oolite. | 
| Outlier | A term used to describe an area of younger rocks surrounded by older rocks. | 
| Pericline | A type of fold, similar to anticline where the rocks are folded upwards, but plunging at each end, forming an elongate structure like an upturned boat. | 
| Periglacial | A term used to describe very cold conditions. Often used to denote the climate or environment close to the edge of an ice sheet. | 
| Phreatic | A term used to describe caves which were formed below the water table. | 
| Rake | A miner’s term for a mineral vein. | 
| Scree | A deposit of angular rock fragments at the base of a cliff, often formed by frost shattering during periglacial climates. | 
| Smithsonite | Zinc ore. Zinc carbonate — ZnCO3, also known as calamine. | 
| Sump | Water-filled cave passage, sometimes passable by cave divers. | 
| Swallet | A local term for a stream sink, commonly developed at the contact between the  | 
| Syncline | A type of fold, where the rocks are folded downwards into a U-shape. | 
| Thrust fault | A fault that is near horizontal or gently dipping, and along which older rocks have been forced over younger rocks. | 
| Unconformity | A term used to describe the surface between two sets of rocks where there is a time gap or a layer of rocks missing. Where the younger rocks are folded at a different angle to those above, this is termed an angular unconformity. | 
| Vadose | A term used to describe caves which were formed above the water table. | 
| Wadi | An Arabic term used to describe an ephemeral water course, only active after storms or during the rainy season. | 
