Vocabularies — view dictionary terms
DIC_ROCK_NAMEV3 (3025 rows)
Dictionary table which is part of version 3 of the BGS Rock Classification Scheme. The main part of the RCS - it contains only single lithologies.
Displaying rows 206 to 225 of 3025
| Row | CODE | DESCRIPTION | RCS_STATUS | TRANSLATION | Q1 | Q2 | Q3 | Q4 | USER_ENTERED | DATE_ENTERED | USER_UPDATED | DATE_UPDATED | TRANSFER | DEFINITION_BKING | STATUS |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| 206 | BCS | Boulders, clayey, sandy [Unlithified Deposits Coding Scheme] | U | Sandy clayey boulders [UDCS] | clayey | sandy | DJLO | 20-FEB-09 | TMCM | 30-AUG-18 | I | Not Available | C | ||
| 207 | BCSV | Boulders, clayey, sandy, gravelly [Unlithified Deposits Coding Scheme] | U | Gravelly sandy clayey boulders [UDCS] | clayey | sandy | gravelly | DJLO | 20-FEB-09 | TMCM | 30-AUG-18 | I | Not Available | C | |
| 208 | BCV | Boulders, clayey, gravelly [Unlithified Deposits Coding Scheme] | U | Gravelly clayey boulders [UDCS] | clayey | gravelly | DJLO | 20-FEB-09 | TMCM | 30-AUG-18 | I | Not Available | C | ||
| 209 | BDCOAL | Banded-dull-coal - A type of bituminous-coal, classified according to brightness. British Geological Survey Research Report RR/99/03, section 6.1 and fig. 10. | R | Banded-dull-coal | GRBA | 24-FEB-00 | TMCM | 08-MAR-19 | Bituminous coal brightness type. Prefix defines type | C | |||||
| 210 | BENMOR | Benmoreite - A sodic trachyandesite. British Geological Survey Research Report RR/99/06, section 5.2 and figs. 17b, 20. | R | Benmoreite | GRBA | 24-FEB-00 | TMCM | 22-FEB-19 | Fine-grained, av.<0.25mm normal crystalline extrusive/intrusive rock; TAS SiO2 53-63wt%, Na2O+K2O 5.9-11.7wt%, (Na2O-2.0)>K2O. Sodic trachyandesite | C | |||||
| 211 | BGCCOL | Boghead-cannel-coal - A type of sapropelic-coal. It is a transitional stage between cannel-coal and boghead-coal in which miospores dominate over alginite. British Geological Survey Research Report RR/99/03, section 6.2 and fig. 10. | R | Boghead-cannel-coal | GRBA | 24-FEB-00 | TMCM | 08-MAR-19 | Sapropelic coal. Brown, mud-grade rock particles, >75% <0.032mm. Miospores >alginite. Macroscopically unstratified. Microscopically alginite with very finely dispersed inertinite & vitrinite. Torbanite | C | |||||
| 212 | BGCOL | Boghead-coal - A type of sapropelic-coal. It is similar to cannel-coal but browner and rich in alginite with very few miospores. It appears unstratified on macroscopic examination. Microscopic examination shows that boghead-coal consists of alginite and very finely dispersed inertinite and vitrinite. The proportion of alginite can vary widely. Boghead-coal is sometimes referred to as torbanite. This term is not recommended for usage. British Geological Survey Research Report RR/99/03, section 6.2 and fig. 10. | R | Boghead-coal | GRBA | 24-FEB-00 | TMCM | 08-MAR-19 | Sapropelic coal. Brown, mud-grade rock particles, >75% <0.032mm. Alginite dominant but variable, minor miospores. Macroscopically unstratified. Microscopically alginite with very finely dispersed inertinite & vitrinite. Torbanite | C | |||||
| 213 | BGFEOR | Bog iron-ore - A type of manganiferous/ferruginous deposit. It is a porous, earthy form of limonite (impure hydrous ferric oxide). British Geological Survey Research Report RR/99/04, section 4 and tables 5, 17. | R | Bog iron-ore | GRBA | 24-FEB-00 | TMCM | 13-MAR-19 | Genetic term for soft, spongy limonite deposit impregnated with plant debris/clay/clastic material. Precipitated from ferruginous water, oxidised by algae/iron bacteria/the atmosphere in bogs/marshes/shallow lakes. Particle size undefined. Bog-ironstone | C | |||||
| 214 | BGR | Boulders, granite [Unlithified Deposits Coding Scheme - Extended] | U | Granite boulders [UDCS-X] | granite | TMCM | 27-MAY-20 | I | Not Available | C | |||||
| 215 | BHAW | Hawaiite, basaltic | U | Basaltic hawaiite | basaltic | DJLO | 07-JUL-08 | TMCM | 31-AUG-18 | I | Not Available | C | |||
| 216 | BIODP | Biological deposit - A type of natural superficial deposit. The term describes a deposit directly formed and characterised by living organisms which secrete either silica or carbonate to form a skeleton or shell. British Geological Survey Research Report RR/99/04, appendix 2. | A | Biological deposit | GRBA | 24-FEB-00 | TMCM | 13-MAR-19 | Not Available | C | |||||
| 217 | BIOM | Deposit, mussel | U | Mussel deposit | mussel | AWEL | 09-JAN-02 | TMCM | 31-AUG-18 | Not Available | C | ||||
| 218 | BIOR | Biological rock - A type of biological deposit. In the Rock Classification Scheme, it is the consolidated equivalent of biological sediment. | A | Biological rock | GRBA | 24-FEB-00 | TMCM | 13-MAR-19 | Not Available | C | |||||
| 219 | BIOSD | Biological sediment - A type of biological deposit. In the Rock Classification Scheme, it is the unconsolidated equivalent of biological rock. | A | Biological sediment | GRBA | 24-FEB-00 | TMCM | 13-MAR-19 | Not Available | C | |||||
| 220 | BIOSND | Bioclastic sand deposit - A type of biological sediment. It consists of sand composed of broken and fragmental remains of organisms including shells, coral and lithothamnium algae. British Geological Survey Research Report RR/99/04, appendix 2. | A | Bioclastic sand deposit | GRBA | 24-FEB-00 | TMCM | 13-MAR-19 | Silicicalstic sediment with >50% grains from pre-existing siliceous rocks. Grains >50% or predominantly sand-grade, 0.032 to 2mm. Contains 5-20% bioclasts, (fossil fragments). Bioclast composition & components depositional environment not defined | C | |||||
| 221 | BITCOL | Bituminous-coal - A type of coal. It is a member of the pure humic coal series. The members of the pure humic coal series can be ranked in order as peat (the unlithified form), lignite, bituminous-coal, and anthracite (the lithified forms) based on increasing carbon content and decreasing volatile content. Bituminous-coal is a black, hard and bright coal which typically breaks into rectangular lumps. The bituminous coals can be subdivided in two ways. The first scheme is based on lithotypes which are macroscopically recognisable bands of coal seams. This scheme can be used for describing individual specimens or discrete horizons within a coal seam. Using this scheme, bituminous-coal can be subdivided into vitrain, clarain, fusain, and durain. The second scheme describes the brightness of the coal, and should be used in the field to describe megascopically distinct layers of coal seams. Using this scheme, bituminous-coal can be subdivided into bright-coal, banded-bright-coal, banded-coal, banded-dull-coal, and dull-coal. British Geological Survey Research Report RR/99/03, section 6.1, table 16 and fig. 10. | A | Bituminous-coal | GRBA | 24-FEB-00 | TMCM | 08-MAR-19 | Lithified, hard, bright, black mixture of a wide range of plant debris of rarely discernable type. Fine-grained, 0.032-0.25mm organic matrix. 75 to 90% carbon, dry, ash-free. Volatiles 14 to 46%. Largely carbonised, breaks into rectangular lumps. | C | |||||
| 222 | BITDP | Bituminous deposit | U | Bituminous deposit | bituminous | AWEL | 25-FEB-00 | TMCM | 31-AUG-18 | Sediment with significantly high organic, dominantly of bituminous material, content to noticeably effect the lithology. A tar sand/bitumen lake. Alt. A humic black, hard, bright coal type with 75-90% carbon, dry ash-free & 14-46% volatiles. | C | ||||
| 223 | BKLIGN | Black-lignite - A type of lignite. It is dark brown to black with a silky lustre, and much harder than brown-lignite. British Geological Survey Research Report RR/99/03, section 6.1 and fig. 10. | R | Black-lignite | GRBA | 24-FEB-00 | TMCM | 08-MAR-19 | Lithified, dark-brown/black, silky lustre mixture of range of plant debris many individually discernable. Fine 0.032-0.25mm organic matrix. 60-75% carbon, dry, ash-free. Volatiles 46-63%. Partly carbonised, cracks/breaks on drying. Hardness >brown-lignite | C | |||||
| 224 | BL | Boulders, cobbly [Unlithified Deposits Coding Scheme] | U | Cobbly boulders [UDCS] | cobbly | AWEL | 17-DEC-04 | TMCM | 30-AUG-18 | Not Available | C | ||||
| 225 | BLBTPH | Block-bomb-tephra - A type of pyroclastic-sediment. In the Rock Classification Scheme, it is a pyroclastic-sediment in which the average size of more than 75% of the pyroclastic fragments exceeds 64 mm. Block-tephra, bomb-block-tephra, block-bomb-tephra, and bomb-tephra are separated according to the relative proportion of blocks (angular fragments exceeding 64 mm) and bombs (rounded fragments exceeding 64 mm): if between 25% and 50% of all pyroclastic fragments bigger than 64 mm are blocks the sediment is block-bomb-tephra. It is the unconsolidated equivalent of agglomerate. British Geological Survey Research Report RR/99/06, section 4.2 and fig. 4. | R | Block-bomb-tephra | AWEL | 17-DEC-04 | TMCM | 15-FEB-19 | Unimodal, well sorted, unlithified clastic material >10% debris formed by volcanic processes, >75% pyroclastic fragments, >75vol% >64mm blocks| C |
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Displaying rows 206 to 225 of 3025