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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 306 to 325 of 3025
| Row | CODE | DESCRIPTION | RCS_STATUS | TRANSLATION | Q1 | Q2 | Q3 | Q4 | USER_ENTERED | DATE_ENTERED | USER_UPDATED | DATE_UPDATED | TRANSFER | DEFINITION_BKING | STATUS |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| 306 | CATUFA | Tufa, calcareous - A type of tufa. British Geological Survey Research Report RR/99/04, section 4 and tables 5, 17. | U | Calcareous tufa | calcareous | GRBA | 24-FEB-00 | TMCM | 13-MAR-19 | Thin, surficial, soft, spongy, semifriable, crystalline incrustation around the mouth of springs, seeps or streams carrying calcium carbonate in solution & exceptionally as thick deposits along lakeshores. 10 to 50% calcite/aragonite. Tufa-limestone. | C | ||||
| 307 | CB | Clay, bouldery [Unlithified Deposits Coding Scheme] | U | Bouldery clay [UDCS] | bouldery | AWEL | 09-JAN-02 | TMCM | 30-AUG-18 | Not Available | C | ||||
| 308 | CBCOAL | Cannel-boghead-coal - A type of sapropelic-coal. It is a transitional stage between cannel-coal and boghead-coal in which alginite dominates over miospores. British Geological Survey Research Report RR/99/03, section 6.2 and fig. 10. | R | Cannel-boghead-coal | GRBA | 24-FEB-00 | TMCM | 08-MAR-19 | A sapropelic coal. Mud-grade, >75% <0.032mm rock. Alginite > miospores, dull black, waxy lustre, homogeneous, conchoidal fracture. Microstratification & siderite common. Microscopically macerals finer, more uniform & intimately mixed than in humic coal. | C | |||||
| 309 | CBFEST | Ironstone, carbonaceous | U | Carbonaceous ironstone | carbonaceous | AWEL | 31-MAY-02 | TMCM | 31-AUG-18 | Sedimentary rock, no recognisable depositional texture with clasts >50% iron-bearing minerals (>15wt% iron). Clast size not defined. 5-20%visible carbon/humic material. | C | ||||
| 310 | CBL | Clay, bouldery, cobbly [Unlithified Deposits Coding Scheme] | U | Cobbly bouldery clay [UDCS] | bouldery | cobbly | DJLO | 20-FEB-09 | TMCM | 30-AUG-18 | I | Not Available | C | ||
| 311 | CBP | Clay, bouldery, peaty [Unlithified Deposits Coding Scheme] | U | Peaty bouldery clay [UDCS] | bouldery | peaty | AWEL | 17-MAR-04 | TMCM | 30-AUG-18 | Not Available | C | |||
| 312 | CBRMY | Carbonate-rock, mylonitic | U | Mylonitic carbonate-rock | mylonitic | AWEL | 21-JAN-02 | TMCM | 31-AUG-18 | Deformed (ductile), intensely foliated rock (protolith, >50% crystals carbonate) with primary cohesion, containing 10-50% porphyroclasts(commonly lensoid with tails indicating shearing sense) in a finer grained dynamically recrystallised matrix | C | ||||
| 313 | CBT | Carbonatite - A type of exotic crystalline igneous rock. In the Rock Classification Scheme, it is defined as an igneous rock that contains more than 50% modal primary carbonate. It is known to occur in extrusive, shallow and deep-seated environments. British Geological Survey Research Report RR/99/06, section 6.1 and figs. 25, 26. | A | Carbonatite | GRBA | 24-FEB-00 | TMCM | 22-FEB-19 | Exotic crystalline intrusive/extrusive rock; >50% modal primary carbonates of calcium/magnesium/iron/manganese | C | |||||
| 314 | CEL | Celestine | - | Celestine | DJLO | 13-FEB-07 | TMCM | 24-AUG-18 | I | Not Available | O | ||||
| 315 | CELN | Celestine, nodular | - | Nodular Celestine | nodular | DJLO | 13-FEB-07 | TMCM | 24-AUG-18 | I | Not Available | O | |||
| 316 | CERMIC | Ceramic waste - A type of artifical deposit. It consists of waste material from the pottery and ceramic industries, commonly comprising partly fired and fired clay products. British Geological Survey Research Report RR/99/04, appendix 1. | R | Ceramic waste | GRBA | 24-FEB-00 | TMCM | 13-MAR-19 | Not Available | C | |||||
| 317 | CESCH | Schist, chlorite-epidote | U | Chlorite-epidote schist | chlorite | epidote | AWEL | 11-JUN-02 | TMCM | 31-AUG-18 | Medium-grained (av. 0.25-2mm), crystalloblastic metamorphic rock (protolith undefined) splits into <5mm slabs/flakes defined by a well developed planar orientation of platy/prismatic minerals; chlorite| C |
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| 318 | CGHSCH | Schist, clinopyroxene-garnet-hornblende | U | Clinopyroxene-garnet-hornblende schist | clinopyroxene | garnet | hornblende | AWEL | 11-JUN-02 | TMCM | 31-AUG-18 | Medium-grained (av. 0.25-2mm), crystalloblastic metamorphic rock (protolith undefined) splits into <5mm slabs/flakes defined by a well developed planar orientation of platy/prismatic minerals; clinopyroxene| C |
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| 319 | CGR | Coarse-grained normal crystalline rock - In the Rock Classification Scheme, a crystalline rock is coarse-grained if its average crystal size is greater than 2 mm. This group corresponds to the plutonic division of the IUGS scheme. British Geological Survey Research Report RR/99/06, section 1.3 and figs. 1, 3 and 9. | A | Coarse-grained normal crystalline rock | AWEL | 08-JUN-01 | TMCM | 15-FEB-19 | Coarse-grained, av. between 2-16mm chemically/mineralogically normal intrusive rock; includes most of volume of coarse-grained igneous rocks | C | |||||
| 320 | CH | Clay, shelly [Unlithified Deposits Coding Scheme - Extended] | U | Shelly clay [UDCS-X] | shelly | TMCM | 27-MAY-20 | I | Not Available | C | |||||
| 321 | CHARNR | Rock, charnockitic - A type of coarse-grained normal crystalline rock. The charnockitic suite of rocks is usually characterised by the presence of orthopyroxene (or fayalite plus quartz, though in such assemblages fayalite is invariably altered) and, in many such rocks, perthite, mesoperthite or antiperthite. Primary hydrous minerals are generally absent. They are commonly associated with norites and anorthosites and are linked closely with high-grade metamorphic terrains. Despite being composed largely of feldspar and quartz, charnockitic rocks are generally melanocratic due to very dark feldspar crystals, which also have a characteristically greasy appearance. British Geological Survey Research Report RR/99/06, section 5.1. Examples (root name and qualifier): charnockitic granite, charnockitic monzonite, charnockitic tonalite. | U | Charnockitic rock | charnockitic | GRBA | 24-FEB-00 | TMCM | 22-FEB-19 | Coarse-grained, av. between 2-16mm normal crystalline intrusive rock with perthitic feldspars (usually dark coloured), magnetite & pyroxene (usually orthopyroxene, commonly hypersthene or altered fayalite & quartz) | C | ||||
| 322 | CHDMTN | Diamicton, chalk-rich | U | Chalk-rich diamicton | chalk-rich | AWEL | 10-JUN-02 | TMCM | 31-AUG-18 | Poorly-sorted sediment with wide clast size range, >50% clasts from pre-existing siliceous rocks, <50% >2mm. >20% of clasts chalk (friable porous sedimentary rock, >50% calcite/aragonite particles largely of biogenic origin, usually white & fine-grained). | C | ||||
| 323 | CHEMDP | Chemical deposit (natural superficial) - A type of natural superficial deposit. It consists of sediments formed primarily by precipitation from solution or colloidal suspension or by the deposition of insoluble precipitates. British Geological Survey Research Report RR/99/04, appendix 2 and tables 5, 17. | A | Chemical deposit (natural superficial) | GRBA | 24-FEB-00 | TMCM | 13-MAR-19 | Not Available | C | |||||
| 324 | CHEMWU | Chemical waste - A type of artifical deposit. It consists of waste material and by-products derived from the chemical industry and chemical processes. British Geological Survey Research Report RR/99/04, appendix 1. | R | Chemical waste | GRBA | 24-FEB-00 | TMCM | 13-MAR-19 | Not Available | C | |||||
| 325 | CHINAW | China clay waste - A type of artifical deposit. It consists of kaolin and waste materials derived from the extraction of kaolin from granitic rocks. British Geological Survey Research Report RR/99/04, appendix 1. | R | China clay waste | GRBA | 24-FEB-00 | TMCM | 13-MAR-19 | Not Available | C |
Displaying rows 306 to 325 of 3025