Spreadsheet: 077e512f-a6c2-4a0c-a3eb-f16e285ac80e
Sheet: stones

BUILDING_STONE_ID | STONE_NAME | PARENT BUILDING STONE  ID | ALTERNATIVE_NAMES | [NAME] | COLOUR | COLOUR_VARIATION | WEATHERED COLOUR | LITHOSTRATIGRAPHY | CHRONOSTRAT | STONE_LITHOLOGY | GRAIN_SIZE | [NAME] | KEY_IDENTIFICATION_FEATURES | FAILURE_WEATHERING | CONTEXT_OF_USE | LOCALITY_OF_USE | DATE_COMPILED | COMPILED_BY | MINERAL PLANNING AREA | English Heritage Atlas Area | SOURCE_OF_INFO | retrieval_date
5301 | Cobbles | 1 | Boulders | Well rounded lithic clasts of cobble- to boulder-grade (typically 10 to 30 cm in diameter, but sometimes more).  Commonly composed of well cemented sandstone or quartzite, but a broad spectrum of rock types is represented. |  | Variable | Variable (dependent on lithology) | GLACIAL DEPOSITS | [NAME] | NOT ENTERED | Medium grained | Variable - strongly dependent on lithology. | Rounded, reworked rock fragments of cobble- or boulder-grade.  Lithologically variable, but most likely to be of well-indurated sandstone/quartzite or of igneous origin. | Dependent on lithology, but generally robust having survived sedimentary recycling. | Used for walling purposes having received some or, on occasions, no dressing.  Occasionally cut ahead of use. | Within a coastal 'strip' extending roughly from Fraisthorpe in the north to [NAME] in the south, and inland approximately as far as the A165. | 2012-08-27 00:00:00 | SFP/GKL | East Riding of Yorkshire Council | EastYorkshire and Humber English Heritage Atlas Area | GKL/SFP personal knowledge; fieldwork | 2012-09-25 16:44:36
5302 | Chalk | 1 | Clunch | Fine-grained, white or grey carbonate lithology, which may or may not carry flint nodules. |  | Variable | Colour dulls.  Can take on shades of yellow and grey. | CHALK GROUP | [NAME] | CHALK | Very fine grained | Can be significantly fractured.  See also descriptions of individual Chalk Group formations below. | Fine-grained, calcareous nature.  May carry flints. | Liable to fragment. | Used as a walling stone either having been squared or having received little or no dressing. | To a limited degree in areas underlain by Chalk.  The likelihood is that much of the [NAME] seen, especially if it is white/off-white and flint-free, originates from the Flamborough Chalk Formation. | 2012-08-27 00:00:00 | SFP/GKL | East Riding of Yorkshire Council | EastYorkshire and Humber English Heritage Atlas Area | GKL/SFP personal knowledge; fieldwork | 2012-09-25 16:44:36
5303 | Flamborough Chalk | 5302 | Chalk | White, well-bedded, flint-free chalk with common [NAME] (typically about one per metre). |  | Variable | Colour dulls.  Can take on shades of yellow and grey. | FLAMBOROUGH CHALK FORMATION | [NAME] | CHALK | Very fine grained | Well-bedded; stylolitic seams present. | Flint-free, white chalk. | Liable to fragment. | Used as a walling stone either having been squared or having received little or no dressing. | To a limited extent within or close to its outcrop area (eastern and northern parts of the East Riding).  Much of the Chalk encountered, especially if it is flint-free, likely originates from this unit. | 2012-08-27 00:00:00 | SFP/GKL | East Riding of Yorkshire Council | EastYorkshire and Humber English Heritage Atlas Area | GKL/SFP personal knowledge; fieldwork; BGS sources. | 2012-09-25 16:44:36
5304 | [NAME] | 5302 | Chalk | White, thinly-bedded chalk with common tabular and discontinuous flint bands; sporadic [NAME]. |  | Variable | Colour dulls.  Can take on shades of yellow and grey. | BURNHAM CHALK FORMATION | [NAME] | CHALK | Very fine grained | Thinly bedded with common tabular and discontinuous flint bands. | White chalk with common flint bands. | Liable to fragment. | Used as a walling stone either having been squared or having received little or no dressing. | To an uncertain extent within or close to its outcrop area; not specifically identified during the course of this study. | 2012-08-27 00:00:00 | SFP/GKL | East Riding of Yorkshire Council | EastYorkshire and Humber English Heritage Atlas Area | BGS sources. | 2012-09-25 16:44:36
5305 | [NAME] | 5302 | Chalk | White, massive or thickly bedded chalk with common flint nodules ('burrow-form flints'), but generally lacking tabular flint bands; sporadic [NAME]. |  | Variable | Colour dulls.  Can take on shades of yellow and grey. | WELTON CHALK FORMATION | [NAME] | CHALK | Very fine grained | Massive or thickly bedded with common flint nodules ('burrow-form flints'). | White chalk with common flint nodules. | Liable to fragment. | Used as a walling stone either having been squared or having received little or no dressing. | To an uncertain extent within or close to its outcrop area; not specifically identified during the course of this study. | 2012-08-27 00:00:00 | SFP/GKL | East Riding of Yorkshire Council | EastYorkshire and Humber English Heritage Atlas Area | BGS sources. | 2012-09-25 16:44:36
5306 | [NAME] | 5302 | Chalk | Grey, soft, marly, flint-free chalk, typically weathering buff in exposures; locally includes pinkish bands; some harder, gritty, shell-debris-rich beds, and thin discrete marl seams. | GREY | Variable | Typically weathers to a buff colour. | FERRIBY CHALK FORMATION | [NAME] | CHALK | Very fine grained | Locally includes pinkish bands.  Some harder, gritty, shell-debris-rich beds, and thin discrete [NAME] also present. | Grey, soft, marly, flint-free chalk. | Liable to fragment. | Not specifically identified during the course of this study. | Not specifically identified during the course of this study. | 2012-08-27 00:00:00 | SFP/GKL | East Riding of Yorkshire Council | EastYorkshire and Humber English Heritage Atlas Area | BGS sources. | 2012-09-25 16:44:36
5307 | Lincolnshire Limestone | 1 |  | Limestone, typically calcilutites, peloidal wackestones and packstones in the lower part (Lower Lincolnshire Limestone) and high energy ooidal and shell fragmental grainstones in the upper part (Upper Lincolnshire Limestone).  Commonly includes sandy lime | WHITE | Variable | Can take on a variety of pale colours when weathered (yellows, oranges, browns). | LINCOLNSHIRE LIMESTONE FORMATION | JURASSIC | LIMESTONE, OOIDAL, SHELLY OR SPARRY | Medium grained | Bedding can be picked out by weathering. | Variably ooidal and bioclastic.  Weathering characteristics (Ancaster Stone often displays 'streaky bacon' texture). | Variable.  Blocks in general tend to weather well, but will disaggregate, spall and generally fail with time. | Variably as a main walling stone, dressings and repair work. | Across the East Riding as dressings and replacement blocks.  In its '[NAME] guise, used as a main walling stone in the Newbald-Cave-Brough area. | 2012-08-27 00:00:00 | SFP/GKL | East Riding of Yorkshire Council | EastYorkshire and Humber English Heritage Atlas Area | GKL/SFP personal knowledge; fieldwork; BGS Lexicon of Named Rock Units | 2012-09-25 16:44:36
5308 | [NAME] | 5307 | Cave Marble | Limestone, high energy ooidal and bioclastic grainstones, with fine-grained weakly or non-ooidal, shelly and/or silty limestone and calcareous siltstone in lower part. |  | Variable | Orange-brown colour in its most weathered state. | CAVE OOLITE [REDUNDANT NAME AND CODE: SEE ULL] | JURASSIC | LIMESTONE, OOIDAL | Medium grained | Cross-bedding can be picked out by weathering. | Typically [NAME] coloured, ooidal and variably bioclastic limestone found to the north of the Humber. | Variable.  Blocks in general tend to weather well, but will disaggregate, spall and generally fail with time. | Principally as a main walling stone, but has also seen use as dressings and seemingly for repair work. | Newbald-Cave-Brough area. | 2012-08-27 00:00:00 | SFP/GKL | East Riding of Yorkshire Council | EastYorkshire and Humber English Heritage Atlas Area | GKL/SFP personal knowledge; fieldwork; BGS Lexicon of Named Rock Units | 2012-09-25 16:44:36
5309 | Chalk | 1 | Clunch | Fine-grained, white or grey carbonate lithology, which may or may not carry flint nodules. |  | Variable | Colour dulls.  Can take on shades of yellow and grey. | CHALK GROUP | [NAME] | CHALK | Very fine grained | Can be significantly fractured.  See also descriptions of individual Chalk Group formations. | Fine-grained, calcareous nature.  May carry flints. | Liable to fragment. | Used as a walling stone either having been squared or having received little or no dressing. | To a limited degree in areas underlain by Chalk.  The likelihood is that much of the [NAME] seen, especially if it is white/off-white and flint-free, originates from the Flamborough Chalk Formation. | 2012-08-27 00:00:00 | SFP/GKL | North Lincolnshire Council | EastYorkshire and Humber English Heritage Atlas Area | GKL/SFP personal knowledge; fieldwork | 2012-09-25 16:44:36
5310 | Flamborough Chalk | 1 | Chalk | White, well-bedded, flint-free chalk with common [NAME] (typically about one per metre). |  |  |  | FLAMBOROUGH CHALK FORMATION | [NAME] | CHALK | Very fine grained | Well-bedded; stylolitic seams present. | Flint-free chalk. | Liable to fragment. |  | To a limited extent within or close to its outcrop area.  Much of the Chalk encountered, especially if it is flint-free, likely originates from this unit. | 2012-08-27 00:00:00 | SFP/GKL | North Lincolnshire Council | EastYorkshire and Humber English Heritage Atlas Area | BGS sources. | 2012-09-25 16:44:36
5311 | [NAME] | 1 | Chalk | White, thinly-bedded chalk with common tabular and discontinuous flint bands; sporadic [NAME]. |  |  |  | BURNHAM CHALK FORMATION | [NAME] | CHALK | Very fine grained | Thinly bedded. | Common flint bands. | Liable to fragment. |  | To an uncertain extent within or close to its outcrop area; not specifically identified during the course of this study. | 2012-08-27 00:00:00 | SFP/GKL | North Lincolnshire Council | EastYorkshire and Humber English Heritage Atlas Area | BGS sources. | 2012-09-25 16:44:36
5312 | [NAME] | 1 | Chalk | White, massive or thickly bedded chalk with common flint nodules ("burrow-form flints"), but generally lacking tabular flint bands; sporadic [NAME]. |  |  |  | WELTON CHALK FORMATION | [NAME] | CHALK | Very fine grained | Massive or thickly bedded. | Common flint nodules. | Liable to fragment. |  | To an uncertain extent within or close to its outcrop area; not specifically identified during the course of this study. | 2012-08-27 00:00:00 | SFP/GKL | North Lincolnshire Council | EastYorkshire and Humber English Heritage Atlas Area | BGS sources. | 2012-09-25 16:44:36
5313 | [NAME] | 1 | Chalk | Grey, soft, marly, flint-free chalk, typically weathering buff in exposures; locally includes pinkish bands; some harder, gritty, shell-debris-rich beds, and thin discrete marl seams. | GREY |  |  | FERRIBY CHALK FORMATION | [NAME] | CHALK | Very fine grained | Locally includes pinkish bands.  Some harder, gritty, shell-debris-rich beds, and thin discrete [NAME] also present. | Grey, soft, marly, flint-free chalk. | Liable to fragment. |  | Not specifically identified during the course of this study. | 2012-08-27 00:00:00 | SFP/GKL | North Lincolnshire Council | EastYorkshire and Humber English Heritage Atlas Area | BGS sources. | 2012-09-25 16:44:36
5314 | Lincolnshire Limestone | 1 |  | Limestone, typically calcilutites, peloidal wackestones and packstones in the lower part (Lower Lincolnshire Limestone) and high energy ooidal and shell fragmental grainstones in the upper part (Upper Lincolnshire Limestone).  Commonly includes sandy lime | WHITE | Variable | Can take on a variety of pale colours when weathered (yellows, oranges, browns). | LINCOLNSHIRE LIMESTONE FORMATION | JURASSIC | LIMESTONE, OOIDAL, SHELLY OR SPARRY | Medium grained | Bedding can be picked out by weathering. | Variably ooidal and bioclastic.  Weathering characteristics. | Variable.  Blocks in general tend to weather well, but will disaggregate, spall and generally fail with time. | Dressings | Quite commonly seen in older buildings located on the N–S trending outcrop of the Lincolnshire Limestone Formation.  More widely seen in ecclesiastical buildings as dressings. | 2012-08-27 00:00:00 | SFP/GKL | North Lincolnshire Council | EastYorkshire and Humber English Heritage Atlas Area | GKL/SFP personal knowledge; fieldwork; BGS Lexicon of Named Rock Units | 2012-09-25 16:44:36
5315 | [NAME] | 5314 |  | Limestone, high-energy ooidal and shell bioclastic grainstones, with 'non-oolitic limestone containing spar-filled shells' (probably secondarily recrystallized and micritized limestone) at base. |  |  |  | HIBALDSTOW LIMESTONE | JURASSIC | LIMESTONE, OOIDAL, OCCASIONALLY SHELLY OR SPARRY |  |  |  |  |  | Not specifically identified during the course of this study, but is almost certainly a source of some of the Lincolnshire Limestone encountered in North Lincolnshire. | 2012-08-27 00:00:00 | SFP/GKL | North Lincolnshire Council | EastYorkshire and Humber English Heritage Atlas Area | GKL/SFP personal knowledge; fieldwork; BGS Lexicon of Named Rock Units | 2012-09-25 16:44:36
5316 | Kirton Cementstones | 5314 |  | Silicate- and calcareous mudstone, interbedded with thin and more or less argillaceous limestones (calcilutite and shelly and peloidal wackestone). Locally includes coralliferous limestone bodies (knoll reef). |  |  |  | [NAME] | JURASSIC | MUDSTONE AND LIMESTONE |  |  |  |  |  | Recorded to only a limited degree during this study, but does see use as a rubblestone in areas where this Lincolnshire Limestone variant crops out. | 2012-08-27 00:00:00 | SFP/GKL | North Lincolnshire Council | EastYorkshire and Humber English Heritage Atlas Area | GKL/SFP personal knowledge; fieldwork; BGS Lexicon of Named Rock Units | 2012-09-25 16:44:36
5317 | [NAME] | 1 | Ironstone | Ferruginous, fossiliferous rock of variable appearance (reflecting the variable nature of its source unit, which comprises repeated alternations of grainstone-dominated ironstone and muddy ironstone including packstone, wackestone and mudstone). |  | Variable | Strongly dependent on iron content. | FRODINGHAM IRONSTONE MEMBER | JURASSIC | IRONSTONE |  |  | Variably but typically strongly ferruginous limestone-mudstone.  Commonly fossiliferous, with conspicuous [NAME]. | Quite variable – some blocks weather well, others less so. | Walling | Features quite prominently in villages underlain by or located close to the outcrop of the Frodingham Ironstone. | 2012-08-27 00:00:00 | SFP/GKL | North Lincolnshire Council | EastYorkshire and Humber English Heritage Atlas Area | GKL/SFP personal knowledge; fieldwork | 2012-09-25 16:44:36
5318 | Cobbles | 1 | Boulders | Well rounded lithic clasts of cobble- to boulder-grade (typically 10 to 30 cm in diameter, but sometimes more).  Commonly composed of well cemented sandstone or quartzite, but a broad spectrum of rock types is represented. |  | Variable | Variable (dependent on lithology) | GLACIAL DEPOSITS | [NAME] | NOT ENTERED | Medium grained | Variable - strongly dependent on lithology. | Rounded, reworked rock fragments of cobble- or boulder-grade.  Lithologically variable, but most likely to be of well-indurated sandstone/quartzite or of igneous origin. | Dependent on lithology, but generally robust having survived sedimentary recycling. | Used for walling purposes having received some or, on occasions, no dressing.  Occasionally cut ahead of use. | Recorded only in Brigsley. | 2012-08-27 00:00:00 | SFP/GKL | North East Lincolnshire Council | EastYorkshire and Humber English Heritage Atlas Area | GKL/SFP personal knowledge; fieldwork | 2012-09-25 16:44:36
5319 | Chalk | 1 | Clunch | Fine-grained, white or grey carbonate lithology, which may or may not carry flint nodules. |  | Variable | Colour dulls.  Can take on shades of yellow and grey. | CHALK GROUP | [NAME] | CHALK | Very fine grained | Can be significantly fractured.  See also descriptions of individual Chalk Group formations. | Fine-grained, calcareous nature.  May carry flints. | Liable to fragment. | Used as a walling stone either having been squared or having received little or no dressing. | To a limited degree in areas underlain by Chalk.  The likelihood is that much of the [NAME] seen, especially if it is white/off-white and flint-free, originates from the Flamborough Chalk Formation. | 2012-08-27 00:00:00 | SFP/GKL | North East Lincolnshire Council | EastYorkshire and Humber English Heritage Atlas Area | GKL/SFP personal knowledge; fieldwork | 2012-09-25 16:44:36
5320 | Flamborough Chalk | 1 | Chalk | White, well-bedded, flint-free chalk with common [NAME] (typically about one per metre). |  |  |  | FLAMBOROUGH CHALK FORMATION | [NAME] | CHALK | Very fine grained | Well-bedded; stylolitic seams present. | Flint-free chalk. | Liable to fragment. |  | To a limited extent within or close to its outcrop area.  Much of the Chalk encountered, especially if it is flint-free, likely originates from this unit. | 2012-08-27 00:00:00 | SFP/GKL | North East Lincolnshire Council | EastYorkshire and Humber English Heritage Atlas Area | BGS sources. | 2012-09-25 16:44:36
5321 | [NAME] | 1 | Chalk | White, thinly-bedded chalk with common tabular and discontinuous flint bands; sporadic [NAME]. |  |  |  | BURNHAM CHALK FORMATION | [NAME] | CHALK | Very fine grained | Thinly bedded. | Common flint bands. | Liable to fragment. |  | To an uncertain extent within or close to its outcrop area; not specifically identified during the course of this study. | 2012-08-27 00:00:00 | SFP/GKL | North East Lincolnshire Council | EastYorkshire and Humber English Heritage Atlas Area | BGS sources. | 2012-09-25 16:44:36
5322 | [NAME] | 1 | Chalk | White, massive or thickly bedded chalk with common flint nodules ("burrow-form flints"), but generally lacking tabular flint bands; sporadic [NAME]. |  |  |  | WELTON CHALK FORMATION | [NAME] | CHALK | Very fine grained | Massive or thickly bedded. | Common flint nodules. | Liable to fragment. |  | To an uncertain extent within or close to its outcrop area; not specifically identified during the course of this study. | 2012-08-27 00:00:00 | SFP/GKL | North East Lincolnshire Council | EastYorkshire and Humber English Heritage Atlas Area | BGS sources. | 2012-09-25 16:44:36
5323 | Lincolnshire Limestone | 1 |  | Limestone, typically calcilutites, peloidal wackestones and packstones in the lower part (Lower Lincolnshire Limestone) and high energy ooidal and shell fragmental grainstones in the upper part (Upper Lincolnshire Limestone).  Commonly includes sandy lime | WHITE | Variable | Can take on a variety of pale colours when weathered (yellows, oranges, browns). | LINCOLNSHIRE LIMESTONE FORMATION | JURASSIC | LIMESTONE, OOIDAL, SHELLY OR SPARRY | Medium grained | Bedding can be picked out by weathering. | Variably ooidal and bioclastic.  Weathering characteristics. | Variable.  Blocks in general tend to weather well, but will disaggregate, spall and generally fail with time. | Dressings and repairs to main walling. | Used in a number of ecclesiastical buildings for dressings and repairs. | 2012-08-27 00:00:00 | SFP/GKL | North East Lincolnshire Council | EastYorkshire and Humber English Heritage Atlas Area | GKL/SFP personal knowledge; fieldwork; BGS Lexicon of Named Rock Units | 2012-09-25 16:44:36
5324 | Lincolnshire Limestone | 1 |  | Limestone, typically calcilutites, peloidal wackestones and packstones in the lower part (Lower Lincolnshire Limestone) and high energy ooidal and shell fragmental grainstones in the upper part (Upper Lincolnshire Limestone).  Commonly includes sandy lime | WHITE | Variable | Can take on a variety of pale colours when weathered (yellows, oranges, browns). | LINCOLNSHIRE LIMESTONE FORMATION | JURASSIC | LIMESTONE, OOIDAL, SHELLY OR SPARRY | Medium grained | Bedding can be picked out by weathering. | Variably ooidal and bioclastic.  Weathering characteristics. | Variable.  Blocks in general tend to weather well, but will disaggregate, spall and generally fail with time. | Walling | Within [NAME] upon Hull city centre. | 2012-08-27 00:00:00 | SFP/GKL | Kingston upon Hull City Council | EastYorkshire and Humber English Heritage Atlas Area | GKL/SFP personal knowledge; fieldwork; BGS Lexicon of Named Rock Units; [NAME] (1981) | 2012-09-25 16:44:36
5325 | [NAME] | 5314 | Cave Marble | Limestone, high energy ooidal and bioclastic grainstones, with fine-grained weakly or non-ooidal, shelly and/or silty limestone and calcareous siltstone in lower part. |  | Variable | Orange-brown colour in its most weathered state. | CAVE OOLITE [REDUNDANT NAME AND CODE: SEE ULL] | JURASSIC | LIMESTONE, OOIDAL | Medium grained | Cross-bedding can be picked out by weathering. | Typically [NAME] coloured, ooidal and variably bioclastic limestone found to the north of the Humber. | Variable.  Blocks in general tend to weather well, but will disaggregate, spall and generally fail with time. | Principally as a main walling stone, but has also seen use as dressings and seemingly for repair work. | Newbald-Cave-Brough area. | 2012-08-27 00:00:00 | SFP/GKL | North Lincolnshire Council | EastYorkshire and Humber English Heritage Atlas Area | GKL/SFP personal knowledge; fieldwork; BGS Lexicon of Named Rock Units | 2012-09-25 16:44:36
5326 | [NAME] | 5325 | [NAME] | Limestone, high energy ooidal and bioclastic grainstones, with fine-grained weakly or non-ooidal, shelly and/or silty limestone and calcareous siltstone in lower part. |  | Variable | Orange-brown colour in its most weathered state. | CAVE OOLITE [REDUNDANT NAME AND CODE: SEE ULL] | JURASSIC | LIMESTONE, OOIDAL | Medium grained | Cross-bedding can be picked out by weathering. | Typically [NAME] coloured, ooidal and variably bioclastic limestone found to the north of the Humber. | Variable.  Blocks in general tend to weather well, but will disaggregate, spall and generally fail with time. | Principally as a main walling stone, but has also seen use as dressings and seemingly for repair work. | Newbald-Cave-Brough area. | 2012-08-27 00:00:00 | SFP/GKL | North Lincolnshire Council | EastYorkshire and Humber English Heritage Atlas Area | GKL/SFP personal knowledge; fieldwork; BGS Lexicon of Named Rock Units | 2012-09-25 16:44:36