Spreadsheet: 03d40a81-d620-403d-8512-74550de95fab
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
430 | Shap Granite | 1 |  | Potassium feldspar-megaphyric granite |  |  |  | SHAP PLUTON |  | GRANITE |  |  | Large Potassium feldspar crystals |  |  |  |  | D Cameron | Cumbria County Council | Cumbria English Heritage Atlas Area | Shropshire Buildings | 2012-05-16 10:20:33
1578 | St Bees Sandstone | 1 |  | Red, fine to medium coarse grained sandstone with mudstone clasts locally common, and subordinate thin beds of greenish grey sandstone. | RED |  |  | PARENT DATA NOT YET ENTERED [HIERARCHY CODE] | TRIASSIC to TRIASSIC | SANDSTONE | FINE GRAINED | Cross bedding with some parallel bedding | Red-brown, commonly micaceous sandstones |  | Replacement/Repairs | Bewdley |  | J.Donaldson | Cumbria County Council | Cumbria English Heritage Atlas Area | British Geological Survey lexicon | 2012-05-16 10:20:33
1885 | Tilberthwaite Slate | 1 |  |  |  |  |  | PARENT DATA NOT YET ENTERED [HIERARCHY CODE] |  | NOT ENTERED |  |  |  |  |  | [NAME] |  | D G Cameron | Cumbria County Council | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4201 | Cobbles | 1 | Boulders | Well rounded lithic clasts of cobble- to boulder-grade (typically 10 to 30 cm in diameter, but sometimes more). Although lithologically variable, they are reflective of the local/regional geology. |  | Variable | Variable, dependent on lithological type. | GLACIAL DEPOSITS | [NAME] | NOT ENTERED |  | Variable, dependent on lithological type. | Well-rounded shape. | Not usually susceptible to failure, with the exception of some igneous types. | Walling | Notably along the coastal plain bordering the southern margin of the Solway Firth |  | SFP/GKL | Cumbria County Council | Cumbria English Heritage Atlas Area | GKL/SFP personal knowledge; fieldwork | 2012-05-16 10:20:33
4202 | Boulders | 4201 | Cobbles | Well rounded lithic clasts of cobble- to boulder-grade (typically 10 to 30 cm in diameter, but sometimes more). Although lithologically variable, they are reflective of the local/regional geology. |  | Variable | Variable, dependent on lithological type. | GLACIAL DEPOSITS | [NAME] | NOT ENTERED |  | Variable, dependent on lithological type. | Well-rounded shape. | Not usually susceptible to failure, with the exception of some igneous types. | Walling | Notably along the coastal plain bordering the southern margin of the Solway Firth |  | SFP/GKL | Cumbria County Council | Cumbria English Heritage Atlas Area | GKL/SFP personal knowledge; fieldwork | 2012-05-16 10:20:33
4203 | [NAME] | 1 |  | A highly porous, low density rock type formed as a result of the precipitation of carbonate around and within organic matter (which subsequently decays). |  | Uniform | Off-white/pale grey colour can darken (enhanced by lichen growth). | [NAME] | [NAME] | NOT ENTERED | Very fine grained | Sizeable voids, often linked, are present (reflecting the decay of organic matter). | Off-white/pale grey, highly porous, low density rock with conspicuous cavities/voids. | Generally robust. | Walling | Only identified within the keep of Brough Castle |  | SFP/GKL | Cumbria County Council | Cumbria English Heritage Atlas Area | GKL/SFP personal knowledge; fieldwork | 2012-05-16 10:20:33
4204 | [NAME] | 1 |  | A general term applied to blocks of red-brown, [NAME] and off-white sandstone which, when removed from their source localities, cannot be readily assigned to either the Appleby or Sherwood Sandstone groups. | RED | Variable | Can darken, particularly in areas which have historically suffered from atmospheric pollution . | PERMIAN ROCKS AND TRIASSIC ROCKS (UNDIFFERENTIATED) | PERMIAN to TRIASSIC | NOT ENTERED |  | Can show cross-bedding, parallel-bedding/lamination, and grading. | Red-brown, but sometimes [NAME] and off-white, relatively hard and resistant sandstone. | Fairly robust, but some [NAME] sandstones can weather badly. | Walling and dressings | Used extensively for building purposes in areas on and close to the outcrop of Permian and Triassic sandstones |  | SFP/GKL | Cumbria County Council | Cumbria English Heritage Atlas Area | GKL/SFP personal knowledge; fieldwork | 2012-05-16 10:20:33
4205 | Sherwood Sandstone | 4204 |  | A non-geographic term applied to blocks of red-brown, [NAME] and off-white sandstone which (based on one or more factors) have without doubt originated from quarries located within the outcrop area of the Sherwood Sandstone Group. | RED | Variable | Can darken, particularly in areas which have historically suffered from atmospheric pollution . | SHERWOOD SANDSTONE GROUP | PERMIAN to TRIASSIC | NOT ENTERED |  | Can show cross-bedding, parallel-bedding/lamination, and grading. | Red-brown, but sometimes [NAME] and off-white, relatively hard and resistant sandstone. | Fairly robust, but some Triassic sandstones can weather badly. | Walling and dressings | Used extensively for building purposes in areas on and close to the outcrop of Triassic sandstones |  | SFP/GKL | Cumbria County Council | Cumbria English Heritage Atlas Area | GKL/SFP personal knowledge; fieldwork | 2012-05-16 10:20:33
4206 | St Bees Sandstone | 4205 |  | A non-geographic term applied to blocks of red-brown, [NAME] and off-white sandstone which (based on one or more factors) have without doubt originated from quarries located within the outcrop area of the St Bees Sandstone Formation. | RED | Variable | Can darken, particularly in areas which have historically suffered from atmospheric pollution . | ST BEES SANDSTONE FORMATION | TRIASSIC | NOT ENTERED |  | Can show cross-bedding, horizontal-bedding/lamination, and grading. | Red-brown, but sometimes [NAME] and off-white, commonly micaceous, relatively hard and resistant sandstone. | Fairly robust, but (as is the case with Triassic sandstones generally) can weather badly. | Walling and dressings | Used extensively for building purposes in areas on and close to the outcrop of the St Bees Sandstone |  | SFP/GKL | Cumbria County Council | Cumbria English Heritage Atlas Area | GKL/SFP personal knowledge; fieldwork | 2012-05-16 10:20:33
4207 | [NAME] | 4206 | St Bees Sandstone | ? |  |  |  | ST BEES SANDSTONE FORMATION | TRIASSIC | NOT ENTERED |  |  |  |  |  | Not specifically identified during the course of this study |  | SFP/GKL | Cumbria County Council | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4208 | Birkham's Stone | 4206 | St Bees Sandstone | ? |  |  |  | ST BEES SANDSTONE FORMATION | TRIASSIC | NOT ENTERED |  |  |  |  |  | Not specifically identified during the course of this study |  | SFP/GKL | Cumbria County Council | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4209 | Bank End Stone | 4206 | St Bees Sandstone | ? |  |  |  | ST BEES SANDSTONE FORMATION | TRIASSIC | NOT ENTERED |  |  |  |  |  | Not specifically identified during the course of this study |  | SFP/GKL | Cumbria County Council | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4210 | Croslacon Stone | 4206 | St Bees Sandstone | ? |  |  |  | ST BEES SANDSTONE FORMATION | TRIASSIC | NOT ENTERED |  |  |  |  |  | Not specifically identified during the course of this study |  | SFP/GKL | Cumbria County Council | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4211 | Penrith Sandstone | 4204 |  | A term applied to blocks of red-brown (occasionally [NAME] and off-white) sandstone which (based on one or more factors) have without doubt originated from quarries located within the outcrop area of the Penrith Sandstone Formation. | RED | Variable | Can darken, particularly in areas which have historically suffered from atmospheric pollution . | PENRITH SANDSTONE FORMATION | PERMIAN | NOT ENTERED |  | Can show cross-bedding, parallel-bedding/lamination, and grading. | Red-brown, but sometimes [NAME] and off-white, commonly (though by no means always) coarse-grained, relatively hard and resistant sandstone.  A 'millet-seed' texture is sometimes conspicuous. | Fairly robust, but poorly cemented varieties can weather badly. | Walling and dressings | Used extensively for building purposes in areas on and close to the outcrop of the Penrith Sandstone |  | SFP/GKL | Cumbria County Council | Cumbria English Heritage Atlas Area | GKL/SFP personal knowledge; fieldwork | 2012-05-16 10:20:33
4212 | [NAME] | 4211 | Chalk Stone | ? |  |  |  | PENRITH SANDSTONE FORMATION | PERMIAN | NOT ENTERED |  |  |  |  |  | Not specifically identified during the course of this study |  | SFP/GKL | Cumbria County Council | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4213 | [NAME] | 4211 | Penrith Sandstone | A term applied to blocks of red-brown (occasionally [NAME] and off-white) sandstone which (based on one or more factors) have without doubt originated from quarries located within the [NAME] area (Penrith Sandstone Formation). | RED | Variable | Can darken, particularly in areas which have historically suffered from atmospheric pollution . | PENRITH SANDSTONE FORMATION | PERMIAN | NOT ENTERED |  | Can show cross-bedding, parallel-bedding/lamination, and grading. | Red-brown, but sometimes [NAME] and off-white, commonly (though by no means always) coarse-grained, relatively hard and resistant sandstone.  A 'millet-seed' texture is sometimes conspicuous. | Fairly robust, but poorly cemented varieties can weather badly. | Walling and dressings | Used extensively for building purposes in the Lazonby area and more widely |  | SFP/GKL | Cumbria County Council | Cumbria English Heritage Atlas Area | GKL/SFP personal knowledge; fieldwork | 2012-05-16 10:20:33
4214 | Plumpton Red Lazonby | 4211 | Penrith Sandstone | ? |  |  |  | PENRITH SANDSTONE FORMATION | PERMIAN | NOT ENTERED |  |  |  |  |  | Not specifically identified during the course of this study |  | SFP/GKL | Cumbria County Council | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4215 | [NAME] | 1 | Brockram | Matrix and clast-supported breccias.  The constituent clasts (Carboniferous Limestone) range from small pebble- to cobble-grade, while the matrix is variously clay, silt and/or sand. | PINK | Variable | Limestone clasts and matrix can darken slightly. | BROCKRAM | PERMIAN to TRIASSIC | NOT ENTERED |  | Some blocks can show grading. | Angular clasts, typically of [NAME], set within a pinkish siltstone or sandstone matrix. | Fairly robust. | Walling | Used fairly significantly within areas where these breccias occur e.g. Kirkby Stephen |  | SFP/GKL | Cumbria County Council | Cumbria English Heritage Atlas Area | GKL/SFP personal knowledge; fieldwork | 2012-05-16 10:20:33
4216 | Stenkrith Brockram | 4215 | Brockram | Matrix and clast-supported breccias.  The constituent clasts (Carboniferous Limestone) range from small pebble- to cobble-grade, while the matrix is variously clay, silt and/or sand. | PINK | Variable | Limestone clasts and matrix can darken slightly. | STENKRITH BROCKRAM | PERMIAN | NOT ENTERED |  | Some blocks can show grading. | Angular clasts, typically of [NAME], set within a pinkish siltstone or sandstone matrix. | Fairly robust. | Walling | Used fairly significantly within areas where these breccias occur e.g. Kirkby Stephen |  | SFP/GKL | Cumbria County Council | Cumbria English Heritage Atlas Area | GKL/SFP personal knowledge; fieldwork | 2012-05-16 10:20:33
4217 | Carboniferous Sandstone | 1 |  | General term applied to non-red/brown sandstone blocks evidently not of [NAME] age, but which cannot be assigned to any specific Carboniferous stratigraphic unit. |  | Variable | Liable to darken. | CARBONIFEROUS ROCKS (UNDIFFERENTIATED) | CARBONIFEROUS | NOT ENTERED |  | Cross-bedding sometimes observed. | Mixed sandstones, usually (but not exclusively) [NAME] in colour.  Ferruginous clasts/concretions are often present. | Fairly robust. | Walling and dressings | Used as walling and dressings |  | SFP/GKL | Cumbria County Council | Cumbria English Heritage Atlas Area | GKL/SFP personal knowledge; fieldwork | 2012-05-16 10:20:33
4218 | [NAME] | 4217 |  | ? |  |  |  | WHITEHAVEN SANDSTONE FORMATION | CARBONIFEROUS | NOT ENTERED |  |  |  |  |  | Not specifically identified during the course of this study |  | SFP/GKL | Cumbria County Council | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4219 | Pennine Coal Measures Sandstone | 4217 |  | Impure sandstones, grey or [NAME] in colour which are evidently from the Coal Measures succession, but whose stratigraphic source can be no better pinpointed.  Ferruginous clasts/concretions are often present. |  | Variable | Liable to darken. | PENNINE COAL MEASURES GROUP | CARBONIFEROUS | NOT ENTERED |  | Cross-bedding and de-watering structures sometimes observed. | Impure sandstones, grey or [NAME] in colour.  Ferruginous clasts/concretions are often present. | Variable; relatively poorly cemented blocks or areas within blocks tend to experience accelerated weathering. | Walling and dressings | On outcrop, e.g. in Workington |  | SFP/GKL | Cumbria County Council | Cumbria English Heritage Atlas Area | GKL/SFP personal knowledge; fieldwork | 2012-05-16 10:20:33
4220 | Pennine Middle Coal Measures Formation | 4219 |  | ? |  |  |  | PENNINE MIDDLE COAL MEASURES [NAME] | CARBONIFEROUS | NOT ENTERED |  |  |  |  |  | Not specifically identified during the course of this study |  | SFP/GKL | Cumbria County Council | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4221 | Pennine Lower Coal Measures Formation | 4219 |  | ? |  |  |  | PENNINE LOWER COAL MEASURES [NAME] | CARBONIFEROUS | NOT ENTERED |  |  |  |  |  | Not specifically identified during the course of this study |  | SFP/GKL | Cumbria County Council | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4222 | Millstone Grit Group | 4217 | Millstone Grit | Grey, pale pink or pale purple, coarse-grained (often gritty), well-cemented, impure sandstones. |  | Variable | Pale coloured blocks can darken | MILLSTONE GRIT GROUP [SEE ALSO MIGR] | CARBONIFEROUS | NOT ENTERED |  | Can show cross-bedding. | Impure, (very) coarse-grained, well-cemented sandstones. | Very robust. | Dressings and structural support | Used as dressings and for buttressing |  | SFP/GKL | Cumbria County Council | Cumbria English Heritage Atlas Area | GKL/SFP personal knowledge; fieldwork | 2012-05-16 10:20:33
4223 | Yoredale Group Sandstone | 4217 |  | General term applied to pale grey, pale yellow and pinkish quartzose sandstone blocks yielded by the Yoredale Group, but whose stratigraphic origins cannot be pinpointed more precisely. |  | Variable | Off-white/pale grey coloured blocks can darken. | YOREDALE GROUP | CARBONIFEROUS | NOT ENTERED |  | Cross-bedding and de-watering structures can be observed. | Quartzose sandstones. | Variable, some blocks are robust, while others tend to weather badly. | Walling | Used as walling in areas underlain by or close to the outcrop of Yoredale Group sandstones |  | SFP/GKL | Cumbria County Council | Cumbria English Heritage Atlas Area | GKL/SFP personal knowledge; fieldwork | 2012-05-16 10:20:33
4224 | Stainmore Formation | 4223 |  | ? |  |  |  | STAINMORE FORMATION | CARBONIFEROUS | NOT ENTERED |  |  |  |  |  | Not specifically identified during the course of this study |  | SFP/GKL | Cumbria County Council | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4225 | Hutton [NAME] | 4224 |  | ? | WHITE |  |  | STAINMORE FORMATION | CARBONIFEROUS | NOT ENTERED |  |  |  |  |  | Not specifically identified during the course of this study |  | SFP/GKL | Cumbria County Council | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4226 | [NAME] Grit | 4224 |  | ? |  |  |  | TAN HILL GRIT | CARBONIFEROUS | NOT ENTERED |  |  |  |  |  | Not specifically identified during the course of this study |  | SFP/GKL | Cumbria County Council | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4227 | [NAME] | 4224 |  | ? | WHITE |  |  | HENSINGHAM GRIT | CARBONIFEROUS | NOT ENTERED |  |  |  |  |  | Not specifically identified during the course of this study |  | SFP/GKL | Cumbria County Council | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4228 | Firestone Sill | 4224 | Firestone Sandstone | ? |  |  |  | FIRESTONE SILL | CARBONIFEROUS | NOT ENTERED |  |  |  |  |  | Not specifically identified during the course of this study |  | SFP/GKL | Cumbria County Council | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4229 | [NAME] | 4223 |  | ? |  |  |  | [NAME] | CARBONIFEROUS | NOT ENTERED |  |  |  |  |  | Not specifically identified during the course of this study |  | SFP/GKL | Cumbria County Council | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4230 | [NAME] | 4223 |  | Pale pink, quartzose sandstone carrying ferruginous 'clots'.  The source of this stone is mentioned in the literature, allowing its stratigraphic origins to be stated precisely. | PINK | Uniform | Little change is evident. | [NAME] | CARBONIFEROUS | NOT ENTERED |  | Can show traces of cross-bedding. | Pale pink, quartzose sandstone carrying ferruginous 'clots'. | Apparently robust. | Walling | Not specifically identified during the course of this study |  | SFP/GKL | Cumbria County Council | Cumbria English Heritage Atlas Area | GKL/SFP personal knowledge; fieldwork; Hyde & Pevsner, 2010.  The Buildings of England: Cumbria (Cumberland, [NAME] and [NAME]).  Yale University Press. | 2012-05-16 10:20:33
4231 | [NAME] | 4230 |  | ? |  |  |  | [NAME] | CARBONIFEROUS | NOT ENTERED |  |  |  |  |  | Not specifically identified during the course of this study |  | SFP/GKL | Cumbria County Council | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4232 | Tyne Limestone Formation Sandstone | 4223 |  | ? |  |  |  | [NAME] | CARBONIFEROUS | NOT ENTERED |  |  |  |  |  | Not specifically identified during the course of this study |  | SFP/GKL | Cumbria County Council | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4233 | [NAME] | 1 |  | Variably fossilferous limestone evidently yielded by the Carboniferous Limestone succession, but whose stratigraphic origins cannot be pinpointed more precisely. | WHITE | Uniform | Can take on a grey colour. | CARBONIFEROUS LIMESTONE SUPERGROUP | CARBONIFEROUS | NOT ENTERED |  | Can show evidence of bioturbation. | Variably fossiliferous, hard limestones. | Generally robust. | Walling and dressings | Not specifically identified during the course of this study |  | SFP/GKL | Cumbria County Council | Cumbria English Heritage Atlas Area | GKL/SFP personal knowledge; fieldwork | 2012-05-16 10:20:33
4234 | Great Scar Limestone | 4233 |  | Various limestones yielded by the Great Scar Limestone Group succession, but whose stratigraphic origins cannot be pinpointed more precisely. |  | Variable | Can darken. | GREAT SCAR LIMESTONE GROUP | CARBONIFEROUS | NOT ENTERED |  | Sometimes shows evidence of bioturbation and can be strongly brecciated. | Variably fossiliferous, hard limestones. | Generally robust, although blocks/slabs of brecciated limestone (e.g. lintels) are seemingly prone to disaggregation over time. | Walling and dressings | Uused extensively for building purposes in areas underlain by and close to outcrops of the Great Scar Limestone |  | SFP/GKL | Cumbria County Council | Cumbria English Heritage Atlas Area | GKL/SFP personal knowledge; fieldwork | 2012-05-16 10:20:33
4235 | Orebank Sandstone | 4234 |  | ? |  |  |  | OREBANK SANDSTONE | CARBONIFEROUS | NOT ENTERED |  |  |  |  |  | Not specifically identified during the course of this study |  | SFP/GKL | Cumbria County Council | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4236 | Fifth Limestone (Cumbria) | 4234 |  | ? |  |  |  | FIFTH LIMESTONE (CUMBRIA) | CARBONIFEROUS | NOT ENTERED |  |  |  |  |  | Not specifically identified during the course of this study |  | SFP/GKL | Cumbria County Council | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4237 | Knipe Scar Limestone Formation | 4234 |  | ? |  |  |  | KNIPE SCAR [NAME] | CARBONIFEROUS | NOT ENTERED |  |  |  |  |  | Not specifically identified during the course of this study |  | SFP/GKL | Cumbria County Council | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4238 | Fourth Shale Member (Fifth Limestone) | 4234 |  | ? |  |  |  | FOURTH SHALE MEMBER | CARBONIFEROUS | NOT ENTERED |  |  |  |  |  | Not specifically identified during the course of this study |  | SFP/GKL | Cumbria County Council | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4239 | [NAME] | 4234 |  | ? |  |  |  | URSWICK LIMESTONE FORMATION | CARBONIFEROUS | NOT ENTERED |  |  |  |  |  | Not specifically identified during the course of this study |  | SFP/GKL | Cumbria County Council | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4240 | Scandal Beck Limestone Formation | 4234 |  | ? |  |  |  | SCANDAL BECK LIMESTONE FORMATION | CARBONIFEROUS | NOT ENTERED |  |  |  |  |  | Not specifically identified during the course of this study |  | SFP/GKL | Cumbria County Council | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4241 | [NAME] | 4234 |  | ? |  |  |  | [NAME] | CARBONIFEROUS | NOT ENTERED |  |  |  |  |  | Not specifically identified during the course of this study |  | SFP/GKL | Cumbria County Council | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4242 | Shap Village Limestone | 4233 |  | Pale grey, hard, texturally and compositionally variable limestones cropping out in the Shap area. |  | Uniform | Can darken. | SHAP VILLAGE LIMESTONE FORMATION | CARBONIFEROUS | NOT ENTERED |  | None specifcally noted in walling blocks. | Pale grey, hard, variably bioclastic limestones. | Apparently robust 9but this may be a consequence of historical render-shielding). | Walling | Only identified within the village of Shap itself |  | SFP/GKL | Cumbria County Council | Cumbria English Heritage Atlas Area | GKL/SFP personal knowledge; fieldwork | 2012-05-16 10:20:33
4243 | Parkhead Sandstone | 4217 |  | ? |  |  |  | PARKHEAD SANDSTONE | CARBONIFEROUS | NOT ENTERED |  |  |  |  |  | Not specifically identified during the course of this study |  | SFP/GKL | Cumbria County Council | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4244 | Windermere Supergroup | 1 |  | Variably cleaved, generally fine-grained metasediments in various shades of grey and green-grey.  This is a general term applied to metasediments originating from Windermere Supergroup units, but whose stratigraphic origins cannot be pinpointed more precisely. | GREY | Variable | Weathering crusts of various colours can develop. | WINDERMERE SUPERGROUP | SILURIAN | NOT ENTERED |  | A slaty cleavage is variably developed (this is lithologically controlled).  Sedimentary bedding is sometimes discernible. | Variably cleaved, generally fine-grained metasediments in various shades of grey and green-grey. | Generally robust | Walling and roofing | Not specifically identified during the course of this study |  | SFP/GKL | Cumbria County Council | Cumbria English Heritage Atlas Area | GKL/SFP personal knowledge; fieldwork | 2012-05-16 10:20:33
4245 | Bannisdale Formation | 4244 |  | ? |  |  |  | [NAME] | SILURIAN | SILTSTONE AND MUDSTONE |  |  |  |  |  | Not specifically identified during the course of this study |  | SFP/GKL | Cumbria County Council | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4246 | Bannisdale Slate | 4245 | Bannisdale Formation | Grey silty mudstones with a moderately well developed cleavage. | GREY | Variable | Weathering crusts of various colours can develop. | [NAME] | SILURIAN | NOT ENTERED |  | Slaty cleavage.  Sedimentary bedding is sometimes discernible. | Grey silty mudstones with a moderately well developed cleavage. | Generally robust | Walling and roofing | Not specifically identified during the course of this study |  | SFP/GKL | Cumbria County Council | Cumbria English Heritage Atlas Area | GKL/SFP personal knowledge; fieldwork | 2012-05-16 10:20:33
4247 | Bannisdale Formation Limestone | 4245 |  | ? |  |  |  | [NAME] | SILURIAN | NOT ENTERED |  |  |  |  |  | Not specifically identified during the course of this study |  | SFP/GKL | Cumbria County Council | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4248 | Newton Toms | 4245 | Bannisdale Formation | ? |  |  |  | [NAME] | SILURIAN | NOT ENTERED |  |  |  |  |  | Not specifically identified during the course of this study |  | SFP/GKL | Cumbria County Council | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4249 | Coniston Group | 4244 |  | ? |  |  |  | CONISTON GROUP | SILURIAN | NOT ENTERED |  |  |  |  |  | Used in areas underlain by Coniston Group lithologies |  | SFP/GKL | Cumbria County Council | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4250 | Coniston Group Sandstone | 4249 |  | Pale grey-green, sandy and silty metasediments.  Cleavage development is litholgically controlled, and blocks may show no obvious cleavage. | GREY | Variable | [NAME] coloured weathering crusts appear to be the norm. | CONISTON GROUP | SILURIAN | NOT ENTERED |  | Cleavage variably developed (lithologically controlled).  Blocks tend to possess a conchoidal fracture. | Pale grey-green, variably cleaved, sandy and silty metasediments. | Robust | Walling | Used in areas underlain by Coniston Group lithologies |  | SFP/GKL | Cumbria County Council | Cumbria English Heritage Atlas Area | GKL/SFP personal knowledge; fieldwork | 2012-05-16 10:20:33
4251 | Moorhowe Formation | 4249 |  | ? |  |  |  | MOORHOWE [NAME] | SILURIAN | NOT ENTERED |  |  |  |  |  | Not specifically identified during the course of this study |  | SFP/GKL | Cumbria County Council | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4252 | Latrigg Formation Slate | 4249 |  | ? |  |  |  | LATRIGG FORMATION | SILURIAN | NOT ENTERED |  |  |  |  |  | Not specifically identified during the course of this study |  | SFP/GKL | Cumbria County Council | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4253 | Latrigg Formation Mudstone | 4249 |  | ? |  |  |  | LATRIGG FORMATION | SILURIAN | NOT ENTERED |  |  |  |  |  | Not specifically identified during the course of this study |  | SFP/GKL | Cumbria County Council | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4254 | Latrigg Formation Green Slate | 4249 |  | ? |  |  |  | LATRIGG FORMATION | SILURIAN | NOT ENTERED |  |  |  |  |  | Not specifically identified during the course of this study |  | SFP/GKL | Cumbria County Council | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4255 | [NAME] | 4249 |  | ? |  |  |  | GAWTHWAITE FORMATION | SILURIAN | NOT ENTERED |  |  |  |  |  | Not specifically identified during the course of this study |  | SFP/GKL | Cumbria County Council | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4256 | Tranearth Group Slate | 4244 |  | Pale grey, fine-grained metasediments (mudstones and silty mudstones) with a moderately developed slaty cleavage. | GREY | Uniform | [NAME] weathering crusts can develop. | TRANEARTH GROUP | SILURIAN | NOT ENTERED |  | Cleavage moderately well developed. | Pale grey, fine-grained metasediments with a moderately developed slaty cleavage. | Robust | Walling | Not specifically identified during the course of this study |  | SFP/GKL | Cumbria County Council | Cumbria English Heritage Atlas Area | GKL/SFP personal knowledge; fieldwork | 2012-05-16 10:20:33
4257 | Wray [NAME] | 4256 |  | ? |  |  |  | WRAY CASTLE FORMATION | SILURIAN | NOT ENTERED |  |  |  |  |  | Not specifically identified during the course of this study |  | SFP/GKL | Cumbria County Council | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4258 | [NAME] | 4256 | Coldwell Formation Slate | ? |  |  |  | [NAME] | SILURIAN | NOT ENTERED |  |  |  |  |  | Not specifically identified during the course of this study |  | SFP/GKL | Cumbria County Council | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4259 | [NAME] | 4256 |  | ? |  |  |  | BIRK RIGGS FORMATION | SILURIAN | SILTSTONE, MUDSTONE AND SANDSTONE |  |  |  |  |  | Not specifically identified during the course of this study |  | SFP/GKL | Cumbria County Council | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4260 | [NAME] | 4256 | Brathay Formation Slate | Pale grey, fine-grained metasediments (mixed mudstones and siltstones) with a moderately developed slaty cleavage. | GREY | Uniform | Paler grey and pale brown weathering crusts can develop | BRATHAY FORMATION | SILURIAN | SILTSTONE AND MUDSTONE |  | Cleavage moderately well developed. | Pale grey, fine-grained metasediments which are cleaved to the extent that they fragment in a blocky and slabby manner. | Robust | Walling | Not specifically identified during the course of this study |  | SFP/GKL | Cumbria County Council | Cumbria English Heritage Atlas Area | GKL/SFP personal knowledge; fieldwork | 2012-05-16 10:20:33
4261 | Brathay Formation Slate | 4260 | [NAME] | ? |  |  |  | BRATHAY FORMATION | SILURIAN | NOT ENTERED |  |  |  |  |  | Not specifically identified during the course of this study |  | SFP/GKL | Cumbria County Council | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4262 | Westmorland Slate | 4260 | Brathay Formation Slate | ? |  |  |  | BRATHAY FORMATION | SILURIAN | NOT ENTERED |  |  |  |  |  | Not specifically identified during the course of this study |  | SFP/GKL | Cumbria County Council | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4263 | Stockdale Group | 4244 |  | ? |  |  |  | STOCKDALE GROUP | SILURIAN | SILTSTONE AND MUDSTONE |  |  |  |  |  | Not specifically identified during the course of this study |  | SFP/GKL | Cumbria County Council | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4264 | Dent Group | 4244 |  | ? |  |  |  | DENT GROUP | ORDOVICIAN | NOT ENTERED |  |  |  |  |  | Not specifically identified during the course of this study |  | SFP/GKL | Cumbria County Council | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4265 | Ashgill Formation | 4264 |  | ? |  |  |  | [NAME] | ORDOVICIAN | NOT ENTERED |  |  |  |  |  | Not specifically identified during the course of this study |  | SFP/GKL | Cumbria County Council | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4266 | Yarlside Volcanic Formation | 4264 |  | ? |  |  |  | YARLSIDE VOLCANIC FORMATION | ORDOVICIAN | NOT ENTERED |  |  |  |  |  | Not specifically identified during the course of this study |  | SFP/GKL | Cumbria County Council | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4267 | Borrowdale Volcanic Group | 1 |  | A lithologically mixed grouping of rocks which includes pale green volcaniclastic metasediments and dark greenish-grey vesicular and non-vesicular volcanic rocks. |  | Variable | Variable, dependent on the nature of an individual block; some blocks can develop substantial pale coloured weathering crusts. | BORROWDALE VOLCANIC GROUP | ORDOVICIAN | NOT ENTERED |  | Meta-volcaniclastic rocks can show slumping-related features, while the volcanic rocks can be vesicular. | Metamorphosed volcaniclastic sediments and volcanic rocks (including vesicular varieties). | Robust | Walling | Not specifically identified during the course of this study |  | SFP/GKL | Cumbria County Council | Cumbria English Heritage Atlas Area | GKL/SFP personal knowledge; fieldwork | 2012-05-16 10:20:33
4268 | Waberthwaite [NAME] | 4267 |  | ? |  |  |  | WABERTHWAITE TUFF FORMATION | ORDOVICIAN | NOT ENTERED |  |  |  |  |  | Not specifically identified during the course of this study |  | SFP/GKL | Cumbria County Council | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4269 | Birker Fell Andesite Formation | 4267 |  | ? |  |  |  | BIRKER FELL ANDESITE FORMATION | ORDOVICIAN | NOT ENTERED |  |  |  |  |  | Not specifically identified during the course of this study |  | SFP/GKL | Cumbria County Council | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4270 | Lincomb Tarns [NAME] | 4267 |  | ? |  |  |  | LINCOMB TARNS TUFF FORMATION | ORDOVICIAN | VOLCANICLASTIC SANDSTONE |  |  |  |  |  | Not specifically identified during the course of this study |  | SFP/GKL | Cumbria County Council | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4271 | [NAME] Intrusives | 1 |  | ? |  |  |  | BORROWDALE SILL SUITE | ORDOVICIAN | NOT ENTERED |  |  |  |  |  | Not specifically identified during the course of this study |  | SFP/GKL | Cumbria County Council | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4272 | Lake District Ordovician Minor Intrusion Suite | 1 |  | ? |  |  |  | LAKE DISTRICT ORDOVICIAN MINOR INTRUSION SUITE | ORDOVICIAN | NOT ENTERED |  |  |  |  |  | Not specifically identified during the course of this study |  | SFP/GKL | Cumbria County Council | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4273 | Skiddaw Group | 1 |  | The Skiddaw Group as a whole is lithologically mixed, but the building stones of Skiddaw Group derivation encountered during this study tended to be dark grey, slabby, imperfectly cleaved meta-siltstones and mudstones. | GREY | Variable | Some blocks weather a rusty brown colour. | SKIDDAW GROUP | ORDOVICIAN | MUDSTONES AND SILTSTONES |  | Imperfect slaty cleavage. | Commonly dark grey, imperfectly cleaved, fine-grained metasediments. | Seemingly robust | Walling | Not specifically identified during the course of this study |  | SFP/GKL | Cumbria County Council | Cumbria English Heritage Atlas Area | GKL/SFP personal knowledge; fieldwork | 2012-05-16 10:20:33
4274 | [NAME] | 4273 |  | ? |  |  |  | KIRK STILE FORMATION | ORDOVICIAN | MUDSTONES AND SILTSTONES |  |  |  |  |  | Not specifically identified during the course of this study |  | SFP/GKL | Cumbria County Council | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4275 | Watch Hill Formation | 4273 |  | ? |  |  |  | WATCH HILL FORMATION | ORDOVICIAN | SANDSTONE, SILTSTONE AND MUDSTONE |  |  |  |  |  | Not specifically identified during the course of this study |  | SFP/GKL | Cumbria County Council | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4276 | Buttermere Formation | 4273 |  | ? |  |  |  | BUTTERMERE FORMATION | ORDOVICIAN | NOT ENTERED |  |  |  |  |  | Not specifically identified during the course of this study |  | SFP/GKL | Cumbria County Council | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4277 | Sandstone, Carboniferous | 4217 |  | Term applied to [NAME] coloured sandstones utilised for dressings in buildings not visited during the course of this study.  These sandstones are believed to derive from the Carboniferous successions of Cumbria or Northern England generally, but physical examination would be necessary to confirm this and better constrain their stratigraphical origins. | BUFF |  |  | CARBONIFEROUS ROCKS (UNDIFFERENTIATED) | CARBONIFEROUS | NOT ENTERED |  |  |  |  | Dressings | Used as dressings |  | SFP/GKL | Cumbria County Council | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4278 | Stone flags (Unknown) | 1 |  | Fissile sedimentary rock. |  |  |  | PARENT DATA NOT YET ENTERED [HIERARCHY CODE] |  | NOT ENTERED |  |  |  |  | Roofing | Cumbria usage |  | SFP/GKL | Cumbria County Council | Cumbria English Heritage Atlas Area | Cumbria Buildings Spreadsheet | 2012-05-16 10:20:33
4401 | Cobbles | 1 | Boulders | Well rounded lithic clasts of cobble- to boulder-grade (typically 10 to 30 cm in diameter, but sometimes more). Although lithologically variable, they are reflective of the local/regional geology. |  | Variable | Variable, dependent on lithological type. | GLACIAL DEPOSITS | [NAME] | NOT ENTERED |  | Variable, dependent on lithological type. | Well-rounded shape. | Not usually susceptible to failure, with the exception of some igneous types. | Walling | Usually in pre-Victorian buildings in areas where the local stone types could not be easily fashioned. |  | SFP/GKL | Lake District National Park Authority | Cumbria English Heritage Atlas Area | GKL/SFP personal knowledge; fieldwork | 2012-05-16 10:20:33
4402 | Boulders | 4401 | Cobbles | Well rounded lithic clasts of cobble- to boulder-grade (typically 10 to 30 cm in diameter, but sometimes more). Although lithologically variable, they are reflective of the local/regional geology. |  | Variable | Variable, dependent on lithological type. | GLACIAL DEPOSITS | [NAME] | NOT ENTERED |  | Variable, dependent on lithological type. | Well-rounded shape. | Not usually susceptible to failure, with the exception of some igneous types. | Walling | Usually in pre-Victorian buildings in areas where the local stone types could not be easily fashioned. |  | SFP/GKL | Lake District National Park Authority | Cumbria English Heritage Atlas Area | GKL/SFP personal knowledge; fieldwork | 2012-05-16 10:20:33
4403 | [NAME] | 1 |  | A general term applied to blocks of red-brown, [NAME] and off-white sandstone which, when removed from their source localities, cannot be readily assigned to either the Appleby or Sherwood Sandstone groups. | RED | Variable | Can darken, particularly in areas which have historically suffered from atmospheric pollution . | PERMIAN ROCKS AND TRIASSIC ROCKS (UNDIFFERENTIATED) | PERMIAN to TRIASSIC | NOT ENTERED |  | Can show cross-bedding, parallel-bedding/lamination, and grading. | Red-brown, but sometimes [NAME] and off-white, relatively hard and resistant sandstone. | Fairly robust, but some [NAME] sandstones can weather badly. | Walling and dressings | Used primarily for dressings as opposed to walling. |  | SFP/GKL | Lake District National Park Authority | Cumbria English Heritage Atlas Area | GKL/SFP personal knowledge; fieldwork | 2012-05-16 10:20:33
4404 | Sherwood Sandstone | 4403 |  | A non-geographic term applied to blocks of red-brown, [NAME] and off-white sandstone which (based on one or more factors) have without doubt originated from quarries located within the outcrop area of the Sherwood Sandstone Group. | RED | Variable | Can darken, particularly in areas which have historically suffered from atmospheric pollution . | SHERWOOD SANDSTONE GROUP | PERMIAN to TRIASSIC | NOT ENTERED |  | Can show cross-bedding, parallel-bedding/lamination, and grading. | Red-brown, but sometimes [NAME] and off-white, relatively hard and resistant sandstone. | Fairly robust, but some Triassic sandstones can weather badly. | Walling and dressings | Used primarily for dressings as opposed to walling. |  | SFP/GKL | Lake District National Park Authority | Cumbria English Heritage Atlas Area | GKL/SFP personal knowledge; fieldwork | 2012-05-16 10:20:33
4405 | St Bees Sandstone | 4404 |  | A non-geographic term applied to blocks of red-brown, [NAME] and off-white sandstone which (based on one or more factors) have without doubt originated from quarries located within the outcrop area of the St Bees Sandstone Formation. | RED | Variable | Can darken, particularly in areas which have historically suffered from atmospheric pollution . | ST BEES SANDSTONE FORMATION | TRIASSIC | NOT ENTERED |  | Can show cross-bedding, horizontal-bedding/lamination, and grading. | Red-brown, but sometimes [NAME] and off-white, commonly micaceous, relatively hard and resistant sandstone. | Fairly robust, but (as is the case with Triassic sandstones generally) can weather badly. | Walling and dressings | Not specifically identified within the LDP. |  | SFP/GKL | Lake District National Park Authority | Cumbria English Heritage Atlas Area | GKL/SFP personal knowledge; fieldwork | 2012-05-16 10:20:33
4406 | [NAME] | 1 | Brockram | Matrix and clast-supported breccias.  The constituent clasts (Carboniferous Limestone) range from small pebble- to cobble-grade, while the matrix is variously clay, silt and/or sand. | PINK | Variable | Limestone clasts and matrix can darken slightly. | BROCKRAM | PERMIAN to TRIASSIC | NOT ENTERED |  | Some blocks can show grading. | Angular clasts, typically of [NAME], set within a pinkish siltstone or sandstone matrix. | Fairly robust. | Walling | Not specifically identified within the LDP. |  | SFP/GKL | Lake District National Park Authority | Cumbria English Heritage Atlas Area | GKL/SFP personal knowledge; fieldwork | 2012-05-16 10:20:33
4407 | Carboniferous Sandstone | 1 |  | General term applied to non-red/brown sandstone blocks evidently not of [NAME] age, but which cannot be assigned to any specific Carboniferous stratigraphic unit. |  | Variable | Liable to darken. | CARBONIFEROUS ROCKS (UNDIFFERENTIATED) | CARBONIFEROUS | NOT ENTERED |  | Cross-bedding sometimes observed. | Mixed sandstones, usually (but not exclusively) [NAME] in colour.  Ferruginous clasts/concretions are often present. | Fairly robust. | Walling and dressings | Used as dressings e.g. in Coniston. |  | SFP/GKL | Lake District National Park Authority | Cumbria English Heritage Atlas Area | GKL/SFP personal knowledge; fieldwork | 2012-05-16 10:20:33
4408 | Yoredale Group Sandstone | 4407 |  | General term applied to pale grey, pale yellow and pinkish quartzose sandstone blocks yielded by the Yoredale Group, but whose stratigraphic origins cannot be pinpointed more precisely. |  | Variable | Off-white/pale grey coloured blocks can darken. | YOREDALE GROUP | CARBONIFEROUS | NOT ENTERED |  | Cross-bedding and de-watering structures can be observed. | Quartzose sandstones. | Variable, some blocks are robust, while others tend to weather badly. | Walling | Not specifically identified during the course of this study. |  | SFP/GKL | Lake District National Park Authority | Cumbria English Heritage Atlas Area | GKL/SFP personal knowledge; fieldwork | 2012-05-16 10:20:33
4409 | Stainmore Formation | 4408 |  | ? |  |  |  | STAINMORE FORMATION | CARBONIFEROUS | NOT ENTERED |  |  |  |  |  | Not specifically identified during the course of this study. |  | SFP/GKL | Lake District National Park Authority | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4410 | [NAME] | 1 |  | ? |  |  |  | [NAME] | CARBONIFEROUS | NOT ENTERED |  |  |  |  |  | Not specifically identified during the course of this study. |  | SFP/GKL | Lake District National Park Authority | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4411 | [NAME] | 4408 |  | Pale pink, quartzose sandstone carrying ferruginous 'clots'.  The source of this stone is mentioned in the literature, allowing its stratigraphic origins to be stated precisely. | PINK | Uniform | Little change is evident. | [NAME] | CARBONIFEROUS | NOT ENTERED |  | Can show traces of cross-bedding. | Pale pink, quartzose sandstone carrying ferruginous 'clots'. | Apparently robust. | Walling | Used to face the Church of St John in Keswick. |  | SFP/GKL | Lake District National Park Authority | Cumbria English Heritage Atlas Area | GKL/SFP personal knowledge; fieldwork; Hyde & Pevsner, 2010.  The Buildings of England: Cumbria (Cumberland, [NAME] and [NAME]).  Yale University Press. | 2012-05-16 10:20:33
4412 | [NAME] | 1 |  | Variably fossilferous limestone evidently yielded by the Carboniferous Limestone succession, but whose stratigraphic origins cannot be pinpointed more precisely. | WHITE | Uniform | Can take on a grey colour. | CARBONIFEROUS LIMESTONE SUPERGROUP | CARBONIFEROUS | NOT ENTERED |  | Can show evidence of bioturbation. | Variably fossiliferous, hard limestones. | Generally robust. | Walling and dressings | Used in connection with limestones observed in Windermere. |  | SFP/GKL | Lake District National Park Authority | Cumbria English Heritage Atlas Area | GKL/SFP personal knowledge; fieldwork | 2012-05-16 10:20:33
4413 | Great Scar Limestone | 4412 |  | Various limestones yielded by the Great Scar Limestone Group succession, but whose stratigraphic origins cannot be pinpointed more precisely. |  | Variable | Can darken. | GREAT SCAR LIMESTONE GROUP | CARBONIFEROUS | NOT ENTERED |  | Sometimes shows evidence of bioturbation and can be strongly brecciated. | Variably fossiliferous, hard limestones. | Generally robust, although blocks/slabs of brecciated limestone (e.g. lintels) are seemingly prone to disaggregation over time. | Walling and dressings | Can be used extensively for building purposes in areas underlain by and close to outcrops of the Great Scar Limestone. |  | SFP/GKL | Lake District National Park Authority | Cumbria English Heritage Atlas Area | GKL/SFP personal knowledge; fieldwork | 2012-05-16 10:20:33
4414 | Fifth Limestone (Cumbria) | 4413 |  | ? |  |  |  | FIFTH LIMESTONE (CUMBRIA) | CARBONIFEROUS | NOT ENTERED |  |  |  |  |  | Not specifically identified during the course of this study. |  | SFP/GKL | Lake District National Park Authority | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4415 | Knipe Scar Limestone Formation | 4413 |  | ? |  |  |  | KNIPE SCAR [NAME] | CARBONIFEROUS | NOT ENTERED |  |  |  |  |  | Not specifically identified during the course of this study. |  | SFP/GKL | Lake District National Park Authority | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4416 | Fourth Shale Member (Fifth Limestone) | 4413 |  | ? |  |  |  | FOURTH SHALE MEMBER | CARBONIFEROUS | NOT ENTERED |  |  |  |  |  | Not specifically identified during the course of this study. |  | SFP/GKL | Lake District National Park Authority | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4417 | [NAME] | 4413 |  | ? |  |  |  | URSWICK LIMESTONE FORMATION | CARBONIFEROUS | NOT ENTERED |  |  |  |  |  | Not specifically identified during the course of this study. |  | SFP/GKL | Lake District National Park Authority | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4418 | [NAME] | 4413 |  | ? |  |  |  | [NAME] | CARBONIFEROUS | NOT ENTERED |  |  |  |  |  | Not specifically identified during the course of this study. |  | SFP/GKL | Lake District National Park Authority | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4419 | Shap Village Limestone | 4412 |  | Pale grey, hard, texturally and compositionally variable limestones cropping out in the Shap area. |  | Uniform | Can darken. | SHAP VILLAGE LIMESTONE FORMATION | CARBONIFEROUS | NOT ENTERED |  | None specifcally noted in walling blocks. | Pale grey, hard, variably bioclastic limestones. | Apparently robust 9but this may be a consequence of historical render-shielding). | Walling | Not identified during the course of this study. |  | SFP/GKL | Lake District National Park Authority | Cumbria English Heritage Atlas Area | GKL/SFP personal knowledge; fieldwork | 2012-05-16 10:20:33
4420 | Shap Granite | 1 |  | Strongly porphyritic pale pink granite.  The groundmass may show subtle colour variation. | PINK | Variable | Little change is evident. | SHAP PLUTON | DEVONIAN | NOT ENTERED |  | Strongly porphyritic. | Strongly porphyritic with prominent pink K-feldspar phenocrysts. | Robust | Walling | Used for internal decoration. Only outside use, Church of St James, Tebay (CMA) |  | SFP/GKL | Lake District National Park Authority | Cumbria English Heritage Atlas Area | GKL/SFP personal knowledge; fieldwork | 2012-05-16 10:20:33
4421 | Windermere Supergroup | 1 |  | Variably cleaved, generally fine-grained metasediments in various shades of grey and green-grey.  This is a general term applied to metasediments originating from Windermere Supergroup units, but whose stratigraphic origins cannot be pinpointed more precisely. | GREY | Variable | Weathering crusts of various colours can develop. | WINDERMERE SUPERGROUP | SILURIAN | NOT ENTERED |  | A slaty cleavage is variably developed (this is lithologically controlled).  Sedimentary bedding is sometimes discernible. | Variably cleaved, generally fine-grained metasediments in various shades of grey and green-grey. | Generally robust | Walling and roofing | Used extensively in areas underlain by Windermere Supergroup lithologies. |  | SFP/GKL | Lake District National Park Authority | Cumbria English Heritage Atlas Area | GKL/SFP personal knowledge; fieldwork | 2012-05-16 10:20:33
4422 | Bannisdale Formation | 4421 |  | ? |  |  |  | [NAME] | SILURIAN | SILTSTONE AND MUDSTONE |  |  |  |  |  | Yes, see 'Bannisdale Slate'. |  | SFP/GKL | Lake District National Park Authority | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4423 | Bannisdale Slate | 4422 | Bannisdale Formation | Grey silty mudstones with a moderately well developed cleavage. | GREY | Variable | Weathering crusts of various colours can develop. | [NAME] | SILURIAN | NOT ENTERED |  | Slaty cleavage.  Sedimentary bedding is sometimes discernible. | Grey silty mudstones with a moderately well developed cleavage. | Generally robust | Walling and roofing | Used extensively in areas underlain by the Bannisdale Formation. |  | SFP/GKL | Lake District National Park Authority | Cumbria English Heritage Atlas Area | GKL/SFP personal knowledge; fieldwork | 2012-05-16 10:20:33
4424 | Bannisdale Formation Limestone | 4422 |  | ? |  |  |  | [NAME] | SILURIAN | NOT ENTERED |  |  |  |  |  | Not specifically identified during the course of this study. |  | SFP/GKL | Lake District National Park Authority | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4425 | Newton Toms | 4422 | Bannisdale Formation | ? |  |  |  | [NAME] | SILURIAN | NOT ENTERED |  |  |  |  |  | Not specifically identified during the course of this study. |  | SFP/GKL | Lake District National Park Authority | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4426 | Coniston Group | 4421 |  | ? |  |  |  | CONISTON GROUP | SILURIAN | NOT ENTERED |  |  |  |  |  | Yes, see 'Coniston Group Sandstone'. |  | SFP/GKL | Lake District National Park Authority | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4427 | Coniston Group Sandstone | 4426 |  | Pale grey-green, sandy and silty metasediments.  Cleavage development is litholgically controlled, and blocks may show no obvious cleavage. | GREY | Variable | [NAME] coloured weathering crusts appear to be the norm. | CONISTON GROUP | SILURIAN | NOT ENTERED |  | Cleavage variably developed (lithologically controlled).  Blocks tend to possess a conchoidal fracture. | Pale grey-green, variably cleaved, sandy and silty metasediments. | Robust | Walling | Used in areas underlain by Coniston Group lithologies. |  | SFP/GKL | Lake District National Park Authority | Cumbria English Heritage Atlas Area | GKL/SFP personal knowledge; fieldwork | 2012-05-16 10:20:33
4428 | Moorhowe Formation | 4426 |  | ? |  |  |  | MOORHOWE [NAME] | SILURIAN | NOT ENTERED |  |  |  |  |  | Not specifically identified during the course of this study. |  | SFP/GKL | Lake District National Park Authority | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4429 | Latrigg Formation Slate | 4426 |  | ? |  |  |  | LATRIGG FORMATION | SILURIAN | NOT ENTERED |  |  |  |  |  | Not specifically identified during the course of this study. |  | SFP/GKL | Lake District National Park Authority | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4430 | Latrigg Formation Mudstone | 4426 |  | ? |  |  |  | LATRIGG FORMATION | SILURIAN | NOT ENTERED |  |  |  |  |  | Not specifically identified during the course of this study. |  | SFP/GKL | Lake District National Park Authority | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4431 | Latrigg Formation Green Slate | 4426 |  | ? |  |  |  | LATRIGG FORMATION | SILURIAN | NOT ENTERED |  |  |  |  |  | Not specifically identified during the course of this study. |  | SFP/GKL | Lake District National Park Authority | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4432 | [NAME] | 4426 |  | ? |  |  |  | GAWTHWAITE FORMATION | SILURIAN | NOT ENTERED |  |  |  |  |  | Not specifically identified during the course of this study. |  | SFP/GKL | Lake District National Park Authority | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4433 | Tranearth Group Slate | 4421 |  | Pale grey, fine-grained metasediments (mudstones and silty mudstones) with a moderately developed slaty cleavage. | GREY | Uniform | [NAME] weathering crusts can develop. | TRANEARTH GROUP | SILURIAN | NOT ENTERED |  | Cleavage moderately well developed. | Pale grey, fine-grained metasediments with a moderately developed slaty cleavage. | Robust | Walling | Yes, but only identified in three buildings. |  | SFP/GKL | Lake District National Park Authority | Cumbria English Heritage Atlas Area | GKL/SFP personal knowledge; fieldwork | 2012-05-16 10:20:33
4434 | Wray [NAME] | 4433 |  | ? |  |  |  | WRAY CASTLE FORMATION | SILURIAN | NOT ENTERED |  |  |  |  |  | Not specifically identified during the course of this study. |  | SFP/GKL | Lake District National Park Authority | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4435 | [NAME] | 4433 | Coldwell Formation Slate | ? |  |  |  | [NAME] | SILURIAN | NOT ENTERED |  |  |  |  |  | Not specifically identified during the course of this study. |  | SFP/GKL | Lake District National Park Authority | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4436 | [NAME] | 4433 |  | ? |  |  |  | BIRK RIGGS FORMATION | SILURIAN | SILTSTONE, MUDSTONE AND SANDSTONE |  |  |  |  |  | Not specifically identified during the course of this study. |  | SFP/GKL | Lake District National Park Authority | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4437 | [NAME] | 4433 | Brathay Formation Slate | Pale grey, fine-grained metasediments (mixed mudstones and siltstones) with a moderately developed slaty cleavage. | GREY | Uniform | Paler grey and pale brown weathering crusts can develop | BRATHAY FORMATION | SILURIAN | SILTSTONE AND MUDSTONE |  | Cleavage moderately well developed. | Pale grey, fine-grained metasediments which are cleaved to the extent that they fragment in a blocky and slabby manner. | Robust | Walling | Yes, but only specifically identified in two buildings ([NAME]). |  | SFP/GKL | Lake District National Park Authority | Cumbria English Heritage Atlas Area | GKL/SFP personal knowledge; fieldwork | 2012-05-16 10:20:33
4438 | Brathay Formation Slate | 4437 | [NAME] | ? |  |  |  | BRATHAY FORMATION | SILURIAN | NOT ENTERED |  |  |  |  |  | See 'Brathay Flags'. |  | SFP/GKL | Lake District National Park Authority | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4439 | Westmorland Slate | 4437 | Brathay Formation Slate | ? |  |  |  | BRATHAY FORMATION | SILURIAN | NOT ENTERED |  |  |  |  |  | Not specifically identified during the course of this study. |  | SFP/GKL | Lake District National Park Authority | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4440 | [NAME] | 4437 | Brathay Formation Slate | ? |  |  |  | BRATHAY FORMATION | SILURIAN | NOT ENTERED |  |  |  |  |  | Not specifically identified during the course of this study. |  | SFP/GKL | Lake District National Park Authority | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4441 | Stockdale Group | 4421 |  | ? |  |  |  | STOCKDALE GROUP | SILURIAN | SILTSTONE AND MUDSTONE |  |  |  |  |  | Not specifically identified during the course of this study. |  | SFP/GKL | Lake District National Park Authority | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4442 | Dent Group | 4421 |  | ? |  |  |  | DENT GROUP | ORDOVICIAN | NOT ENTERED |  |  |  |  |  | Not specifically identified during the course of this study. |  | SFP/GKL | Lake District National Park Authority | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4443 | Stile End Formation | 4442 |  | ? |  |  |  | STILE END FORMATION | ORDOVICIAN | NOT ENTERED |  |  |  |  |  | Not specifically identified during the course of this study. |  | SFP/GKL | Lake District National Park Authority | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4444 | Longsleddale Member | 4443 |  | ? |  |  |  | [NAME] MEMBER | ORDOVICIAN | NOT ENTERED |  |  |  |  |  | Not specifically identified during the course of this study. |  | SFP/GKL | Lake District National Park Authority | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4445 | Yarlside Volcanic Formation | 4442 |  | ? |  |  |  | YARLSIDE VOLCANIC FORMATION | ORDOVICIAN | NOT ENTERED |  |  |  |  |  | Not specifically identified during the course of this study. |  | SFP/GKL | Lake District National Park Authority | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4446 | Threlkeld Granite | 1 |  | Pale grey, alkali feldspar-quartz-plagioclase-phyric microgranite. | GREY | Uniform | Not observed | THRELKELD INTRUSION | ORDOVICIAN | NOT ENTERED |  | Carries phenocrysts. | Pale grey, porphyritic microgranite seen only in the vicinity of the Threlkeld Intrusion. | Robust | Walling (quoins) | Yes, but only specifically identified in Threlkeld itself. |  | SFP/GKL | Lake District National Park Authority | Cumbria English Heritage Atlas Area | GKL/SFP personal knowledge; fieldwork | 2012-05-16 10:20:33
4447 | Eskdale Granite | 1 |  | Pink, muscovite-bearing granite.  Seen as angular and squared blocks. | PINK | Uniform | Not observed | ESKDALE INTRUSIONS | ORDOVICIAN | NOT ENTERED |  |  | Pink, medium- and coarse-grained, muscovite-bearing granite. | Robust | Walling | Locally in SW Cumbria, locally in southwestern parts of the Park. |  | SFP/GKL | Lake District National Park Authority | Cumbria English Heritage Atlas Area | GKL/SFP personal knowledge; fieldwork | 2012-05-16 10:20:33
4448 | Ennerdale Granite | 1 |  | Pink biotite-microgranite (sometimes porphyritic, sometimes granophyric) accompnaied by greenish-grey 'diorite' and pink-grey hybridised variants. | PINK | Variable | Variable, dependent on the nature of an individual block. | ENNERDALE INTRUSION | ORDOVICIAN | NOT ENTERED |  | Phenocrysts obsrved in some blocks. | Pink biotite-microgranite accompanied by more basic lithologies and 'hybrids'. | Robust | Walling | Only observed in Buttermere. |  | SFP/GKL | Lake District National Park Authority | Cumbria English Heritage Atlas Area | GKL/SFP personal knowledge; fieldwork | 2012-05-16 10:20:33
4449 | Borrowdale Volcanic Group | 1 |  | A lithologically mixed grouping of rocks which includes pale green volcaniclastic metasediments and dark greenish-grey vesicular and non-vesicular volcanic rocks. |  | Variable | Variable, dependent on the nature of an individual block; some blocks can develop substantial pale coloured weathering crusts. | BORROWDALE VOLCANIC GROUP | ORDOVICIAN | NOT ENTERED |  | Meta-volcaniclastic rocks can show slumping-related features, while the volcanic rocks can be vesicular. | Metamorphosed volcaniclastic sediments and volcanic rocks (including vesicular varieties). | Robust | Walling | Used in areas underlain by or located close to Borrowdale Volcanic Group lithologies e.g. Ambleside. |  | SFP/GKL | Lake District National Park Authority | Cumbria English Heritage Atlas Area | GKL/SFP personal knowledge; fieldwork | 2012-05-16 10:20:33
4450 | [NAME] | 4449 |  | ? |  |  |  | DUDDON HALL TUFF FORMATION | ORDOVICIAN | NOT ENTERED |  |  |  |  |  | Not specifically identified during the course of this study. |  | SFP/GKL | Lake District National Park Authority | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4451 | Dunnerdale Sandstone Formation | 4449 |  | ? |  |  |  | DUNNERDALE SANDSTONE FORMATION | ORDOVICIAN | VOLCANICLASTIC SANDSTONE |  |  |  |  |  | Not specifically identified during the course of this study. |  | SFP/GKL | Lake District National Park Authority | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4452 | Caw Sandstone Formation | 4449 |  | ? |  |  |  | CAW SANDSTONE FORMATION | ORDOVICIAN | VOLCANICLASTIC SANDSTONE |  |  |  |  |  | Not specifically identified during the course of this study. |  | SFP/GKL | Lake District National Park Authority | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4453 | Lickle Tuff Formation | 4449 |  | ? |  |  |  | LICKLE TUFF FORMATION | ORDOVICIAN | NOT ENTERED |  |  |  |  |  | Not specifically identified during the course of this study. |  | SFP/GKL | Lake District National Park Authority | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4454 | Paddy End Tuff Member | 4453 |  | ? |  |  |  | PADDY END TUFF MEMBER | ORDOVICIAN | NOT ENTERED |  |  |  |  |  | Not specifically identified during the course of this study. |  | SFP/GKL | Lake District National Park Authority | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4455 | Stickle Pike Tuff Member | 4453 |  | ? |  |  |  | STICKLE PIKE TUFF MEMBER | ORDOVICIAN | NOT ENTERED |  |  |  |  |  | Not specifically identified during the course of this study. |  | SFP/GKL | Lake District National Park Authority | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4456 | Lag Bank Tuff Formation | 4449 |  | ? |  |  |  | LAG BANK TUFF FORMATION | ORDOVICIAN | NOT ENTERED |  |  |  |  |  | Not specifically identified during the course of this study. |  | SFP/GKL | Lake District National Park Authority | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4457 | Tarn Hows Tuff Formation | 4449 |  | ? |  |  |  | TARN HOWS TUFF FORMATION | ORDOVICIAN | NOT ENTERED |  |  |  |  |  | Not specifically identified during the course of this study. |  | SFP/GKL | Lake District National Park Authority | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4458 | Ulpha Andesite Formation | 4449 |  | ? |  |  |  | ULPHA ANDESITE FORMATION | ORDOVICIAN | NOT ENTERED |  |  |  |  |  | Not specifically identified during the course of this study. |  | SFP/GKL | Lake District National Park Authority | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4459 | [NAME] | 4449 |  | ? |  |  |  | WALLOWBARROW TUFF FORMATION | ORDOVICIAN | NOT ENTERED |  |  |  |  |  | Not specifically identified during the course of this study. |  | SFP/GKL | Lake District National Park Authority | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4460 | Waberthwaite [NAME] | 4449 |  | ? |  |  |  | WABERTHWAITE TUFF FORMATION | ORDOVICIAN | NOT ENTERED |  |  |  |  |  | Not specifically identified during the course of this study. |  | SFP/GKL | Lake District National Park Authority | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4461 | Elterwater Green Slates | 4460 | Waberthwaite [NAME] | ? |  |  |  | WABERTHWAITE TUFF FORMATION | ORDOVICIAN | NOT ENTERED |  |  |  |  |  | Not specifically identified during the course of this study. |  | SFP/GKL | Lake District National Park Authority | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4462 | Seathwaite Fell Sandstone Formation | 4449 |  | ? |  |  |  | SEATHWAITE FELL SANDSTONE FORMATION | ORDOVICIAN | VOLCANICLASTIC SEDIMENTS |  |  |  |  |  | Not specifically identified during the course of this study. |  | SFP/GKL | Lake District National Park Authority | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4463 | Tilberthwaite Green Slate | 4462 | Seathwaite Fell Sandstone Formation | ? |  |  |  | SEATHWAITE FELL SANDSTONE FORMATION | ORDOVICIAN | VOLCANICLASTIC SEDIMENTS |  |  |  |  |  | Not specifically identified during the course of this study. |  | SFP/GKL | Lake District National Park Authority | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4464 | Burlington Green Slate | 4462 | Seathwaite Fell Sandstone Formation | ? |  |  |  | SEATHWAITE FELL SANDSTONE FORMATION | ORDOVICIAN | VOLCANICLASTIC SEDIMENTS |  |  |  |  |  | Not specifically identified during the course of this study. |  | SFP/GKL | Lake District National Park Authority | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4465 | [NAME] | 4449 |  | ? |  |  |  | [NAME] | ORDOVICIAN | NOT ENTERED |  |  |  |  |  | Not specifically identified during the course of this study. |  | SFP/GKL | Lake District National Park Authority | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4466 | [NAME] | 4449 | [NAME] | ? |  |  |  | [NAME] | ORDOVICIAN | NOT ENTERED |  |  |  |  |  | Not specifically identified during the course of this study. |  | SFP/GKL | Lake District National Park Authority | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4467 | Birker Fell Andesite Formation | 4449 |  | ? |  |  |  | BIRKER FELL ANDESITE FORMATION | ORDOVICIAN | NOT ENTERED |  |  |  |  |  | Not specifically identified during the course of this study. |  | SFP/GKL | Lake District National Park Authority | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4468 | Eagle Crag Sandstone Member | 4467 |  | ? |  |  |  | EAGLE CRAG SANDSTONE MEMBER | ORDOVICIAN | VOLCANICLASTIC SEDIMENTS |  |  |  |  |  | Not specifically identified during the course of this study. |  | SFP/GKL | Lake District National Park Authority | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4469 | Buttermere & Honister Green Slates | 4467 |  | ? |  |  |  | EAGLE CRAG SANDSTONE MEMBER | ORDOVICIAN | NOT ENTERED |  |  |  |  |  | Not specifically identified during the course of this study. |  | SFP/GKL | Lake District National Park Authority | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4470 | Esk Pike Sandstone Formation | 4449 |  | ? |  |  |  | ESK PIKE SANDSTONE FORMATION | ORDOVICIAN | VOLCANICLASTIC SEDIMENTS |  |  |  |  |  | Not specifically identified during the course of this study. |  | SFP/GKL | Lake District National Park Authority | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4471 | Lincomb Tarns [NAME] | 4449 |  | ? |  |  |  | LINCOMB TARNS TUFF FORMATION | ORDOVICIAN | VOLCANICLASTIC SANDSTONE |  |  |  |  |  | Not specifically identified during the course of this study. |  | SFP/GKL | Lake District National Park Authority | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4472 | [NAME] Intrusives | 1 |  | ? |  |  |  | BORROWDALE SILL SUITE | ORDOVICIAN | NOT ENTERED |  |  |  |  |  | Not specifically identified during the course of this study. |  | SFP/GKL | Lake District National Park Authority | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4473 | Lake District Ordovician Minor Intrusion Suite | 1 |  | ? |  |  |  | LAKE DISTRICT ORDOVICIAN MINOR INTRUSION SUITE | ORDOVICIAN | NOT ENTERED |  |  |  |  |  | Not specifically identified during the course of this study. |  | SFP/GKL | Lake District National Park Authority | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4474 | Skiddaw Group | 1 |  | The Skiddaw Group as a whole is lithologically mixed, but the building stones of Skiddaw Group derivation encountered during this study tended to be dark grey, slabby, imperfectly cleaved meta-siltstones and mudstones. | GREY | Variable | Some blocks weather a rusty brown colour. | SKIDDAW GROUP | ORDOVICIAN | MUDSTONES AND SILTSTONES |  | Imperfect slaty cleavage. | Commonly dark grey, imperfectly cleaved, fine-grained metasediments. | Seemingly robust | Walling | Used in areas underlain by or located close to Skiddaw Group lithologies. |  | SFP/GKL | Lake District National Park Authority | Cumbria English Heritage Atlas Area | GKL/SFP personal knowledge; fieldwork | 2012-05-16 10:20:33
4475 | [NAME] | 4474 |  | ? |  |  |  | KIRK STILE FORMATION | ORDOVICIAN | MUDSTONES AND SILTSTONES |  |  |  |  |  | Not specifically identified during the course of this study. |  | SFP/GKL | Lake District National Park Authority | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4476 | Watch Hill Formation | 4474 |  | ? |  |  |  | WATCH HILL FORMATION | ORDOVICIAN | SANDSTONE, SILTSTONE AND MUDSTONE |  |  |  |  |  | Not specifically identified during the course of this study. |  | SFP/GKL | Lake District National Park Authority | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4477 | Buttermere Formation | 4474 |  | ? |  |  |  | BUTTERMERE FORMATION | ORDOVICIAN | NOT ENTERED |  |  |  |  |  | Not specifically identified during the course of this study. |  | SFP/GKL | Lake District National Park Authority | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4478 | Sandstone, Carboniferous | 4407 |  | Term applied to [NAME] coloured sandstones utilised for dressings in buildings not visited during the course of this study.  These sandstones are believed to derive from the Carboniferous successions of Cumbria or Northern England generally, but physical examination would be necessary to confirm this and better constrain their stratigraphical origins. | BUFF |  |  | CARBONIFEROUS ROCKS (UNDIFFERENTIATED) | CARBONIFEROUS | NOT ENTERED |  |  |  |  | Dressings | Yes (used as dressings) |  | SFP/GKL | Lake District National Park Authority | Cumbria English Heritage Atlas Area |  | 2012-05-16 10:20:33
4479 | Stone flags (Unknown) | 1 |  | Fissile sedimentary rock. |  |  |  | PARENT DATA NOT YET ENTERED [HIERARCHY CODE] |  | NOT ENTERED |  |  |  |  | Roofing | Lake District usage |  | SFP/GKL | Lake District National Park Authority | Cumbria English Heritage Atlas Area | Cumbria Buildings Spreadsheet | 2012-05-16 10:20:33
10752 | Westmorland Green Slate | 1 |  |  |  |  |  | BORROWDALE VOLCANIC GROUP | ORDOVICIAN | SLATE |  |  |  |  | Building stone, roofing stone | Manchester usage |  | D Cameron | Cumbria County Council | Cumbria English Heritage Atlas Area | GM Buildings Spreadsheet, [NAME] spreadsheet | 2012-05-16 10:20:33
11731 | Penrith Sandstone | 1 |  | Red Sandstone | RED | Uniform |  | PENRITH SANDSTONE FORMATION | PERMIAN | SANDSTONE | FINE GRAINED |  |  |  | Building stone | Manchester usage |  | D Cameron | Cumbria County Council | Cumbria English Heritage Atlas Area | GM Buildings Spreadsheet | 2012-05-16 10:20:33
11732 | Shap Granite | 1 | Red Shap | Coarse grained, red, granite with pink feldspar phenocrysts | RED | Uniform |  | SHAP PLUTON |  | GRANITE, COARSE-GRAINED | [NAME] |  | Large Potassium feldspar crystals |  | Building stone | Manchester usage |  | D Cameron | Cumbria County Council | Cumbria English Heritage Atlas Area | GM Buildings Spreadsheet | 2012-05-16 10:20:33
11733 | Borrowdale Volcanics | 1 |  | Medium to high-k, continental margin [NAME] basalt-andesite-rhyolite volcanic association of lavas, sills, pyroclastic and reworked pyroclastic deposits | GREEN | Banded |  | BORROWDALE VOLCANIC GROUP | ORDOVICIAN | VOLCANOCLASTIC ROCKS |  |  |  |  | Walling, decorative | Manchester usage |  | D Cameron | Cumbria County Council | Cumbria English Heritage Atlas Area | GM Buildings Spreadsheet | 2012-05-16 10:20:33