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Millstone Grit

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The Lower Follifoot Grit, Silver Hills Sandstone, Nottage Crag Grit, Marchup Grit, Red Scar Grit, Ward’s Stone Sandstone, Cocklett Scar Sandstones and Dure Clough Sandstones are all assigned to the following Arnsbergian sub-stage. The Kinderscoutian includes the Kinder Grit, Longnor Sandstones, Shale
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across the areas where it outcrops is considerable. In neighbouring limestone areas, gritstone has often been preferred in the past for use as gateposts and lintels. The very name of the rock derives from its widespread use within cornmills where it proved suitable for grinding stones. It also found
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Rivers running north off the Wales-Brabant High deposited material in the southern parts of the Pennine basin from northeast Wales to the Peak District. Southerly flowing rivers from this same landmass were responsible for the Millstone Grit/Marros Group succession in South Wales.
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agricultural use as drinking troughs for animals. The majority of the quarrying for such use took place along the eastern edges of the Peak District. Millstone Edge was a significant source whilst abandoned millstones can be seen below the edges at Stanage, Froggatt and Baslow.
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A millstone shaped from Millstone Grit quarried in the area has been adopted as the emblem of the Peak District National Park. As an image, the millstone is widely visible on literature but use is made of the objects themselves at many of the entrances to the National Park.
421:. Britain lay in the equatorial region. At times of high sea-level, silt and mud accumulated within the Pennine basin whilst at times of low sea-level, major deltas prograded across the region, their legacy being the thick sandstone beds of the Millstone Grit Group. 518:
developed at much the same time as access for walkers to the moors of the Pennines was established during the first half of the twentieth century. Their proximity to large centres of population resulted in their rapid development as climbing venues.
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The Millstone Grit Group comprises over thirty individually named sandstones, some of regional extent, others more local in their occurrence. The intervening mudstones and siltstones are not generally named though important
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Rocks assigned to the Millstone Grit Group occur over a wide area of Northern England, where they are a hugely important landscape-forming element of the rock succession. They also occur in parts of northeast
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During much of the Carboniferous Period, world sea-levels were fluctuating in response to the growth and decline of a series of major ice-caps over the continents then clustered around the
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Towards the western margins of the Peak District are a rather more broken series of edges, facing in a variety of directions, from those surrounding the high plateaux of
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The closing sub-stage of the Namurian, the Yeadonian includes the Lower Haslingden Flags and the last sandstone in the entire Millstone Grit succession known as the
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Various of the sandstone beds of the Millstone Grit have been quarried for building stone, paving flags and roofing material. Its use in the construction of
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The gritstone edges of West Yorkshire and the Peak District provide one of the classic areas in Britain for rock climbing. Public access to these edges for
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of central Lancashire. It is succeeded by the sandstone known variously as the Brennand Grit, Warley Wise Grit and Grassington Grit. These are all of
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was formerly considered to be the uppermost unit of the Millstone Grit series of South Wales though it is now included within the overlying
752: 691: 742: 757: 464:, Gorpley Grit, Pule Hill Grit, Fletcher Bank Grit, Brooksbottom Grit, Five Clouds Sandstones and Sheen Sandstones are assigned. 609: 348:. The thickest bed of sandstone within it was known as the Basal Grit and this has now been renamed as the Twrch Sandstone. The 747: 368:
in northwest Ireland, describing the series of shales, grits, and coal seams, occurring from the base of the Namurian upwards.
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The ‘eastern edges of the Peak District’ comprise a broadly north-south arranged series of west-facing cliffs from
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was formerly used to refer to the rocks now included within the Millstone Grit Group together with the underlying
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in the south. To the east of these edges is a broad band of relatively flat moorland known as the Eastern Moors.
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describes any sandstone composed of coarse angular grains, and specifically refers to such sandstones within the
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Grit, Todmorden Grit, Parsonage Sandstone, Heysham Harbour Sandstone, Eldroth Grit and Ellel Crag Sandstone.
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received input of sand and mud largely from southerly directed rivers from these northern landmasses.
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are found though the Millstone Grit Series of this region has recently been formally renamed by the
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is a notable type of Millstone Grit sourced from around the village of Bramley, near Leeds.
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The next sub-stage of the Namurian succession is the Marsdenian and it is to this that the
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into which numerous wells and boreholes have been sunk to provide local water supplies.
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region. One particular east-west aligned landmass stretched from Wales through the
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throughout the region, many of which are of considerable cultural significance.
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and fringed with broken outcrops of gritstone are characteristic of the area.
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The Palaeontology of the Namurian Rocks of Slieve Anierin, Co. Leitrim, Eire
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which attains a thickness of around 45m though is more generally 15m thick.
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Explanation to Accompany Sheets 1-, Volume 60; Volumes 62-63; Volumes 65-90
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They are the major landscape-forming rocks of the northern part of the
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The oldest, and hence lowermost in the succession is the thick
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A small area of Millstone Grit Group rocks stretches through
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British Regional Geology: the Pennines and adjacent areas
571: 539:. Grassington: Yorkshire Dales National Park Committee. 553: 445:(E1) age – the lowermost sub-stage of the Namurian. 599:
Various of BGS 1:50,000 scale geological map sheets
286:they cover the south-east edge, but north of the 734: 157:) and of its eastern and western flanks in the 332:The term "Millstone Grit" was also adopted in 294:, they form only cappings to separate hills. 582: 580: 537:Geology of the Yorkshire Dales National Park 97:and neighbouring areas of Northern England. 528: 258:These rocks extend northwards through the 100: 577: 402:to the continent and is now known as the 173:. The great expanses of moorland around 137: 26: 14: 735: 690:: CS1 maint: archived copy as title ( 534: 478: 717: 559: 46:is any of a number of coarse-grained 701: 31:The Salt Cellar, a gritstone tor on 24: 753:Stratigraphy of the United Kingdom 709:Geological Survey Ireland (1878). 502:Crushed gritstone is also used as 364:The term has also been adopted at 297: 25: 769: 509: 495:Some of the sandstones serve as 376:The Millstone Grit dates to the 743:Sandstone in the United Kingdom 506:in path and road construction. 424: 336:where rocks of similar age and 758:Carboniferous System of Europe 653: 627: 602: 593: 572:Geological Survey Ireland 1878 321: 282:, also in Lancashire. At the 13: 1: 748:Geology of the United Kingdom 639:Stone in Archaeology Database 522: 310:into the northwest corner of 145:in the eastern Peak district 7: 718:Yates, Patricia J. (1957). 641:. University of Southampton 590:(4th Edn) (BGS, Nottingham) 133: 10: 774: 586:Aitkenhead, N. et al 2002 371: 359: 325: 78:. The term Millstone Grit 354:South Wales Coal Measures 342:British Geological Survey 239:to the imposing crags of 70:beds and the intervening 535:Wilson, Alfred (1992). 434:within them are named. 270:and westwards into the 126:, and a series of high 101:Geographical occurrence 62:for use principally in 54:age which occur in the 146: 74:as the Millstone Grit 40: 471:. It is a widespread 326:Further information: 188:in the north through 141: 30: 635:"Bramley Fall Stone" 272:Forest of Rossendale 218:Dobb/Chatsworth Edge 562:, pp. 356–357. 479:Economic importance 122:, known locally as 490:Bramley Fall stone 404:Wales-Brabant High 147: 41: 702:Secondary sources 280:Forest of Bowland 84:Edale Shale Group 16:(Redirected from 765: 728: 726: 714: 696: 695: 689: 681: 679: 678: 672: 666:. Archived from 665: 657: 651: 650: 648: 646: 631: 625: 624: 622: 621: 612:. Archived from 606: 600: 597: 591: 584: 575: 569: 563: 557: 551: 550: 532: 396:English Midlands 21: 773: 772: 768: 767: 766: 764: 763: 762: 733: 732: 731: 724: 704: 699: 683: 682: 676: 674: 670: 663: 661:"Archived copy" 659: 658: 654: 644: 642: 633: 632: 628: 619: 617: 608: 607: 603: 598: 594: 585: 578: 570: 566: 558: 554: 547: 533: 529: 525: 512: 485:dry stone walls 481: 454:Chatsworth Grit 427: 374: 362: 330: 324: 300: 298:Northeast Wales 284:Yorkshire Dales 136: 103: 23: 22: 15: 12: 11: 5: 771: 761: 760: 755: 750: 745: 730: 729: 715: 705: 703: 700: 698: 697: 652: 626: 601: 592: 576: 574:, p. 188. 564: 552: 545: 526: 524: 521: 511: 508: 480: 477: 426: 423: 373: 370: 366:Slieve Anierin 361: 358: 323: 320: 299: 296: 268:West Yorkshire 260:South Pennines 251:in the south. 135: 132: 110:and northwest 102: 99: 44:Millstone Grit 18:Millstone grit 9: 6: 4: 3: 2: 770: 759: 756: 754: 751: 749: 746: 744: 741: 740: 738: 723: 722: 716: 712: 707: 706: 693: 687: 673:on 2009-11-12 669: 662: 656: 640: 636: 630: 616:on 2009-11-11 615: 611: 605: 596: 589: 583: 581: 573: 568: 561: 556: 548: 546:0-905455-34-7 542: 538: 531: 527: 520: 517: 510:Rock climbing 507: 505: 500: 498: 493: 491: 486: 476: 474: 470: 465: 463: 459: 455: 450: 446: 444: 440: 435: 433: 422: 420: 415: 411: 409: 408:Pennine Basin 405: 401: 397: 393: 392:British Isles 389: 386: 385:Carboniferous 382: 379: 369: 367: 357: 355: 351: 350:Farewell Rock 347: 343: 339: 335: 329: 319: 317: 313: 309: 305: 295: 293: 289: 288:Craven Faults 285: 281: 277: 276:West Pennines 273: 269: 265: 261: 256: 252: 250: 249:Ramshaw Rocks 246: 242: 238: 234: 229: 227: 226:Fallinge Edge 223: 219: 215: 211: 210:Gardom's Edge 207: 203: 199: 198:Froggatt Edge 195: 191: 187: 182: 180: 176: 172: 168: 167:Staffordshire 164: 160: 156: 152: 151:Peak District 144: 140: 131: 129: 125: 121: 117: 113: 109: 98: 96: 92: 87: 85: 81: 77: 73: 69: 65: 61: 57: 56:British Isles 53: 52:Carboniferous 49: 45: 38: 37:Peak District 34: 29: 19: 720: 675:. Retrieved 668:the original 655: 643:. Retrieved 638: 629: 618:. Retrieved 614:the original 610:"Black Rock" 604: 595: 587: 567: 555: 536: 530: 513: 501: 494: 482: 466: 462:Ashover Grit 458:Roaches Grit 451: 447: 436: 432:marine bands 428: 425:Stratigraphy 416: 412: 375: 363: 346:Marros Group 331: 328:Marros Group 301: 257: 253: 233:Kinder Scout 230: 222:Harland Edge 214:Birchen Edge 194:Burbage Edge 190:Stanage Edge 186:Bamford Edge 183: 148: 143:Stanage Edge 123: 104: 88: 43: 42: 33:Derwent Edge 439:Pendle Grit 400:East Anglia 334:South Wales 322:South Wales 241:the Roaches 206:Baslow Edge 202:Curbar Edge 120:escarpments 737:Categories 677:2009-12-20 645:13 January 620:2009-12-20 560:Yates 1957 523:References 469:Rough Rock 419:South Pole 312:Shropshire 304:Flintshire 292:weathering 264:Lancashire 237:Combs Moss 179:Black Hill 163:Derbyshire 116:siltstones 64:watermills 60:millstones 48:sandstones 504:aggregate 443:Pendleian 338:lithology 290:, due to 245:Hen Cloud 155:Dark Peak 91:gritstone 89:The term 72:mudstones 68:limestone 39:, England 686:cite web 516:climbing 497:aquifers 378:Namurian 316:Oswestry 278:and the 175:Bleaklow 171:Cheshire 159:counties 134:Pennines 128:plateaux 95:Pennines 383:of the 372:Origins 360:Ireland 344:as the 308:Wrexham 112:Ireland 35:in the 543:  388:Period 80:Series 725:(PDF) 671:(PDF) 664:(PDF) 381:Stage 314:near 153:(the 124:edges 108:Wales 76:Group 692:link 647:2023 541:ISBN 473:unit 398:and 306:and 274:and 266:and 247:and 235:and 224:and 177:and 169:and 262:of 161:of 50:of 739:: 688:}} 684:{{ 637:. 579:^ 460:, 356:. 318:. 243:, 220:, 216:, 212:, 208:, 204:, 200:, 196:, 192:, 165:, 86:. 694:) 680:. 649:. 623:. 549:. 20:)

Index

Millstone grit

Derwent Edge
Peak District
sandstones
Carboniferous
British Isles
millstones
watermills
limestone
mudstones
Group
Series
Edale Shale Group
gritstone
Pennines
Wales
Ireland
siltstones
escarpments
plateaux

Stanage Edge
Peak District
Dark Peak
counties
Derbyshire
Staffordshire
Cheshire
Bleaklow

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