Knowledge (XXG)

Magnesian Limestone

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Marl') and above this the Brotherton Formation (formerly the 'Upper Magnesian Limestone'). In the north, the Lower Magnesian Limestone is now referred to as the Raisby Formation and the middle Magnesian Limestone as the Ford Formation. The Upper Magnesian Limestone is replaced by the Roker Formation
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but also for aggregate for road-building and other construction purposes. It is also used in the production of agricultural lime. This type of limestone was used for statues in antiquity because of its resistance to acid. Many pieces of dolomite were found in the ruins of Rome, though they are
105:(in its lower part) and the Seaham Formation (in its upper part) with the Edlington formation between them, though in the Durham area this last is replaced by the Fordham Evaporite Formation and the Seaham Residue. 201: 45: 33: 112:, i.e. calcium magnesium carbonate, and has been for many years the main source of dolomite-rock in Britain. It is used in connection with the production of 89:. The term has now been discontinued in formal use though it appears widely in popular and scientific literature on the geology of northern England. 221: 226: 38: 118: 20: 96:. In the southern part of its outcrop, the former 'Lower Magnesian Limestone' is now referred to as the ' 185: 97: 137:
British Geological Survey 1:625,000 scale geological maps (North and South sheets) 3rd edition 1979
113: 194: 109: 93: 27: 173: 58: 215: 86: 78: 101: 82: 70: 74: 66: 62: 44: 32: 100:'. Overlying this it is the 'Edlington Formation' (formerly the ' 176:, George Shaw, Richard Pearson, C, & R. Baldwin (1809). "". 178:
Philosophical Transactions of the Royal Society of London
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British Regional Geology: the Pennines and adjacent areas
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The Magnesian Limestone is now incorporated within the
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Cellular patterns in a boulder of Magnesian Limestone
163:(5th ed.) (British Geological Survey, Nottingham) 150:(4th ed.) (British Geological Survey, Nottingham) 8: 81:where it is exposed along the coast between 161:British Regional Geology: Northern England 26:For general magnesium-rich limestone, see 200:CS1 maint: multiple names: authors list ( 130: 183: 7: 108:Much of the Magnesian Limestone is 69:period. The outcrop stretches from 37:The cliffs of Magnesian Limestone, 16:Suite of carbonate rocks in England 117:thought to have been brought from 14: 1: 146:Aitkenhead, N., et al 2002. 243: 25: 18: 193:Cite uses generic title ( 222:Permian System of Europe 19:Not to be confused with 159:Stone, P., et al 2010 50: 42: 21:Magnesian Conglomerate 48: 36: 73:northwards through 55:Magnesian Limestone 227:Geology of England 51: 43: 114:refractory bricks 234: 206: 205: 198: 191: 189: 181: 170: 164: 157: 151: 144: 138: 135: 98:Cadeby Formation 65:dating from the 242: 241: 237: 236: 235: 233: 232: 231: 212: 211: 210: 209: 199: 192: 182: 172: 171: 167: 158: 154: 145: 141: 136: 132: 127: 94:Zechstein Group 59:carbonate rocks 31: 28:Dolomite (rock) 24: 17: 12: 11: 5: 240: 238: 230: 229: 224: 214: 213: 208: 207: 174:Charles Hutton 165: 152: 139: 129: 128: 126: 123: 102:Middle Permian 61:in north-east 57:is a suite of 15: 13: 10: 9: 6: 4: 3: 2: 239: 228: 225: 223: 220: 219: 217: 203: 196: 187: 179: 175: 169: 166: 162: 156: 153: 149: 143: 140: 134: 131: 124: 122: 120: 115: 111: 106: 103: 99: 95: 90: 88: 87:South Shields 84: 80: 79:County Durham 76: 72: 68: 64: 60: 56: 47: 40: 35: 29: 22: 186:cite journal 177: 168: 160: 155: 147: 142: 133: 107: 91: 54: 52: 121:in Greece. 216:Categories 125:References 83:Hartlepool 71:Nottingham 39:Grangetown 77:and into 75:Yorkshire 41:promenade 119:Magnesia 110:dolomite 67:Permian 63:England 202:link 195:help 85:and 53:The 218:: 190:: 188:}} 184:{{ 204:) 197:) 180:. 30:. 23:.

Index

Magnesian Conglomerate
Dolomite (rock)

Grangetown

carbonate rocks
England
Permian
Nottingham
Yorkshire
County Durham
Hartlepool
South Shields
Zechstein Group
Cadeby Formation
Middle Permian
dolomite
refractory bricks
Magnesia
Charles Hutton
cite journal
help
link
Categories
Permian System of Europe
Geology of England

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