Knowledge (XXG)

Laumontite

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It is monoclinic, space group C2/m. It forms prismatic crystals with a diamond-shaped cross-section and an angled termination. When pure, the color is colorless or white. Impurities may color it orange, brownish, gray, yellowish, pink, or reddish. It has perfect cleavage on and and its fracture
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Laumontite easily dehydrates when stored in a low humidity environment. When freshly collected, if it has not already been exposed to the environment, it can be translucent or transparent. Over a period of hours to days the loss of water turns it opaque white. In the past, this variety has been
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scale hardness is 3.5-4. It has a vitreous luster and a white streak. It is found in hydrothermal deposits left in calcareous rocks, often formed as a result of secondary mineralization. Host rock types include
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called leonhardite, though this is not a valid mineral species. The dehydrated laumontite is very friable, often falling into a powder at the slightest touch.
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It is a common mineral, found worldwide. It can be locally abundant, forming seams and veins. It is frequently associated with other zeolites, including
252:. It forms at a temperature of about 100 °C (212 °F), and becomes unstable above about 150 °C (302 °F), and so its presence in 506: 60: 435: 232: 145: 511: 501: 491: 471: 275:
in 1809. The current name was given by K.C. von Leonhard (Handbuch der Oryktognosie) in 1821. It is named after
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Sedimentary geology : an introduction to sedimentary rocks and stratigraphy
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The identification of laumontite goes back to the early days of
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may substitute for the calcium but only in very small amounts.
430:(2nd ed.). New York: W.H. Freeman. p. 124. 256:indicates that these have experienced intermediate 157: 144: 134: 124: 116: 111: 99: 81: 69: 59: 49: 37: 32: 18: 271:(System of Mineralogy) in 1805, and laumonite by 341:after laumontite (epimorphs) have been found in 8: 426:Prothero, Donald R.; Schwab, Fred (2004). 387: 279:who collected samples from lead mines in 231:is conchoidal. It is very brittle. The 219:, a hydrated calcium-aluminium silicate. 214: 207: 203: 197: 354: 15: 120:White, colorless, yellowish, brownish 7: 364:"IMA–CNMNC approved mineral symbols" 267:. It was first named lomonite by 14: 413:Field Guide to Rocks and Minerals 411:National Audubon Society (1979). 185:group. Its molecular formula is 24: 1: 306:. Notable occurrences are 528: 507:Minerals in space group 12 460:IMA Zeolite Classification 23: 415:. Alfred A. Knopf, Inc. 130:Perfect, two directions 368:Mineralogical Magazine 171: 455:Webmineral Laumontite 169: 61:Strunz classification 512:Luminescent minerals 312:Paterson, New Jersey 502:Monoclinic minerals 389:10.1180/mgm.2021.43 380:2021MinM...85..291W 362:Warr, L.N. (2021). 170:Laumontite crystals 492:Aluminium minerals 472:Structure type LAU 287:, making them the 172: 450:Mindat Laumontite 277:Gillet de Laumont 254:sedimentary rocks 246:metamorphic rocks 164: 163: 95: 519: 487:Calcium minerals 442: 441: 423: 417: 416: 408: 402: 401: 391: 359: 218: 150: 89: 87:Prismatic (2/m) 28: 16: 527: 526: 522: 521: 520: 518: 517: 516: 477: 476: 468: 446: 445: 438: 425: 424: 420: 410: 409: 405: 361: 360: 356: 351: 216: 209: 205: 199: 186: 148: 88: 44: 12: 11: 5: 525: 523: 515: 514: 509: 504: 499: 494: 489: 479: 478: 475: 474: 467: 466:External links 464: 463: 462: 457: 452: 444: 443: 436: 418: 403: 374:(3): 291–320. 353: 352: 350: 347: 314:; Pine Creek, 273:René Just Haüy 162: 161: 159: 155: 154: 151: 142: 141: 138: 132: 131: 128: 122: 121: 118: 114: 113: 112:Identification 109: 108: 103: 97: 96: 85: 79: 78: 73: 71:Crystal system 67: 66: 63: 57: 56: 53: 47: 46: 42:Tectosilicates 39: 35: 34: 30: 29: 21: 20: 13: 10: 9: 6: 4: 3: 2: 524: 513: 510: 508: 505: 503: 500: 498: 495: 493: 490: 488: 485: 484: 482: 473: 470: 469: 465: 461: 458: 456: 453: 451: 448: 447: 439: 433: 429: 422: 419: 414: 407: 404: 399: 395: 390: 385: 381: 377: 373: 369: 365: 358: 355: 348: 346: 344: 340: 337: 333: 329: 325: 321: 317: 313: 309: 305: 301: 296: 292: 290: 289:type locality 286: 282: 278: 274: 270: 266: 261: 259: 255: 251: 247: 243: 239: 234: 228: 226: 222: 213: 202: 196: 193: 189: 184: 181:, one of the 180: 176: 168: 160: 156: 152: 147: 143: 139: 137: 133: 129: 127: 123: 119: 115: 110: 107: 104: 102: 98: 93: 86: 84: 83:Crystal class 80: 77: 74: 72: 68: 64: 62: 58: 54: 52: 48: 43: 40: 36: 31: 27: 22: 17: 427: 421: 412: 406: 371: 367: 357: 339:pseudomorphs 328:Bay of Fundy 297: 293: 262: 229: 174: 173: 105: 332:Nova Scotia 101:Space group 481:Categories 437:0716739054 349:References 326:; and the 316:California 304:heulandite 269:R. Jameson 265:mineralogy 258:diagenesis 175:Laumontite 158:References 146:Mohs scale 92:H-M symbol 76:Monoclinic 51:IMA symbol 19:Laumontite 398:235729616 221:Potassium 497:Zeolites 336:Prehnite 324:Scotland 300:stilbite 285:Brittany 281:Huelgoat 250:granites 242:andesite 210:· 4 149:hardness 136:Fracture 126:Cleavage 45:Zeolites 38:Category 376:Bibcode 320:Iceland 183:zeolite 179:mineral 65:9.GB.10 33:General 434:  396:  238:basalt 225:sodium 140:Uneven 90:(same 394:S2CID 343:India 308:India 177:is a 117:Color 432:ISBN 302:and 248:and 233:Mohs 106:C2/m 384:doi 334:. 223:or 55:Lmt 483:: 392:. 382:. 372:85 370:. 366:. 345:. 330:, 322:; 318:; 310:; 291:. 283:, 260:. 244:, 240:, 195:Si 192:Al 188:Ca 440:. 400:. 386:: 378:: 217:O 215:2 212:H 208:2 206:) 204:6 201:O 198:2 190:( 153:4 94:)

Index


Tectosilicates
IMA symbol
Strunz classification
Crystal system
Monoclinic
Crystal class
H-M symbol
Space group
Cleavage
Fracture
Mohs scale

mineral
zeolite
Ca
Al
Si
O
H
Potassium
sodium
Mohs
basalt
andesite
metamorphic rocks
granites
sedimentary rocks
diagenesis
mineralogy

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