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Rimstone

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structures on a floor with a gradual sloping surface or on the side of rounded stalagmites derived from concrete. Most of the calcium carbonate carried by the leachate is deposited as stalactites (when the drop rate is slower than one drop per minute), leaving little in solution to be carried to the
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above or below the original rimstone. Often, rimstone is covered with small, micro-gours on horizontal surfaces. Rimstone basins may form terraces that extend over hundreds of feet, with single basins known up to 200 feet long from Tham Xe Biang Fai in Laos.
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When dams form under running water, they tend to be higher when the passage is steeper. Shallow-gradient dams tend to be lower and more sinuous in nature. Rimstone is one of the most common cave formations, after flowstone,
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ground to create stalagmites, flowstone and gours. The leachate which does reach the ground usually evaporates quickly due to air movement beneath the concrete structure, hence micro-gours are more common.
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leachate solution, which facilitates the chemical reactions to precipitate any calcium carbonate remaining in solution as a stalagmite and micro-gours. This chemical reaction creating
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Rimstone or gours can be formed by the secondary deposits derived from concrete, lime or mortar. These secondary deposits consisting primarily of calcium carbonate, are called
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Macleod, G., Hall, A. J. and Fallick, A. E., 1990. "An applied mineralogical investigation of concrete degradation in a major concrete road bridge".
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deposition as micro-gours occur when the solution drops to the ground under the concrete structure. Carbon dioxide is absorbed into the
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interface. The turbulence caused by flow over the edge of the building dam may contribute to the outgassing or loss of
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and other minerals that build up in cave pools. The formation created, which looks like stairs, often extends into
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Secondary deposits, which create stalagmites, stalactites, flowstone, rimstone etc., outside the natural
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are leached out of the concrete in solution and redeposited on the underside of a concrete structure.
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The secondary deposits derived from concrete are the result of concrete degradation, where
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Calthemite gours on a small rounded stalagmite – a secondary deposit derived from concrete
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Smith, G. K. (2016). "Calcite straw stalactites growing from concrete structures".
89:, and hence flow, over the edge of a pool. Crystallization begins to occur at the 42: 37: 102: 98: 308: 86: 49: 184: 183:”. These concrete derived secondary deposits cannot be referred to as “ 180: 172:, is different from that which creates speleothems in limestone caves. 169: 142: 138: 118: 114: 65: 73: 68:(cave formation) in the form of a stone dam. Rimstone is made up of 165: 146: 154: 69: 141:
and mimics the shapes and forms of cave speleothems to create
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Moore, G. W. (1952). "Speleothems – a new cave term".
306: 124: 256: 232: 230: 228: 226: 30:"Gours" redirects here. For other uses, see 223: 203: 128: 48: 36: 85:Rimstone dams form where there is some 14: 307: 206:"The World's Largest Cave Formations" 187:” due to the definition of the word. 300:The Virtual Cave's page on Rimstone 284:National Speleological Society News 262:Hill, C. A. and Forti, P., (1997). 24: 25: 326: 179:environment, are referred to as “ 53:Rimstone in Cate's Cave, Anguilla 276: 243: 197: 13: 1: 190: 125:Concrete derived micro-gours 80: 7: 10: 331: 293: 264:Cave Minerals of the World 29: 251:Mineralogical Magazine 238:Cave and Karst Science 134: 54: 46: 32:Gours (disambiguation) 132: 52: 40: 266:, Second edition. 253:, Vol. 54, 637–644. 286:, Vol.10(6), p. 2. 135: 55: 47: 162:Calcium carbonate 16:(Redirected from 322: 287: 280: 274: 260: 254: 247: 241: 240:43(1), pp. 4–10. 234: 221: 220: 218: 216: 210:The Virtual Cave 201: 21: 330: 329: 325: 324: 323: 321: 320: 319: 305: 304: 296: 291: 290: 281: 277: 261: 257: 248: 244: 235: 224: 214: 212: 202: 198: 193: 127: 83: 64:, is a type of 43:Endless Caverns 35: 28: 23: 22: 15: 12: 11: 5: 328: 318: 317: 303: 302: 295: 292: 289: 288: 275: 255: 242: 222: 204:Dave Bunnell. 195: 194: 192: 189: 126: 123: 103:carbon dioxide 82: 79: 60:, also called 27:Cave formation 26: 9: 6: 4: 3: 2: 327: 316: 313: 312: 310: 301: 298: 297: 285: 279: 273: 272:1-879961-07-5 269: 265: 259: 252: 246: 239: 233: 231: 229: 227: 211: 207: 200: 196: 188: 186: 182: 178: 173: 171: 167: 163: 159: 156: 151: 148: 144: 140: 131: 122: 120: 116: 110: 108: 104: 100: 96: 92: 88: 78: 75: 71: 67: 63: 59: 51: 44: 39: 33: 19: 283: 278: 263: 258: 250: 245: 237: 215:December 16, 213:. Retrieved 209: 199: 174: 152: 136: 111: 84: 61: 57: 56: 315:Speleothems 185:speleothems 181:calthemites 170:calthemites 143:stalactites 139:calthemites 119:stalagmites 115:stalactites 41:Rimstone – 191:References 66:speleothem 45:, Virginia 81:Formation 74:flowstone 18:Gour pool 309:Category 166:alkaline 147:concrete 87:gradient 58:Rimstone 294:Sources 155:calcium 70:calcite 270:  117:, and 107:water 105:from 95:water 62:gours 268:ISBN 217:2008 177:cave 158:ions 99:rock 91:air 311:: 225:^ 208:. 121:. 219:. 97:/ 93:/ 34:. 20:)

Index

Gour pool
Gours (disambiguation)

Endless Caverns

speleothem
calcite
flowstone
gradient
air
water
rock
carbon dioxide
water
stalactites
stalagmites

calthemites
stalactites
concrete
calcium
ions
Calcium carbonate
alkaline
calthemites
cave
calthemites
speleothems
"The World's Largest Cave Formations"

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