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Panhole

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184:, where they are thought to indicate rock surfaces that are unglaciated or escaped more recent glaciations. In Sierra Nevada granitic rocks, these features have a characteristic shape such that they expand more rapidly in width than they grow in depth. One explanation for their conformation is because the most active environment for weathering is the zone of alternate wetting and drying along the margins of the pools that collect in the pits, the margins tend to deepen and enlarge until all points of the bottom are equally wet or dry at the same time, thus producing their characteristic shape. Panholes can expand from weathering and erosion but the main activity of how panholes expand is from biological weathering. At one time the belief was that the only agents involved with the expansion of panholes were physical weathering. 161: 31: 193: 152:. Panholes do not contain predators like fish or aquatic insects. The biofilm breaks down some of the siliceous minerals in the panhole for nutrients resulting in furthering the weathering the panhole. The organisms that live in the panholes have to tolerate rapid change in water temperature, pH, oxygen, carbon dioxide concentration, and ion concentration. 88:
is typically used for a smooth, bowl-shaped or cylindrical hollow, generally deeper than wide, found developed in the rocky bed of a stream. This type of feature is created by the grinding action either of a stone or stones or of coarse sediment whirled around and kept in motion by eddies or the
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Panholes are erosional or destructional features that are developed in a variety of climatic environments and in a wide range of rock types. These shallow basins, or closed depressions, are quite commonly well developed in surfaces of
110:. Diameters are rarely greater than 6 ft (1.8 m). Some panholes were at one time thought to be man-made because their roundness was so perfect they were argued not be natural and must have been shaped by humans. 447: 137:. Panholes range in size from a few centimeters to many meters in diameter. The cavities can be shallow or more than 15 meters (49 ft) deep, containing hundreds of liters of water. The 129:, and Moab. Panholes are capable of collecting water when it rains, freezing over when the weather gets cold, dry out in hotter weather, and can even contain some species of bacteria, 145:, in particular, implies a depression capable of holding water in arid areas, forming an important water resource for Aboriginal people that needed to be carefully maintained. 160: 520:
Clyde Warhaftig, attributed on page p. 63 in Huber, N. King. 1989. The geological story of Yosemite National Park. U.S. Geological Survey Bulletin 1595.
106:. They are generally characterized by flat bottoms and sometimes by overhanging sides. The initial form may be a closed hollow created by a patch of 224:
to describe a naturally formed rock hole as well as its retained rainwater. The term "gnamma hole" is also widely used, but is incorrect, being a
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Bacterial Communities and their Influence on the Formation and Development of Potholes in Sandstone Surfaces of the Semi-Arid Colorado Plateau
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Géomorphologie: Relief, Processus, Environnement, Articles sous presse, Varia, mis en ligne le 08 janvier 2018, consulté le 01 juillet 2018.
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Within the panholes is a varied eco-system that contains bacteria such as cyanobacteria, fungi, and algae which can be referred to as
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Matthes, Francois E. 1930. Geologic History of the Yosemite Valley. U.S. Geological Survey Professional Paper 160
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is a depression or basin eroded into flat or gently sloping cohesive rock. Similar terms for this feature are
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Huber, N. King. 1989. The geological story of Yosemite National Park. U.S. Geological Survey Bulletin 1595.
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In Australia, the terms "gnamma" and "rock hole" (or "rockhole") are used. Gnamma is an anglicization of a
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University of Western Ontario - Electronic Thesis and Dissertation Repository. Paper 543.
459: 317: 285: 560: 267: 169: 81: 80:, which is a term typically used for similarly shaped riverine landforms. In fluvial 165: 192: 103: 370:"SA students take to the bush to connect with land and Indigenous culture" 121:. A few well-known panholes are found developed in sandstone surfaces in 99: 427:(5th ed.). Alexandria, Virginia, American Geological Institute. 800 pp. 17: 149: 35: 130: 114: 27:
Depression or basin eroded into flat or gently sloping cohesive rock
491:"What are “Potholes” and how are organisms able to live in them?." 191: 159: 107: 29: 423:
Neuendorf, K.K.E., J.P. Mehl, Jr., and J.A. Jackson, eds., 2011.
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In the Sierra Nevada, California these features were termed
532:"Geomorphology of pit gnammas in southwestern Australia" 472:
Geomorphology of pit gnammas in southwestern Australia
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Utah Geological Survey. N.p., n.d. Web. 9 Oct 2013.
539:Journal of the Royal Society of Western Australia 475:Journal of the Royal Society of Western Australia 404: 402: 400: 398: 396: 394: 89:force of the stream current in a given spot. 8: 485: 483: 34:Panholes on a granite surface near Corscia, 442: 440: 363: 361: 316:Twidale, C.R., and Bourne, J.A., 2018. 304: 76:Some authors refer to panholes also as 477:, 96: 7–16 Retrieved 2 November 2020. 332: 330: 328: 7: 270:, Yosemite National Park, California 172:, Yosemite National Park, California 113:Panholes are most commonly found in 378:Australian Broadcasting Corporation 460:10.1016/B978-0-12-374739-6.00068-3 368:Jonscher, Samantha (3 June 2018). 25: 319:Rock basins (gnammas) revisited. 292:Stone Mountain (North Carolina) 1: 448:Tafoni and Other Rock Basins 588: 127:Capitol Reef National Park 452:Treatise on Geomorphology 343:Western Australian Museum 262:Canyonlands National Park 123:Canyonlands National Park 408:Hughes, Kebbi A., 2012. 280:Shenandoah National Park 274:Navajo National Monument 446:Paradise, T. R., 2013 ' 243:Hiltaba Nature Reserve 204: 198:Hiltaba Nature Reserve 173: 38: 572:Depressions (geology) 530:Timms, B. V. (2013). 195: 163: 139:Australian Aboriginal 33: 470:Timms, B.V., 2013. 425:Glossary of Geology 256:Forbes State Forest 216:word, used by that 182:François E. Matthes 115:desert environments 489:Davis, Jim, 2013. 205: 174: 39: 222:Western Australia 214:Nyoongar language 16:(Redirected from 579: 551: 550: 548: 546: 536: 527: 521: 518: 512: 509: 503: 500: 494: 487: 478: 468: 462: 444: 435: 421: 415: 406: 389: 388: 386: 384: 365: 356: 355: 353: 351: 334: 323: 314: 294:, North Carolina 135:blue-green algae 119:Colorado Plateau 55:armchair hollows 21: 587: 586: 582: 581: 580: 578: 577: 576: 557: 556: 555: 554: 544: 542: 534: 529: 528: 524: 519: 515: 510: 506: 501: 497: 488: 481: 469: 465: 454:, V.4, 111-126 445: 438: 422: 418: 407: 392: 382: 380: 367: 366: 359: 349: 347: 336: 335: 326: 315: 306: 301: 251: 239: 234: 210: 202:South Australia 190: 178:weathering pits 158: 95: 59:weathering pans 28: 23: 22: 15: 12: 11: 5: 585: 583: 575: 574: 569: 559: 558: 553: 552: 522: 513: 504: 495: 479: 463: 436: 416: 390: 357: 338:"Gnamma Holes" 324: 303: 302: 300: 297: 296: 295: 289: 286:Stone Mountain 283: 277: 271: 265: 259: 258:, Pennsylvania 250: 247: 246: 245: 238: 235: 233: 230: 209: 206: 189: 186: 157: 154: 133:, mosses, and 94: 91: 26: 24: 14: 13: 10: 9: 6: 4: 3: 2: 584: 573: 570: 568: 565: 564: 562: 540: 533: 526: 523: 517: 514: 508: 505: 499: 496: 492: 486: 484: 480: 476: 473: 467: 464: 461: 457: 453: 449: 443: 441: 437: 434: 433:0-922152-89-6 430: 426: 420: 417: 413: 412: 405: 403: 401: 399: 397: 395: 391: 379: 375: 371: 364: 362: 358: 345: 344: 339: 333: 331: 329: 325: 321: 320: 313: 311: 309: 305: 298: 293: 290: 287: 284: 281: 278: 275: 272: 269: 268:Glacier Point 266: 263: 260: 257: 253: 252: 249:United States 248: 244: 241: 240: 236: 231: 229: 227: 223: 219: 215: 207: 203: 199: 196:Rock hole in 194: 187: 185: 183: 179: 171: 170:Glacier Point 167: 162: 155: 153: 151: 146: 144: 140: 136: 132: 128: 124: 120: 116: 111: 109: 105: 101: 92: 90: 87: 83: 82:geomorphology 79: 74: 72: 68: 67:solution pans 64: 60: 56: 53:(Australia), 52: 48: 44: 37: 32: 19: 543:. Retrieved 538: 525: 516: 507: 498: 474: 466: 451: 424: 419: 410: 381:. Retrieved 373: 348:. Retrieved 341: 318: 254:Beam Rocks, 211: 177: 175: 166:granodiorite 164:Panholes in 147: 142: 117:such as the 112: 96: 85: 75: 70: 66: 62: 58: 54: 50: 46: 42: 40: 188:Terminology 93:Description 84:, the term 561:Categories 350:5 November 299:References 282:, Virginia 220:people of 218:Aboriginal 102:rocks and 51:rock holes 567:Landforms 545:9 January 383:9 January 288:, Georgia 276:, Arizona 237:Australia 232:Locations 226:tautology 208:Australia 104:sandstone 374:ABC News 100:granitic 78:potholes 18:Rockhole 541:(96): 7 150:biofilm 131:lichens 86:pothole 43:panhole 36:Corsica 431:  346:. 2017 264:, Utah 156:Origin 143:gnamma 65:) and 47:gnamma 535:(PDF) 450:' in 141:term 108:humus 547:2022 429:ISBN 385:2022 352:2021 71:pits 69:(or 63:pits 61:(or 456:doi 180:by 168:at 73:). 49:or 563:: 537:. 482:^ 439:^ 393:^ 376:. 372:. 360:^ 340:. 327:^ 307:^ 228:. 200:, 125:, 57:, 41:A 549:. 458:: 387:. 354:. 20:)

Index

Rockhole

Corsica
potholes
geomorphology
granitic
sandstone
humus
desert environments
Colorado Plateau
Canyonlands National Park
Capitol Reef National Park
lichens
blue-green algae
Australian Aboriginal
biofilm

granodiorite
Glacier Point
François E. Matthes

Hiltaba Nature Reserve
South Australia
Nyoongar language
Aboriginal
Western Australia
tautology
Hiltaba Nature Reserve
Forbes State Forest
Canyonlands National Park

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