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Sump (cave)

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122: 25: 201:. Pumping the water away requires the inward flow of water into the sump to be less than the rate at which the pump empties it, as well as a suitable place to collect the emptied water. Upstream sumps have been successfully emptied using hoses to siphon water out of them, such as at the 141:, is a passage in a cave that is submerged under water. A sump may be static, with no inward or outward flow, or active, with continuous through-flow. Static sumps may also be connected underwater to active stream passage. When short in length, a sump may be called a 181:). This is known as "free diving" and can only be attempted if the sump is known to be short and not technically difficult (e.g. constricted or requiring navigation). Longer and more technically difficult sumps can only be passed by 210: 177:
Short sumps may be passed simply by holding one's breath while ducking through the submerged section (for example, Sump 1 in
164:– sumps and ducks may fluctuate in water level and depth (and sometimes in length, due to the shape of adjacent passage). 89: 61: 341: 269: 108: 730: 322: 68: 46: 209:, and the emptied sumps revealed virgin passage behind them. During a rescue from beyond a downstream sump at 783: 75: 42: 125:
Sumps often block access to "dry" passage beyond them. Diagram B shows a "perched" sump, which could be
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done to the fragile cave environment usually rules out the use of such methods.
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Culver, David C.; Pipan, Tanja; White, William B., eds. (10 May 2019).
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When practical, a sump can also be drained using buckets, pumps or
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during exploration in 2005. The water was sent deeper into the
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constructed a few metres above the flooded passage.
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Unsourced material may be challenged and removed. 824: 257: 240: – Zone in an aquifer below the water table 224:or other forms of force to empty sumps, but the 16:Passage in a cave that is submerged under water 185:(as happened repeatedly in the exploration of 316: 323: 309: 213:in 2002, water was pumped upstream into a 167: 160:flow, or the relationship with the local 152:factors specific to a cave – such as the 109:Learn how and when to remove this message 120: 825: 304: 220:Some manuals also mention the use of 251: 47:adding citations to reliable sources 18: 13: 14: 849: 342:Glossary of caving and speleology 289: 23: 731:Nok and Mamproug Cave Dwellings 330: 34:needs additional citations for 1: 244: 784:List of UK caving fatalities 7: 231: 192: 10: 854: 807: 776: 744: 703: 588: 433: 348: 339: 172: 129:to lower the water level. 760:Cave of Forgotten Dreams 753:Diving into the Unknown 168:Exploration past a sump 799:Tham Luang cave rescue 794:Riesending cave rescue 130: 767:The Underground Eiger 261:Encyclopedia of Caves 124: 264:. Elsevier Science. 43:improve this article 789:Alpazat cave rescue 434:Types and formation 716:Cave-dwelling Jews 463:Estavelle/Inversac 131: 820: 819: 598:(Cave formations) 361:Cave conservation 226:ecological damage 119: 118: 111: 93: 845: 443:Anchihaline cave 425:Caves by country 325: 318: 311: 302: 301: 283: 282: 280: 278: 255: 203:Sinkhole Dersios 114: 107: 103: 100: 94: 92: 58:"Sump" cave 51: 27: 19: 853: 852: 848: 847: 846: 844: 843: 842: 823: 822: 821: 816: 803: 772: 745:Popular culture 740: 699: 597: 592: 584: 530:Solutional cave 435: 429: 344: 335: 329: 292: 287: 286: 276: 274: 272: 256: 252: 247: 234: 195: 175: 170: 115: 104: 98: 95: 52: 50: 40: 28: 17: 12: 11: 5: 851: 841: 840: 835: 818: 817: 815: 814: 808: 805: 804: 802: 801: 796: 791: 786: 780: 778: 774: 773: 771: 770: 763: 756: 748: 746: 742: 741: 739: 738: 733: 728: 723: 721:Cave monastery 718: 713: 707: 705: 701: 700: 698: 697: 692: 687: 682: 677: 675:Speleoseismite 672: 667: 662: 657: 652: 647: 642: 637: 632: 627: 622: 617: 612: 607: 601: 599: 586: 585: 583: 582: 581: 580: 575: 570: 562: 557: 552: 547: 542: 537: 532: 527: 522: 517: 512: 507: 506: 505: 495: 490: 485: 480: 475: 470: 465: 460: 455: 450: 448:Breathing cave 445: 439: 437: 431: 430: 428: 427: 422: 417: 412: 407: 406: 405: 400: 390: 389: 388: 383: 373: 368: 363: 358: 352: 350: 346: 345: 340: 337: 336: 328: 327: 320: 313: 305: 299: 298: 291: 290:External links 288: 285: 284: 270: 249: 248: 246: 243: 242: 241: 233: 230: 194: 191: 179:Swildon's Hole 174: 171: 169: 166: 117: 116: 31: 29: 22: 15: 9: 6: 4: 3: 2: 850: 839: 836: 834: 831: 830: 828: 813: 810: 809: 806: 800: 797: 795: 792: 790: 787: 785: 782: 781: 779: 775: 769: 768: 764: 762: 761: 757: 755: 754: 750: 749: 747: 743: 737: 734: 732: 729: 727: 724: 722: 719: 717: 714: 712: 709: 708: 706: 702: 696: 693: 691: 688: 686: 683: 681: 678: 676: 673: 671: 668: 666: 663: 661: 658: 656: 653: 651: 648: 646: 643: 641: 638: 636: 633: 631: 630:Dogtooth spar 628: 626: 623: 621: 618: 616: 615:Calcite rafts 613: 611: 608: 606: 603: 602: 600: 596: 591: 587: 579: 576: 574: 571: 569: 566: 565: 563: 561: 558: 556: 553: 551: 548: 546: 543: 541: 538: 536: 533: 531: 528: 526: 523: 521: 518: 516: 513: 511: 508: 504: 501: 500: 499: 496: 494: 491: 489: 486: 484: 481: 479: 476: 474: 471: 469: 466: 464: 461: 459: 456: 454: 451: 449: 446: 444: 441: 440: 438: 432: 426: 423: 421: 418: 416: 415:Speleogenesis 413: 411: 408: 404: 401: 399: 396: 395: 394: 391: 387: 384: 382: 379: 378: 377: 374: 372: 369: 367: 366:Cave painting 364: 362: 359: 357: 356:Biospeleology 354: 353: 351: 347: 343: 338: 333: 326: 321: 319: 314: 312: 307: 306: 303: 297: 294: 293: 273: 271:9780128141250 267: 263: 262: 254: 250: 239: 238:Phreatic zone 236: 235: 229: 227: 223: 218: 216: 212: 208: 204: 200: 190: 188: 184: 180: 165: 163: 159: 156:, changes in 155: 151: 148:Depending on 146: 144: 140: 136: 128: 123: 113: 110: 102: 91: 88: 84: 81: 77: 74: 70: 67: 63: 60: –  59: 55: 54:Find sources: 48: 44: 38: 37: 32:This article 30: 26: 21: 20: 765: 758: 751: 711:Cave dweller 625:Cave popcorn 564:Underground 554: 483:Karst spring 473:Glacier cave 275:. 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Two sectional diagrams illustrating the concept of a sump. Diagram "A" illustrates a U-shaped passage with water filling the rounded bottom section, blocking the dry passage either side. Diagram "B" shows a passage blocked similarly by a sump, but on one side the water level is being held back by a natural dam, with dry passage continuing beyond, below the water level of the sump.
siphoned
hydrological
sea tide
river
water table
Swildon's Hole
cave diving
Krubera Cave
siphons
Sinkhole Dersios
sinkhole
Sarkhos Cave
dam
explosives
ecological damage
Phreatic zone
Encyclopedia of Caves
ISBN

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