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Cave survey

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other. A diver's digital wristwatch with a depth gauge function is submerged in the box. If the rubber glove is placed on one station and the box with the depth gauge is placed on a lower one, then the hydrostatic pressure between the two points depends only on the difference in heights and the density of the water, i.e. the route of the tube does not affect the pressure in the box. Reading the depth gauge gives the apparent depth change between the higher and lower station. Depth changes are 'apparent' because depth gauges are calibrated for sea water, and the hydrolevel is filled with fresh water. Therefore, a coefficient must be determined to convert apparent depth changes to true depth changes. Adding the readings for consecutive pairs of stations gives the total depth of the cave.
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in August 2011, as were the Paisley Caves Archaeological dig site in SE Oregon. Both were scanned with a FARO Focus Phase shift scanner with +/-2mm accuracy. The Oregon Caves were scanned from the main public entrance to the 110 exit and were loop surveyed to the point of beginning. The data is not yet available for public use, but copies are retained by both the US Park Service and i-TEN Associates in Portland, Oregon.
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used, attached to a strip of wood, and the tube is filled with water and the depth at each end marked. In Russia, measuring the depth of caves by hydrolevelling began in the 1970s, and was considered to be the most accurate means of measuring depth despite the difficulties in using the cumbersome equipment of the time. Interest in the method has been revived following the discovery of
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Terrestrial LiDAR units are increasing significantly in accuracy and decreasing in price. Several Caves have been "scanned" using both "time of flight" and "phase shift" LiDAR units. The differences are in the relative accuracies available to each. The Oregon Caves National Park, was LiDAR scanned
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have started to change the process, leading to the advent of fully paperless surveying around 2007. The main variation on the normal methodology detailed below have been devices such as LIDAR and SONAR surveyors that produce a point cloud rather than a series of linked stations. Video-based surveying
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The use of a low-frequency cave radio can also verify survey accuracy. A receiving unit on the surface can pinpoint the depth and location of a transmitter in a cave passage by measurement of the geometry of its radio waves. A survey over the surface from the receiver back to the cave entrance forms
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was the first person to describe surveying techniques. His surveys were made by having an assistant walk down the passage until they were almost out of sight. Martel would then take a compass bearing to the assistant's light, and measure the distance by pacing up to the assistant. This would equate
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The hydrolevel device used in recent Voronja expeditions comprises a 50-metre (160 ft) transparent tube filled with water, which is coiled or placed on a reel. A rubber glove which acts as a reservoir is placed on one end of the tube, and a metal box with a transparent window is placed on the
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Hydrolevelling is an alternative to measuring depth with clinometer and tape that has a long history of use in Russia. The technique is regularly used in building construction for finding two points with the same height, as in levelling a floor. In the simplest case, a tube with both ends open is
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There are a large number of surveying packages available on various computer platforms, most of which have been developed by cavers with a basis in computer programming. Many of the packages perform particularly well for specific tasks, and as such many cave surveyors will not solely choose one
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to the previous station in the opposite direction. A back-sight compass reading that is different by 180 degrees and a clinometer reading that is the same value but with the reverse direction (positive rather than negative, for example) indicates that the original measurement was accurate.
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A Grade 6 survey requires the compass to be used at the limit of possible accuracy, i.e. accurate to ±0.5 Â°; clinometer readings must be to the same accuracy. Station position error must be less than ±2.5 cm, which will require the use of tripods at all stations or other fixed station
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Coincident with recording straight-line data, details of passage dimensions, shape, gradual or sudden changes in elevation, the presence or absence of still or flowing water, the location of notable features and the material on the floor are recorded, often by means of a sketch map.
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measurements between stations. The stations are temporary fixed locations chosen chiefly for their ease of access and clear sight along the cave passage. In some cases, survey stations may be permanently marked to create a fixed reference point to which to return at a later date.
740:"HORTA unit for determining the geographic position underground. HORTA-Honeywell Ore Retrieval and Tunneling Aid-is a box containing a gyro and an accelerometer, originally developed for the U.S. military, that solves the problem of positioning and location underground." 105:. It consists of an elevational section of the cave. Numerous other surveys of caves were made in the following years, though most are sketches and are limited in accuracy. The first cave that is likely to have been accurately surveyed with instruments is the 380:
Grade X is only potentially more accurate than Grade 6. It should never be forgotten that the theodolite/Total Station is a complex precision instrument that requires considerable training and regular practice if serious errors are not to be made through its
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Despite these advances, faulty instruments, imprecise measurements, recording errors or other factors may still result in an inaccurate survey, and these errors are often difficult to detect. Some cave surveyors measure each station twice, recording a
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have full centerline and map editing capabilities. Therion notably, when it closes survey loops, warps the passages to fit over their length, meaning that entire passages do not have to be redrawn. Unlike Therion's 2D warping capabilities,
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methodology, but most are based on a similar set of steps which haven't changed fundamentally in 250 years, although the instruments (compass and tape) have become smaller and more accurate. Since the late 1990s, digital instruments such as
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The equipment used to undertake a cave survey continues to improve. The use of computers, inertia systems, and electronic distance finders has been proposed, but few practical underground applications have evolved at present.
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warps passages in 3D. This includes warping plan and profile sketches. CaveWhere also supports loop closure (using Survex) and provides a user friendly interface for entering and visualizing cave survey data.
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Caving organisations, etc., are encouraged to reproduce Table 1 and Table 2 in their own publications; permission is not required from BCRA to do so, but the tables must not be reprinted without these notes.
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A Grade X survey must include on the drawing notes descriptions of the instruments and techniques used, together with an estimate of the probable accuracy of the survey compared with Grade 3, 5 or 6 surveys.
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Grades 2 and 4 are for use only when, at some stage of the survey, physical conditions have prevented the survey from attaining all the requirements for the next higher grade and it is not practical to
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A Magnetic survey. Horizontal and vertical angles measured to ±1 Â°; distances should be observed and recorded to the nearest centimetre and station positions identified to less than 10 cm.
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To attain Grade 5 it is essential for instruments to be properly calibrated, and all measurements must be taken from a point within a 10 cm diameter sphere centred on the survey station.
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In the past, cavers were reluctant to redraw complex cave maps after detecting survey errors. Today, computer cartography can automatically redraw cave maps after data has been corrected.
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When a loop within a cave is surveyed back to its starting point, the resulting line-plot should also form a closed loop. Any gap between the first and last stations is called a
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Traditionally, cave surveys are produced in two-dimensional form due to the confines of print, but given the three-dimensional environment inside a cave, modern techniques using
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The above table is a summary, omitting some technical details and definitions; the definitions of the survey grades given above must be read in conjunction with these notes.
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A rough magnetic survey. Horizontal & vertical angles measured to ±2.5 Â°; distances measured to ±50 cm; station position error less than 50 cm.
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system, which may be produced to meet differing standards of accuracy depending on the cave conditions and equipment available underground. Cave surveying and
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Such automated methods have provided a more than fifty-fold increase in underground surveying productivity with more accurate and finer detail maps as well.
106: 43:, i.e. the creation of an accurate, detailed map, is one of the most common technical activities undertaken within a cave and is a fundamental part of 322:
May be used, if necessary, to describe a survey that fails to attain all the requirements of Grade 5 but is more accurate than a Grade 3 survey.
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The cartographer then draws details around the line-plot, using the additional data of passage dimensions, water flow and floor/wall
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The first known plan of a cave dates from 1546, and was of a man-made cavern in tufa called the Stufe di Nerone (Nero's Oven) in
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In drawing up, the survey co-ordinates must be calculated and not hand-drawn with scale rule and protractor to obtain Grade 5.
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recorded at the time, to produce a completed cave survey. Cave surveys drawn on paper are often presented in two-dimensional
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Measurements of detail made at survey stations and wherever else needed to show significant changes in passage dimensions.
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views, while computer surveys may simulate three dimensions. Although primarily designed to be functional, some
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in 1964. The software was programmed onto a large university mainframe computer and a paper plot was produced.
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May be used, if necessary, to describe a sketch that is intermediate in accuracy between Grade 1 & 3
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A survey team begins at a fixed point (such as the cave entrance) and measures a series of consecutive
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an artificial loop with the underground survey, whose loop-closure error can then be determined.
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In all cases it is necessary to follow the spirit of the definition and not just the letter.
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To attain Grade 3 it is necessary to use a clinometer in passages having appreciable slope.
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The first cave to have its centreline calculated by a computer is the Fergus River Cave in
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analyzes the recorded data, converting them into two-dimensional measurements by way of
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Nicholson, F.H.; Patmore, D.J. (1965). "The Fergus River Cave, Co. Clare, Ireland".
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Normally only one of the following combinations of survey grades should be used:
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are increasingly used to allow a more realistic representation of a cave system.
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The accuracy of the detail should be similar to the accuracy of the line.
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In recent years an underground geographic positioning technology called
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optionally, distance to surrounding walls â€“ left, right, up, down (
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Degtjarev, Alexander; Snetkov, Eugene; Gurjanov, Alexey (July 2007).
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A magnetic survey that is more accurate than grade 5, (see note 5).
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or total station instead of a compass, (see notes 6 and 10 below).
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Another early survey dates from before 1680, and was made by
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Sketch of low accuracy where no measurements have been made
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A popular program for producing a centerline survey is
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in Italy. The first natural cave to be mapped was the
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The measurements taken between the stations include:
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Measurements of detail made at survey stations only.
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Passage details estimated and recorded in the cave.
267: â€“ currently the world's second deepest cave. 645:"Obtaining accurate cave depths by hydrolevelling" 487:product over another for all cartographic tasks. 340:A survey that is based primarily on the use of a 1295: 620: 287:in the 1960s, which uses a scale of six grades. 389:BCRA gradings for recording cave passage detail 181:inclination from horizontal (dip) taken with a 787: 187:distance measured with a low-stretch tape or 319:Grade 4 (use only if necessary, see note 7) 307:Grade 2 (use only if necessary, see note 7) 794: 780: 768:, A collection of Surveys of British Caves 706: 676: 598:An Encyclopedia of Caves and Karst Science 727: 725: 716:16th International Congress of Speleology 700: 449: 218:calculations. From them he/she creates a 506:. Other programmes such as 'Tunnel' and 94:, of which a sketch from 1656 survives. 65: 18: 1296: 722: 290: 246:consider cave surveys as an art form. 205: 125:, which was plotted by members of the 775: 755:Laser Scanning History: Paisley Caves 481: 118:to a modern-day BCRA Grade 2 survey. 709:"Quick 3D Cave maps using Cavewhere" 595: 567: â€“ Diving in water-filled caves 523: 397:All passage details based on memory. 296:BCRA gradings for a cave line survey 738:, April 2000, accessed 2010-12-02. 16:Map of all or part of a cave system 13: 14: 1325: 813:Glossary of caving and speleology 748: 688:British Cave Research Association 285:British Cave Research Association 249: 1202:Nok and Mamproug Cave Dwellings 801: 147:also exists in prototype form. 74:by the Yorkshire Ramblers' Club 614: 589: 132: 1: 582: 225: 137:There are many variations to 1255:List of UK caving fatalities 150: 7: 707:Schuchardt, Philip (2013). 558: 274: 10: 1330: 538:inertial navigation system 419: 61: 1278: 1247: 1215: 1174: 1059: 904: 819: 810: 658:Cave Survey Group: 8–12. 552:-position determination. 532:has been utilized in the 1231:Cave of Forgotten Dreams 348: 1224:Diving into the Unknown 736:Canadian Mining Journal 684:"BCRA Surveying Grades" 1270:Tham Luang cave rescue 1265:Riesending cave rescue 540:technology utilizes a 450:Survey error detection 367:markers ("roofhooks"). 75: 24: 1238:The Underground Eiger 577:List of longest caves 115:Édouard-Alfred Martel 69: 56:computer aided design 22: 766:CaveMaps.org Surveys 101:of Long Hole in the 35:of all or part of a 1260:Alpazat cave rescue 905:Types and formation 291:BCRA grading system 206:Drawing a line-plot 1187:Cave-dwelling Jews 934:Estavelle/Inversac 732:Inco's Innovations 482:Surveying software 469:loop-closure error 107:Grotte de Miremont 76: 25: 1291: 1290: 1069:(Cave formations) 832:Cave conservation 607:978-1-57958-399-6 596:Gunn, J. (2003). 524:Automated methods 500:Adobe Illustrator 279:The accuracy, or 189:laser rangefinder 72:Marble Arch Caves 1321: 914:Anchihaline cave 896:Caves by country 796: 789: 782: 773: 772: 742: 729: 720: 719: 713: 704: 698: 697: 695: 694: 680: 674: 673: 671: 670: 649: 640: 631: 630: 623:UBSS Proceedings 618: 612: 611: 593: 443:XA, XB, XC or XD 1329: 1328: 1324: 1323: 1322: 1320: 1319: 1318: 1294: 1293: 1292: 1287: 1274: 1243: 1216:Popular culture 1211: 1170: 1068: 1063: 1055: 1001:Solutional cave 906: 900: 815: 806: 800: 751: 746: 745: 730: 723: 711: 705: 701: 692: 690: 682: 681: 677: 668: 666: 647: 641: 634: 619: 615: 608: 594: 590: 585: 561: 536:industry. The 526: 484: 452: 422: 391: 351: 298: 293: 277: 252: 228: 208: 175:) taken with a 153: 135: 70:1908 survey of 64: 17: 12: 11: 5: 1327: 1317: 1316: 1311: 1306: 1304:Cave surveying 1289: 1288: 1286: 1285: 1279: 1276: 1275: 1273: 1272: 1267: 1262: 1257: 1251: 1249: 1245: 1244: 1242: 1241: 1234: 1227: 1219: 1217: 1213: 1212: 1210: 1209: 1204: 1199: 1194: 1192:Cave monastery 1189: 1184: 1178: 1176: 1172: 1171: 1169: 1168: 1163: 1158: 1153: 1148: 1146:Speleoseismite 1143: 1138: 1133: 1128: 1123: 1118: 1113: 1108: 1103: 1098: 1093: 1088: 1083: 1078: 1072: 1070: 1057: 1056: 1054: 1053: 1052: 1051: 1046: 1041: 1033: 1028: 1023: 1018: 1013: 1008: 1003: 998: 993: 988: 983: 978: 977: 976: 966: 961: 956: 951: 946: 941: 936: 931: 926: 921: 919:Breathing cave 916: 910: 908: 902: 901: 899: 898: 893: 888: 883: 878: 877: 876: 871: 861: 860: 859: 854: 844: 839: 834: 829: 823: 821: 817: 816: 811: 808: 807: 799: 798: 791: 784: 776: 770: 769: 763: 760:Compass Points 757: 750: 749:External links 747: 744: 743: 721: 699: 675: 652:Compass Points 632: 613: 606: 587: 586: 584: 581: 580: 579: 574: 568: 560: 557: 525: 522: 483: 480: 451: 448: 447: 446: 445: 444: 441: 438: 435: 432: 426: 421: 418: 417: 416: 413: 410: 407: 404: 401: 398: 395: 390: 387: 386: 385: 382: 378: 375: 371: 368: 364: 361: 358: 355: 350: 347: 346: 345: 338: 335: 332: 329: 326: 323: 320: 317: 314: 311: 308: 305: 302: 297: 294: 292: 289: 276: 273: 261:Arabica Massif 251: 250:Hydrolevelling 248: 227: 224: 207: 204: 199: 198: 191: 185: 179: 152: 149: 134: 131: 63: 60: 15: 9: 6: 4: 3: 2: 1326: 1315: 1312: 1310: 1307: 1305: 1302: 1301: 1299: 1284: 1281: 1280: 1277: 1271: 1268: 1266: 1263: 1261: 1258: 1256: 1253: 1252: 1250: 1246: 1240: 1239: 1235: 1233: 1232: 1228: 1226: 1225: 1221: 1220: 1218: 1214: 1208: 1205: 1203: 1200: 1198: 1195: 1193: 1190: 1188: 1185: 1183: 1180: 1179: 1177: 1173: 1167: 1164: 1162: 1159: 1157: 1154: 1152: 1149: 1147: 1144: 1142: 1139: 1137: 1134: 1132: 1129: 1127: 1124: 1122: 1119: 1117: 1114: 1112: 1109: 1107: 1104: 1102: 1101:Dogtooth spar 1099: 1097: 1094: 1092: 1089: 1087: 1086:Calcite rafts 1084: 1082: 1079: 1077: 1074: 1073: 1071: 1067: 1062: 1058: 1050: 1047: 1045: 1042: 1040: 1037: 1036: 1034: 1032: 1029: 1027: 1024: 1022: 1019: 1017: 1014: 1012: 1009: 1007: 1004: 1002: 999: 997: 994: 992: 989: 987: 984: 982: 979: 975: 972: 971: 970: 967: 965: 962: 960: 957: 955: 952: 950: 947: 945: 942: 940: 937: 935: 932: 930: 927: 925: 922: 920: 917: 915: 912: 911: 909: 903: 897: 894: 892: 889: 887: 886:Speleogenesis 884: 882: 879: 875: 872: 870: 867: 866: 865: 862: 858: 855: 853: 850: 849: 848: 845: 843: 840: 838: 837:Cave painting 835: 833: 830: 828: 827:Biospeleology 825: 824: 822: 818: 814: 809: 804: 797: 792: 790: 785: 783: 778: 777: 774: 767: 764: 761: 758: 756: 753: 752: 741: 737: 733: 728: 726: 717: 710: 703: 689: 685: 679: 665: 661: 657: 653: 646: 639: 637: 628: 624: 617: 609: 603: 600:. Routledge. 599: 592: 588: 578: 575: 572: 569: 566: 563: 562: 556: 553: 551: 547: 546:accelerometer 543: 539: 535: 531: 521: 517: 514: 509: 505: 501: 497: 493: 488: 479: 476: 472: 470: 465: 462: 456: 442: 439: 436: 433: 430: 429: 427: 424: 423: 414: 411: 408: 405: 402: 399: 396: 393: 392: 383: 379: 376: 372: 369: 365: 362: 359: 356: 353: 352: 343: 339: 336: 333: 330: 327: 324: 321: 318: 315: 312: 309: 306: 303: 300: 299: 288: 286: 282: 272: 268: 266: 262: 258: 247: 245: 241: 237: 233: 223: 221: 217: 213: 203: 196: 192: 190: 186: 184: 180: 178: 174: 170: 166: 165: 164: 161: 158: 157:line-of-sight 148: 145: 140: 130: 128: 124: 119: 116: 112: 108: 104: 103:Cheddar Gorge 100: 95: 93: 89: 88:Baumannshöhle 85: 81: 73: 68: 59: 57: 52: 50: 49:speleogenesis 46: 42: 38: 34: 30: 23:A cave survey 21: 1236: 1229: 1222: 1182:Cave dweller 1096:Cave popcorn 1035:Underground 954:Karst spring 944:Glacier cave 841: 739: 735: 715: 702: 691:. Retrieved 678: 667:. Retrieved 651: 626: 622: 616: 597: 591: 554: 527: 518: 489: 485: 477: 473: 468: 466: 460: 457: 453: 280: 278: 269: 253: 239: 235: 229: 219: 212:cartographer 209: 200: 194: 162: 154: 136: 120: 96: 77: 53: 28: 26: 1061:Speleothems 974:Exploration 874:Troglofauna 842:Cave survey 820:Main topics 565:Cave diving 216:geometrical 210:Later, the 167:direction ( 144:distometers 133:Methodology 99:John Aubrey 41:cartography 29:cave survey 1298:Categories 1197:Kome Caves 1161:Stalagnate 1156:Stalagmite 1151:Stalactite 1141:Soda straw 1131:Shelfstone 1091:Cave pearl 1066:Speleogens 1031:Talus cave 964:Ley tunnel 891:Speleology 869:Stygofauna 693:2009-05-02 669:2009-05-02 583:References 548:to aid in 461:back-sight 374:re-survey. 342:theodolite 232:topography 226:Finalising 183:clinometer 45:speleology 1314:Map types 1309:Surveying 1248:Incidents 1175:Dwellings 1116:Helictite 1111:Frostwork 1106:Flowstone 1076:Anthodite 1049:Waterfall 1021:Suffosion 1006:Show cave 991:Salt cave 959:Lava cave 907:processes 857:Equipment 664:1361-8962 629:(3): 285. 542:gyroscope 513:CaveWhere 220:line-plot 151:Surveying 139:surveying 1283:Category 1136:Snottite 1126:Rimstone 1121:Moonmilk 1011:Sinkhole 996:Sea cave 981:Pit cave 949:Ice cave 559:See also 504:Inkscape 437:5C or 5D 434:3B or 3C 275:Accuracy 265:Caucasus 80:Pozzuoli 1207:Yaodong 1081:Boxwork 924:Cave-in 544:and an 508:Therion 496:AutoCAD 412:Class D 406:Class C 400:Class B 394:Class A 337:Grade X 331:Grade 6 325:Grade 5 313:Grade 3 301:Grade 1 263:in the 259:on the 257:Voronja 240:profile 238:and/or 177:compass 173:bearing 169:azimuth 123:Ireland 92:Germany 62:History 1016:Spring 929:Cenote 852:Diving 847:Caving 805:topics 662:  654:(38). 604:  571:Caving 534:mining 492:Survex 244:cavers 111:France 84:Naples 1044:River 986:Ponor 939:Foiba 881:Karst 864:Fauna 712:(PDF) 648:(PDF) 530:HORTA 420:Notes 349:Notes 281:grade 82:near 31:is a 1064:and 1039:Lake 1026:Sump 969:Mine 803:Cave 660:ISSN 656:BCRA 602:ISBN 502:and 381:use! 236:plan 195:LRUD 127:UBSS 37:cave 1166:Vug 171:or 109:in 90:in 33:map 1300:: 734:, 724:^ 714:. 686:. 650:. 635:^ 627:10 625:. 550:3D 498:, 440:6D 431:1A 27:A 795:e 788:t 781:v 718:. 696:. 672:. 610:. 197:)

Index


map
cave
cartography
speleology
speleogenesis
computer aided design
Hand-drawn map of a cave, showing meandering underground river passage as well as surface topography including large shakeholes.
Marble Arch Caves
Pozzuoli
Naples
Baumannshöhle
Germany
John Aubrey
Cheddar Gorge
Grotte de Miremont
France
Édouard-Alfred Martel
Ireland
UBSS
surveying
distometers
line-of-sight
azimuth
bearing
compass
clinometer
laser rangefinder
cartographer
geometrical

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