Knowledge (XXG)

Inner Terai Valleys of Nepal

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297:. During heavy rainfall forests absorb water. During floods, rivers overflow their banks and flood adjacent forests. Later the forests gradually release water back into the rivers. Deforestation reduces this buffering effect. It also accelerates soil erosion, causing downstream rivers to silt up and overflow their banks. The frequency and severity of flooding in the Gangetic plain and Bangladesh has steadily increased in recent years. 368: 100: 605: 421: 119: 357: 354: 196: 444:
The Deukhuri Valley is southeast of the Dang Valley and extends about 60 km (37 mi) in WNW-ESE direction with a maximum width of 20 km (12 mi). It forms a nearly 600 km (230 sq mi) plain within a drainage basin of 6,100 km (2,400 sq mi). The valley is
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The well-meaning malaria eradication campaign has had unexpected consequences by opening up the Terai region to human settlement. The Inner Terai valleys are home to a rich and diverse ecosystem. Since the early 1990s, however, the forests have been increasingly destroyed because of growing demands
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of central Nepal. The Chitwan Valley lies south-west of the Kathmandu valley and it has 600 square miles in area. After the re-structuring of the country in 2015, two districts of this valley, namely, Makwanpur and Chitwan lies in Bagmati Province and Nawalpur district lies in Gandaki Province. It
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in the late 1760s, the rulers granted large areas of fertiIe land and forest resources to members of the royal family, officials, priests and selected groups of the society. The beneficiaries of these grants had the right to collect revenues from cultivated land and forest products. They appointed
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in mid-western Nepal. The Dang Valley lies between the Mahabharat Range in the north and the Churia Range in the south. It forms a nearly 1,000 km (390 sq mi) plain within a local drainage basin of less than 3,000 km (1,200 sq mi). It is drained by the
468: 305:. However, these efforts may have mixed results. They contain floodwater in the short term, but may increase the problem in the longer term by reducing water velocity in the rivers downstream, and thus accelerating silting and reducing the drainage capacity of the rivers. 1285:. Kathmandu: International Centre for Integrated Mountain Development; Government of Nepal, Ministry of Environment, Science and Technology; United Nations Environment Programme, Regional Office for Asia and the Pacific. Archived from 407: 646: 643: 543: 281:, where seven colonies were developed for resettling about 7,000 people. They acquired property rights over uncultivated forest and waste land, thus accelerating the deforestation process in the Terai. 616:
in southeastern Nepal. It is about 30 km (19 mi) long and between 2 km (1.2 mi) and 4 km (2.5 mi) wide. It is drained by the Triyuga river flowing east to join the great
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Terrenato, L., Shrestha, S., Dixit, K.A., Luzzatto, L., Modiano, G., Morpurgo, G., Arese, P. (1988). "Decreased malaria morbidity in the Tharu people compared to sympatric populations in Nepal".
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Gautam, A. P., Shivakoti, G. P., & Webb, E. L. (2004). A review of forest policies, institutions, and changes in the resource condition in Nepal. International Forestry Review 6 (2): 136–148.
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was prevalent in this region until the late 1950s. Since its eradication, the area became a viable destination for large-scale migration of people from the hills who transformed the area from
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climate. The mean annual rainfall at the Rampur weatherstation in Chitwan was 2,214 mm (87.2 in) between 1995 and 2006. More than 80% of the total annual rainfall occurs during the
383:. The valley is about 700 m (2,300 ft) above sea level, forming an ellipse about 9 km (5.6 mi) east-west by 6 km (3.7 mi) north-south. It is drained by the 301:
of the Terai appears to be one of the major causes. The Indian and Nepalese governments are cooperating in measures including construction of barrages and dams in the Terai, such as the
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The major Inner Terai Valleys are listed from west to east. Click on the terrain and satellite imagery links to see vegetation, rivers, topography, roads and towns.
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Hasegawa S.; Dahal, R. K.; Yamanaka M.; Bhandary N. P.; Yatabe R.; Inagaki H. (2009). "Causes of large-scale landslides in the Lesser Himalaya of central Nepal".
1277: 620:. This valley lies between the Mahabharat Range to the north and the Sivalik Hills to the south, with an average elevation of about 430 m (1,410 ft). 140: 218:
In the past, the inner and outer Terai were a formidable barrier between Nepal and potential invaders from India because marshes and forests were infested by
555:, Nepal's first national park established in 1973, was declared a World Heritage site by UNESCO in 1984. It contains the largest and least disturbed natural 187:. They hold flat plains with winding rivers that shift their courses from time to time, running northwest or southeast along the axis of the Sivalik Hills. 1212:
Mugnier J. L., Leturmy P., Mascle G., Huyghe P., Chalaron E., Vidal G., Delcaillau B. (1999). "The Siwaliks of western Nepal: I. Geometry and kinematics".
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in Nepal. The reserve is mostly wetlands, subject to seasonal flooding, but also includes some grasslands and small patches of riverine forest. It is a
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season from June to September. Average temperatures ranged from 8.08 °C (46.54 °F) in January to 34.91 °C (94.84 °F) in June.
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An Overview of Floral Diversity in Wetlands of Terai Region of Nepal: M. Siwakoti, Natural History Museum, Tribhuvan University Swayambhu, Nepal
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Kimura, K. (1998). Geomorphic Development of the Deukhuri Dun, Nepal Sub-Himalaya. The science reports of the Tohoku University, 7th series.
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Regmi, R. R. (1994). Deforestation and Rural Society in the Nepalese Terai. Occasional Papers in Sociology and Anthropology 4: 72–89.
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The mouth of the valley opens onto a 175 km (109 mi) rectangle of land where the Triyuga meets the Koshi river above the
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Until the mid 18th century, the Terai was divided into several smaller kingdoms, and the forests were little disturbed. After the
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tax collectors who were also responsible for reclamation of land and establishment of settlements. In the late 1920s, the
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Department of Hydrology and Meteorology (2006). Climatological Records of Nepal (Several Volumes), Babarmahal, Kathmandu.
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people (or Danuwar), but there is a fast-growing population of migrants from the Nepali hills and from India.
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in the mid-1950s, people from the hills migrated to the Terai. Timber export continued to 1969. In 1970, the
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The Manjani System of the Danuwar State of the Kamala Valley: A Brief Study of an Egalitarian Judiciary
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for timber and agricultural land. This has led to concerns about the risk of losing many rare plants.
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is 150 km (93 mi) long and roughly 30–48 km (19–30 mi) wide. The cities of
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flowing from the Mahabharat Range near Hetauda, then west down the valley to join the bigger
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have been living in the Terai for many centuries, and reputedly had an innate resistance to
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Nepal Biodiversity Resource Book. Protected Areas, Ramsar Sites, and World Heritage Sites
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Sharmai, D. R. (1988). Archaeological Remains of the Dang Valley. Ancient Nepal 88: 8–15.
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Nagendra, H. (2002). "Tenure and forest conditions: community forestry in the Nepal
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in order to collect revenues. Cleared areas were subsequently used for agriculture.
852: 560: 250: 240: 1009: 726: 1319:"Notes on the mosquitoes of Nepal: II. New species records from 1991 collections" 1031:"Indian Ministry of Water Resources – Flood and centrally sponsored schemes (c)" 636: 617: 438: 395:. Tharu people from Dang settled in the valley since at least the 19th century. 392: 384: 118: 76: 787:
Gurung, H. (1988). "Nepal: Consequences of migration and policy implications".
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passes through the Deukhuri Valley. Both valleys are settled by Tharu people.
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rulers ordered the clearing of forests and extraction of timber for export to
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Nepal topography. The green/yellow zones hold the Inner Terai valleys.
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Geologic – Tectonic map of the Himalaya, modified after Le Fort (1988)
1062:"Causes, Effects and responses to flooding: The UK and Bangladesh" 603: 419: 366: 244: 204: 194: 98: 35: 1276:
Bhuju, U. R., Shakya, P. R., Basnet, T. B., Shrestha, S. (2007).
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comprise several elongated river valleys in the southern lowland
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Traditionally, the Kamala Valley was primarily inhabited by the
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Hydrological Analysis for Bheri-Babai Hydropower Project Nepal
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Darsie, R. F. Jr; Pradhan, S. P. & Vaidya, R. G. (1992).
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hill forest and associated communities. Its fauna comprises
490:, the biggest valley in Nepal, encompasses the districts of 265:
granted land to loyal ex-army personnel in the districts of
1174:"The Anthropology of the Tharus: An Annotated Bibliography" 1120:
Thapa L. B., Dhakal T. M., Chaudhary R., Thapa H. (2014).
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in 1976, and is home to the last remaining population of
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The valleys also mitigate the severity of floods on the
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The Kamala Valley, also called Udayapur Valley is in
1354:. Contributions to Nepalese Studies 22 (1): 43–55. 1167: 1165: 1163: 671:Gurung, H. (1971). "Landscape pattern of Nepal". 441:, and is one of the largest Inner Terai valleys. 424:Map of the settlements in Dang-Deukhuri District 83:are some of the largest Inner Terai Valleys. 8: 1302:: CS1 maint: multiple names: authors list ( 1246:: CS1 maint: multiple names: authors list ( 1152:: CS1 maint: multiple names: authors list ( 873:: CS1 maint: multiple names: authors list ( 841:Annals of Tropical Medicine and Parasitology 813: 811: 1271: 1269: 825: 823: 608:Sagarmatha zone: Udayapur district in green 147:. Unsourced material may be challenged and 1207: 1205: 1203: 1259: 1257: 1137: 167:Learn how and when to remove this message 64:. They are filled up with coarse to fine 519:are in the valley. It is drained by the 179:The Inner Terai valleys lie between the 663: 1295: 1239: 1145: 866: 391:. The district is the homeland of the 375:The Surkhet Valley is situated in the 257:. After malaria was eradicated using 222:that transmitted virulent strains of 7: 914:"Forests Monitor: The Terai Forests" 145:adding citations to reliable sources 727:"Terai-Duar savanna and grasslands" 724:Dinerstein, E., Loucks, C. (2001). 371:Map of the VDCs in Surkhet District 25: 1375:Terai-Duar savanna and grasslands 789:Contributions to Nepalese Studies 59:Terai-Duar savanna and grasslands 428:Both valleys are located in the 117: 1214:Journal of Asian Earth Sciences 853:10.1080/00034983.1988.11812202 57:These valleys are part of the 1: 1234:10.1016/s1367-9120(99)00038-3 629:Koshi Tappu Wildlife Reserve 531:situated within the valley. 42:valleys are enclosed by the 32:Inner Terai Valleys of Nepal 91:and grassland to farmland. 38:part of the country. These 1406: 692:Environmental Conservation 642:Imagery of Kamala valley: 106: 766:10.1007/s00254-008-1420-z 704:10.1017/S0376892902000383 416:Dang and Deukhuri Valleys 633:wild Asian water buffalo 627:. It was designated the 1329:: 23–28. Archived from 1172:Krauskopff, G. (1995). 569:great one-horned rhinos 109:Geology of the Himalaya 733:. World Wildlife Fund. 731:Terrestrial Ecoregions 609: 430:Dang Deukhuri District 425: 372: 200: 104: 27:River valleys in Nepal 1139:10.3126/on.v11i2.9645 1086:Yadav, S. K. (2002). 746:Environmental Geology 607: 553:Chitwan National Park 423: 387:, a tributary of the 370: 198: 102: 1323:Mosquito Systematics 285:Environmental issues 236:unification of Nepal 220:anopheline mosquitos 141:improve this section 1380:Grasslands of Nepal 1350:Khatry, P. (1995). 1226:1999JAESc..17..629M 1187:(3&4): 185–213. 758:2009EnGeo..57.1423H 321:Markers at valleys 46:foothills, viz the 610: 426: 373: 201: 105: 1390:Wetlands of Nepal 614:Udayapur district 459:Imagery of Dang ( 381:mid-western Nepal 177: 176: 169: 16:(Redirected from 1397: 1370:Valleys of Nepal 1355: 1348: 1342: 1341: 1339: 1338: 1314: 1308: 1307: 1301: 1293: 1291: 1284: 1273: 1264: 1261: 1252: 1251: 1245: 1237: 1209: 1198: 1195: 1189: 1188: 1178: 1169: 1158: 1157: 1151: 1143: 1141: 1117: 1111: 1110: 1108: 1107: 1101: 1094: 1083: 1077: 1076: 1074: 1073: 1064:. Archived from 1058: 1052: 1051: 1049: 1048: 1042: 1036:. Archived from 1035: 1027: 1021: 1020: 1018: 1017: 1008:. Archived from 1002: 996: 995: 993: 992: 983:. Archived from 977: 971: 966: 960: 959: 957: 956: 950: 944:. Archived from 943: 935: 929: 928: 926: 925: 916:. Archived from 910: 904: 903: 901: 900: 891:. Archived from 885: 879: 878: 872: 864: 836: 830: 827: 818: 815: 806: 803: 797: 796: 784: 778: 777: 752:(6): 1423–1434. 741: 735: 734: 722: 716: 715: 683: 677: 676: 673:Himalayan Review 668: 463:) and Deukhuri ( 454:Mahendra Highway 447:West Rapti River 377:Surkhet district 185:Mahabharat Range 172: 165: 161: 158: 152: 121: 113: 81:Deukhuri Valleys 48:Mahabharat Range 21: 1405: 1404: 1400: 1399: 1398: 1396: 1395: 1394: 1385:Plains of Nepal 1360: 1359: 1358: 1349: 1345: 1336: 1334: 1316: 1315: 1311: 1294: 1289: 1282: 1275: 1274: 1267: 1262: 1255: 1238: 1211: 1210: 1201: 1196: 1192: 1176: 1171: 1170: 1161: 1144: 1119: 1118: 1114: 1105: 1103: 1099: 1092: 1085: 1084: 1080: 1071: 1069: 1060: 1059: 1055: 1046: 1044: 1040: 1033: 1029: 1028: 1024: 1015: 1013: 1004: 1003: 999: 990: 988: 979: 978: 974: 967: 963: 954: 952: 948: 941: 937: 936: 932: 923: 921: 912: 911: 907: 898: 896: 887: 886: 882: 865: 838: 837: 833: 828: 821: 816: 809: 804: 800: 786: 785: 781: 743: 742: 738: 725: 723: 719: 685: 684: 680: 670: 669: 665: 661: 602: 597: 589:marsh crocodile 484: 479: 445:drained by the 418: 365: 319: 311: 295:Gangetic plains 287: 232: 193: 173: 162: 156: 153: 138: 122: 111: 97: 54:farther south. 28: 23: 22: 15: 12: 11: 5: 1403: 1401: 1393: 1392: 1387: 1382: 1377: 1372: 1362: 1361: 1357: 1356: 1343: 1309: 1292:on 2011-07-26. 1265: 1253: 1220:(5): 629–642. 1199: 1190: 1159: 1132:(2): 177–186. 1112: 1078: 1053: 1022: 997: 972: 961: 930: 905: 880: 831: 819: 807: 798: 779: 736: 717: 698:(4): 530–539. 678: 662: 660: 657: 601: 598: 596: 593: 581:monitor lizard 573:Asian elephant 565:Indian leopard 525:Narayani River 488:Chitwan Valley 483: 482:Chitwan Valley 480: 478: 475: 417: 414: 364: 363:Surkhet Valley 361: 318: 315: 310: 307: 286: 283: 231: 228: 192: 189: 175: 174: 125: 123: 116: 107:Main article: 96: 93: 73:Chitwan Valley 26: 24: 14: 13: 10: 9: 6: 4: 3: 2: 1402: 1391: 1388: 1386: 1383: 1381: 1378: 1376: 1373: 1371: 1368: 1367: 1365: 1353: 1347: 1344: 1333:on 2008-12-19 1332: 1328: 1324: 1320: 1313: 1310: 1305: 1299: 1288: 1281: 1280: 1272: 1270: 1266: 1260: 1258: 1254: 1249: 1243: 1235: 1231: 1227: 1223: 1219: 1215: 1208: 1206: 1204: 1200: 1194: 1191: 1186: 1182: 1175: 1168: 1166: 1164: 1160: 1155: 1149: 1140: 1135: 1131: 1127: 1123: 1116: 1113: 1102:on 2008-12-19 1098: 1091: 1090: 1082: 1079: 1068:on 2009-01-21 1067: 1063: 1057: 1054: 1043:on 2008-12-19 1039: 1032: 1026: 1023: 1012:on 1997-07-24 1011: 1007: 1001: 998: 987:on 2008-09-22 986: 982: 976: 973: 970: 965: 962: 951:on 2008-12-19 947: 940: 934: 931: 920:on 2017-06-29 919: 915: 909: 906: 895:on 2008-12-01 894: 890: 884: 881: 876: 870: 862: 858: 854: 850: 846: 842: 835: 832: 826: 824: 820: 814: 812: 808: 802: 799: 794: 790: 783: 780: 775: 771: 767: 763: 759: 755: 751: 747: 740: 737: 732: 728: 721: 718: 713: 709: 705: 701: 697: 693: 689: 682: 679: 674: 667: 664: 658: 656: 654: 649: 648: 645: 640: 638: 634: 630: 626: 625:Koshi Barrage 621: 619: 615: 606: 600:Kamala Valley 599: 595:Eastern Terai 594: 592: 590: 586: 582: 578: 574: 570: 566: 562: 558: 554: 549: 548: 545: 541: 537: 532: 530: 526: 522: 518: 514: 510: 506: 501: 497: 493: 489: 481: 477:Central Terai 476: 474: 473: 470: 466: 462: 457: 455: 450: 448: 442: 440: 435: 431: 422: 415: 413: 412: 409: 405: 401: 396: 394: 390: 386: 382: 378: 369: 362: 360: 359: 356: 352: 348: 344: 340: 336: 332: 328: 324: 317:Western Terai 316: 314: 308: 306: 304: 303:Koshi Barrage 300: 299:Deforestation 296: 291: 284: 282: 280: 276: 272: 268: 264: 260: 256: 252: 248: 246: 242: 237: 229: 227: 225: 221: 216: 214: 210: 207:has a humid, 206: 197: 190: 188: 186: 182: 181:Sivalik Hills 171: 168: 160: 157:December 2014 150: 146: 142: 136: 135: 131: 126:This section 124: 120: 115: 114: 110: 101: 94: 92: 90: 89:virgin forest 86: 82: 78: 74: 70: 67: 63: 60: 55: 53: 52:Sivalik Hills 49: 45: 41: 37: 33: 19: 1346: 1335:. 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Index

Inner Terai
Terai
tropical
Himalayan
Mahabharat Range
Sivalik Hills
Terai-Duar savanna and grasslands
ecoregion
alluvial
sediments
Chitwan Valley
Dang
Deukhuri Valleys
Malaria
virgin forest

Geology of the Himalaya

cite
sources
improve this section
adding citations to reliable sources
removed
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Sivalik Hills
Mahabharat Range

Terai
subtropical
monsoon

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