57:
85:
854:
657:
1025:
1036:(6.9 m/s), while winter and spring peak flows top 7,585 cubic feet per second (214.8 m/s) on average. The highest recorded peak flow at the creek's mouth in Spokane was 21,200 cubic feet per second (600 m/s) on 1 January 1997, closely followed by a flow of 20,600 cubic feet per second (580 m/s) on 3 February 1963. The lowest recorded peak flow was 395 cubic feet per second (11.2 m/s) in 1994.
925:
92:
64:
800:, which is the continuation of Lovell Valley Road in Washington State, it receives Moctileme Creek, its largest tributary, on the left bank. Moctileme Creek is about 6 miles (9.7 km) long, flowing west from Windfall Pass and mostly paralleling State Route 60. At this point, Little Latah Creek has already grown large from agricultural runoff. The creek then bisects Tekoa, flows underneath
40:
972:, including Plummer Creek. Tributaries flowing off this divide into Latah Creek (right-bank tributaries) include Little Latah Creek, Rattlers Run Creek, Rock Creek and California Creek. Left-bank tributaries include Marshall Creek and North Pine Creek. The watershed is bordered on the south by that of the
1076:
War", or "Big Fight", Qualchan and six other
Palouses were captured and hanged along Latah Creek, giving rise to the name, Hangman Creek. On 5 October of that year, four more Indians were hanged alongside the creek. In November, 33 Indian hostages were released, ending the war. In the aftermath, the
636:
passed the area in 1805, they believed that the name was "Lau-taw". Later in a railroad survey, the name used on the small-scale maps was Camas
Prairie Creek, while on the maps of larger scale, the name was Kamas Prairie Creek. Other derivatives, including Lahtoo and Kamass, arose from these names,
587:
resides. Some major tributaries of the approximately 60-mile (97 km) creek include Little Latah Creek (also known as Little
Hangman Creek) and Rock Creek. The average flow of the creek can range from 20 cubic feet per second (0.57 m/s) to 20,000 cubic feet per second (570 m/s). Latah
999:
Agricultural land use covers 212,880 acres (861.5 km) of the Latah Creek watershed, followed by 119,490 acres (483.6 km) of forest. Urban areas within the Latah Creek basin cover only 12,565 acres (50.85 km). Because of its importance as a tributary to the
Spokane, the pollution in
877:. The topography here are steep ridges and peaks dissected by deep, forested close-to-bedrock valleys, drained by rocky and steep mountain streams, with a light covering of soil. After its mountainous headwaters, the creek passes through the much more rounded, older Palouse Hills. Below the deep
726:
After having received Rock Creek, Latah Creek receives
California Creek, a 8-mile (13 km), west-southwest tributary, also on the right bank. In its final few miles, California Creek also plunges down a narrow gorge into the Latah Creek canyon. Latah Creek then continues north, and begins to
1288:
1113:. Nearby homesteaders William and Thomas Donahoe also drained a similar bog and located more bones and a skull. These bones, along with those from the Coplen bog, were delivered first to other cities in Washington State for exhibition. The original mammoth skeleton was later delivered to the
1035:
Streamflow in Latah Creek is highly variable, with the creek tending to flood in the winter and spring, diminishing to almost completely dry in the summer. The creek typically does not totally dry up, however, due to agricultural return flows. The monthly average is 242 cubic feet per second
824:, then turns west then north, crossing under State Route 27, entering a narrow gorge similar to that of Latah Creek. After meandering in the down cut gorge for a while, the creek straightens out and heads west-northwest, spilling into Latah Creek after turning sharply south just southwest of
747:
neighborhoods. As
Highway 195 continues to parallel it on the left, High Drive winds along the canyon rim on the east (right) bank. With high bluffs rising on the east side and lower cliffs on the west, the creek receives Marshall Creek on the left bank, and its second-last named tributary,
912:, was breached. The floods have deposited "terraces", otherwise known as "backflood deposits", which the creek has eroded through, creating steep and unstable gravel slopes topped by sheer cliffs. Near Spokane, the creek turns to the northwest in a nearly straight line; this is caused by a
637:
but another name, Ned-Whauld Creek (or Ned-Whauld River) was also documented. Other variant names of the creek include Sin-sin-too-ooley, Hangmans Creek, Hangman's Creek, Hngosmn, Kamas
Prairie Creek, Lah-Tah, Lah-taw, Lah-too, Lahtoo, Lartoo, Neduald, and Sin-sin-too-aley.
889:, which finally rises to meet stream elevation at the Washington-Idaho state border. Most of the creek from where it turns north at Sanders to about 20 miles (32 km) upstream of its mouth flows in a broad and shallow, arid valley atop several hundred feet of
619:
overall in the Latah Creek basin is quite low, and "Washington State water quality standards for temperature, dissolved oxygen, pH, and fecal coliforms are routinely violated." The remaining third of the land in the watershed is mostly forest.
1149:. Because of the aridity of its basin and the increasing pollution in Latah Creek and many of its tributaries, it is no longer a productive watershed for fishes and other aquatic species. Even as early as 1892, Latah Creek was described as
940:, is located at the junction of Latah Creek and the Spokane River. Except for its upper headwaters and the canyon it flows through in its final few miles, the creek flows in an open plain surrounded by low hills, and originally would form
844:
where it was once dammed for a mill, and enters Latah Creek between the Creek at
Qualchan golf course and the Cheney-Spokane Road exit of US-195. The creek receives flow from Minnie Creek, which also begins in the wetlands East of Cheney.
1154:
This is an unimportant stream tributary to the
Spokane. It was examined in the vicinity of Tekoa, Washington, where it was found to be a small filthy stream not suitable for trout but well supplied with minnows and suckers of several
1766:
1802:
816:. Like Little Latah Creek, it is in the vicinity of 10 miles (16 km) long. The creek turns west from its headwaters and begins to parallel its North Fork, which flows south then turns west from its headwaters at
1081:
have frequently disagreed on the name of the creek. While
Washington State, specifically Spokane County, claims and refers to the creek as Latah, the Board and local residents still refers to the creek as Hangman.
1168:
have disappeared in that time period. In the inventory taken by Gilbert and Evermann (1892) there were many species of suckers, some of which are still present in the creek today. The Native American variant name
956:
in the creek has increased, while water quality and habitat have decreased. At its mouth, Latah Creek has been known to contribute up to 90 percent of the flow of the downstream Spokane, and as low as 1 percent.
784:
Little Latah Creek, about 10 miles (16 km) long, is a generally southwest-flowing stream, and at the confluence carries almost as much water as Latah Creek. The creek begins a few miles south of
704:, where it is channelized and runs due north for a short distance. At this point, it has already picked up much agricultural runoff. At Tekoa, it also receives a large tributary, Little Latah Creek.
700:. Still small, it runs northwest in a vegetation-choked gully for several miles, beginning to parallel Latah Creek Road. The creek then crosses the Idaho-Washington state border and flows through
1056:
outpost while traveling alone. He was said to have prayed to the god of the mist to disarm the camp's sentries, and as a result, it began to snow, and when the snow had changed into a
711:, named for the creek. At Latah, it receives a short tributary, Cove Creek, on the right bank. The creek then bends west and runs north, then swings west again to run near the town of
1777:
820:. The North Fork is actually longer than the mainstream, although it carries only a slight amount of water when they join. The creek then crosses the state border and flows west of
1813:
688:. A few miles after its headwaters, it receives the South Fork Latah Creek, which flows north. At the confluence, the creek turns north, flowing past the towns of Sanders and
603:, which has released large amounts of sediment from the surrounding Palouse soils into the watershed on an annual basis. This has caused the ruin of natural fish populations,
1532:
716:
932:
The watershed of Latah Creek covers 673 square miles (1,740 km), stretching from southeast to northwest and straddling the Washington-Idaho state border. The mostly
977:
491:
723:.) The creek then enters a steadily deepening, winding gorge that runs generally northwest. It then receives another large tributary, Rock Creek, on the right bank.
1810:
Virginia Cooperative Fisheries Unit, Virginia Polytechnic Institute and State University; Bureau of Sport Fisheries and Wildlife, Division of River Basin Studies
993:
793:
1568:
948:
across this wide floodplain. The conversion of the floodplain to agricultural uses, however, forced the creek to flow in a straighter course. As a result,
825:
1141:
fish. However, the creek was shallow and slow-moving naturally, and was not an important habitat for these fish. The primary fishes of Latah Creek were
1109:. The bog was quickly drained, and an enormous quantity of bones were discovered. The shoulder blade and vertebra were later determined to be that of a
1000:
Latah Creek directly affects the Spokane downstream of their confluence. The only Spokane River tributary larger or equal in size to Latah Creek is the
936:
basin is divided mostly among forests and agriculture, with small towns spread along the length of the creek and its tributaries. The largest city,
865:
Latah Creek can be divided into three distinct geological regions; these are a small section of its upper headwaters, a long and broad valley, and
685:
665:
681:
17:
1412:
1068:. The Indians later rediscovered the whites' camp, only to find that they had left. His war party was later discovered, and after a brief
56:
1069:
644:
were hanged along the creek after a war. Washington State and Spokane County both approve Latah Creek as the official name, while the
1890:
1232:
84:
1543:
1078:
645:
1671:
1311:
1044:
In 1854, Latah Creek received its other name, Hangman Creek, which stayed for over a century and a half. According to legend, a
321:
1880:
1182:
1137:
It was said that in the early 19th century, Latah Creek was a clear and pristine stream that provided suitable habitat for
792:
crosses the creek very near the headwaters, and for its entire length, it follows Lovell Valley Road. Near the junction of
1160:
At the time of the 1892–93 sampling, there were two fishes that have apparently become extinct between then and 1974. The
1223:
1004:, which joins about 10 miles (16 km) downstream of Latah Creek. Although there are larger tributaries upstream of
1597:
1864:
1849:
1676:
529:
1627:
236:
1576:
1187:
1173:
is known to mean "Suckers in the Water", which implies that the sucker are likely the primary fish of Latah Creek.
764:. Its last named tributary, Indian Canyon Creek, enters on the left bank as the creek turns northeast to join the
1681:
1658:
1228:
1118:
1341:
1719:
1218:
1381:
592:
word likely meaning "fish". In 1854, the creek received another name, Hangman Creek, from a war between the
474:
1469:"The Case of the Mullan Road: Naming Features Along the Railroad and Road Surveys in the Northern Rockies"
1114:
858:
753:
615:, islands and natural channel formations have been destroyed. In response to these damaging factors, the
1256:
797:
707:
After meeting Little Latah Creek, Latah Creek continues northwards along State Route 27 to the town of
633:
580:
576:
1468:
1257:"Hangman Creek Conservation Success Index: Opportunities for Redband Trout Restoration and Protection"
989:
801:
757:
608:
1885:
744:
677:
1420:
1073:
981:
761:
1013:
984:, a tributary of the Spokane. Roads paralleling Latah Creek include (from mouth to headwaters)
736:
572:
1857:
Landscape traveled by coyote and crane: The world of the Schitsu'umsh (Coeur d'Aléne Indians).
1744:
1005:
965:
720:
669:
568:
218:
1146:
1001:
874:
841:
821:
769:
749:
478:
8:
1126:
1094:
1090:
937:
909:
894:
866:
740:
732:
712:
693:
560:
549:
396:
299:
189:
596:
and white soldiers, which resulted in several Palouse being hanged alongside the creek.
1720:"Benjamin Coplen discovers mammoth bones on Hangman [Latah] Creek in May 1876."
905:
893:
deposits. In the final 20 miles (32 km), the Latah Creek watershed intersects the
837:
788:, and its headwaters are near the ridge where north-flowing Plummer Creek also begins.
629:
589:
545:
542:
307:
163:
133:
1860:
1845:
1319:
1089:
lay beside Latah Creek for many tens of thousands of years, dating from the previous
933:
913:
708:
701:
185:
181:
1161:
985:
964:
on the east side of the watershed separates Latah Creek from streams draining into
902:
728:
506:
1122:
961:
898:
870:
789:
556:
1110:
1065:
945:
853:
817:
785:
689:
656:
604:
584:
449:
303:
1446:
1874:
1045:
1031:
waters of Latah Creek entering the Spokane River during a period of high flow
1009:
973:
969:
813:
773:
765:
641:
616:
593:
564:
453:
445:
336:
323:
287:
251:
238:
177:
153:
1142:
1061:
16:"Hangman Creek" redirects here. For the White Salmon River tributary, see
1803:"Further Information on the Inventory of Fishes in Hangman (Latah) Creek"
1634:
1165:
886:
719:. (SR 27 breaks away from the creek before Waverly to run to the town of
697:
600:
282:
1287:
Based on average of 59 water years, from 1949 to 2008; statistics from
1138:
1724:
History Link: The Free Online Encyclopedia of Washington State History
1097:, Benjamin Coplen, who found what seemed to be a gigantic bone in the
1800:
1764:
1349:
1028:
953:
812:
Rock Creek begins just about 1-mile (1.6 km) west-southwest of
1102:
1057:
1049:
890:
1602:
Washington State University Department of Earth and Space Sciences
869:. In its headwaters, the creek flows through the foothills of the
1466:
1106:
1053:
1024:
949:
941:
632:
word meaning "a place of pines and sestles", or "fish". When the
612:
924:
772:
is on the left bank of the Spokane, not too far downstream from
494:, Cove Creek, Rattler Run Creek, California Creek, Stevens Creek
18:
List of rivers of Washington (state) § Lower Columbia Basin
1382:"The Hangman (Latah) Creek Water Resources and Management Plan"
1312:"Hangman (Latah) Creek Watershed Planning Project: Project Map"
882:
731:
as it winds through a widening gorge towards the urban area of
1774:
U.S. Fish and Wildlife Service Division of River Basin Studies
39:
878:
673:
552:
222:
167:
1502:
1129:
of Washington and Idaho, including in this particular bog.
1098:
521:
515:
1767:"Preliminary Inventory of Fishes in Hangman (Latah) Creek"
1331:
Note: The creek length is an estimate from this map scale.
1086:
1064:
horses out of the camp, and took them to his camp on the
567:. It drains 673 square miles (1,740 km) in parts of
555:
in the United States. The creek flows northwest from the
1125:
were responsible for depositing a "bathtub ring" in the
660:
Sunset Highway and I-90 Crossing Latah Creek in Spokane.
752:, also on the left bank, and crosses under bridges for
1348:. Spokane County Conservation District. Archived from
1318:. Spokane County Conservation District. Archived from
530:
996:. There are no dams on the mainstem of Latah Creek.
980:, a tributary of the Palouse, and on the northwest,
518:
512:
1812:. Northwest Science, Vol. 48, No. 1. Archived from
1776:. Northwest Science, Vol. 47, No. 1. Archived from
1391:. Spokane County Conservation District. 19 May 2005
509:
1419:. Spokane Basin Watershed Planning. Archived from
1342:"Hangman (Latah) Creek Watershed Planning Project"
118:
71:Location of the mouth of Latah Creek in Washington
1533:"Spokane Subbasin Overview (section Latah Creek)"
1008:, the source of the Spokane River (including the
1872:
1801:Maughan, O. Eugene; Laumeyer, Philip L. (1974).
1765:Laumeyer, Philip H.; Maughan, O. Eugene (1973).
901:that inundated the area after an ice dam on the
735:. As it enters the Spokane it flows through the
607:, and natural flow patterns. The creek has been
1672:"USGS Gage #12424000 on Latah Creek at Spokane"
1633:. www.ecy.wa.gov. February 2006. Archived from
1507:(Map). Cartography by NAVTEQ. Google Maps. 2009
1254:
125:
1497:
1495:
1493:
1491:
1489:
1283:
1281:
836:Marshall Creek begins in the wetlands East of
473:South Fork Latah/Hangman Creek, Sheep Creek,
1842:Indians of the Pacific Northwest: A History.
1622:
1620:
1618:
1467:Grim, Ronald E.; McDermott, Paul D. (2004).
680:of the creek are in a small valley south of
583:in Washington, where over 64 percent of its
1486:
1278:
1250:
1248:
1121:of Chicago. It was later proposed that the
1093:. This bog was discovered in May 1876 by a
1072:, called the "George Wright War", "Spokane-
640:The name "Hangman" originated from when 17
1604:. www.geophys.washington.edu. 30 July 2001
1441:
1439:
1437:
1016:) those do not directly feed the Spokane.
988:, Latah Creek Road, Spangle-Waverly Road,
599:The Latah Creek watershed is dominated by
490:Indian Creek, Little Latah/Hangman Creek,
1615:
1407:
1405:
648:still identifies the creek is "Hangman".
1540:Northwest Power and Conservation Council
1245:
1233:United States Department of the Interior
1023:
923:
852:
739:neighborhood before passing between the
655:
1840:Ruby, Robert H.; Brown, John A (1988).
1573:University of Wisconsin - Stevens Point
1527:
1525:
1523:
1521:
1475:. COLUMBIA: Winter 2004, Vol. 18, No. 4
1434:
664:Latah Creek begins east of the town of
428:21,200 cu ft/s (600 m/s)
1873:
1794:
1402:
1334:
1255:Fesenmyer, Kurt; Reinke, Drew (2014).
1213:
1211:
1209:
1207:
1205:
1203:
1101:-covered water. Coplen then located a
1747:. Northwest History. 26 December 2007
1566:
1376:
1374:
1372:
1370:
1368:
1366:
1306:
1304:
1302:
1300:
1298:
1296:
779:
44:Ice-jam break up on Latah Creek, 2005
1518:
1183:List of rivers of Washington (state)
1077:Washington State government and the
418:10 cu ft/s (0.28 m/s)
408:231 cu ft/s (6.5 m/s)
1542:. www.nwcouncil.org. Archived from
1224:Geographic Names Information System
1200:
374:673 sq mi (1,740 km)
91:
63:
13:
1598:"2001 Spokane Earthquake Sequence"
1363:
1293:
14:
1902:
1677:National Water Information System
831:
1188:List of longest streams of Idaho
1105:of similarly large scale, and a
928:Map of the Latah Creek watershed
715:, and north to pass the town of
505:
90:
83:
62:
55:
38:
1891:Rivers of Benewah County, Idaho
1758:
1745:"Mammoths of the Inland Empire"
1737:
1712:
1703:
1694:
1664:
1659:United States Geological Survey
1651:
1590:
1569:"Channeled Scablands: Overview"
1560:
1229:United States Geological Survey
1119:Field Museum of Natural History
885:layer separates the creek from
873:, specifically in those of the
588:Creek receives its name from a
99:Latah Creek (the United States)
1844:University of Oklahoma Press.
1834:
1575:. www.uwsp.edu. Archived from
1460:
1079:U.S. Board on Geographic Names
628:The name "Latah" stems from a
315: • coordinates
230: • coordinates
74:Show map of Washington (state)
1:
1567:Dutch, Steve (9 April 2003).
1193:
1019:
807:
196:Physical characteristics
102:Show map of the United States
23:River in Idaho, United States
1881:Rivers of Washington (state)
1266:. Trout Unlimited. p. 2
919:
840:, flows through the town of
696:that have been converted to
563:, where it empties into the
354: • elevation
273:3,600 ft (1,100 m)
269: • elevation
7:
1176:
1115:Chicago Academy of Sciences
897:, which were formed by the
861:along the creek in Spokane.
392: • location
295: • location
214: • location
10:
1907:
1859:University of Washington.
1657:Data was collected by the
1039:
848:
804:, and enters Latah Creek.
798:Washington State Route 274
634:Lewis and Clark Expedition
424: • maximum
414: • minimum
404: • average
358:1,700 ft (520 m)
15:
1628:"Hangman Creek Watershed"
1132:
990:Washington State Route 27
916:named Latah Creek Fault.
802:Washington State Route 27
651:
484:
467:
459:
441:
436:
432:
422:
412:
402:
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382:
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212:
204:
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195:
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159:
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111:
49:
37:
28:
1449:. Spokane Outdoors. 2003
978:Hole-In-The-Ground Creek
881:in the Palouse Hills, a
486: • right
1219:"Hangman (Latah) Creek"
623:
579:and a small portion of
541:, is a large stream in
469: • left
366:60 mi (97 km)
126:
119:
1682:U.S. Geological Survey
1158:
1032:
929:
862:
661:
337:47.66000°N 117.45778°W
252:47.11472°N 116.71667°W
1855:Frey, Rodney (2001).
1151:
1027:
927:
856:
659:
1002:Little Spokane River
994:Idaho State Route 95
875:Clearwater Mountains
794:Idaho State Route 60
750:Garden Springs Creek
611:in some places, and
479:Garden Springs Creek
342:47.66000; -117.45778
257:47.11472; -116.71667
1127:channeled scablands
1060:, Qualchan led the
1014:Coeur d'Alene River
976:, and on the west,
895:Channeled Scablands
867:channeled scablands
694:channeled scablands
575:counties in Idaho,
437:Basin features
333: /
248: /
1504:Map of Latah Creek
1033:
1006:Coeur d'Alene Lake
966:Coeur d'Alene Lake
930:
906:Pend Oreille River
863:
780:Little Latah Creek
662:
646:federal government
1726:. HistoryLink.org
1661:from 1948 to 2001
1473:COLUMBIA Magazine
1417:Spokanecounty.org
1352:on April 17, 2009
1171:Snt'ut'u'lmkhwkwe
914:strike-slip fault
537:), also known as
498:
497:
120:Snt'ut'u'lmkhwkwe
1898:
1828:
1827:
1825:
1824:
1818:
1807:
1798:
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1756:
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1579:on 5 August 2009
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1252:
1243:
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1239:
1215:
1162:Bridgelip sucker
986:U.S. Highway 195
768:. Latah Creek's
762:Sunset Boulevard
729:U.S. Highway 195
533:
528:
527:
524:
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520:
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511:
487:
470:
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42:
26:
25:
1906:
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1900:
1899:
1897:
1896:
1895:
1886:Rivers of Idaho
1871:
1870:
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1487:
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1452:
1450:
1447:"Hangman Creek"
1445:
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1394:
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1322:on May 17, 2008
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1196:
1179:
1135:
1123:Missoula Floods
1117:, and then the
1085:A single known
1052:, discovered a
1042:
1022:
962:drainage divide
946:braided streams
922:
899:Missoula Floods
871:Rocky Mountains
851:
834:
810:
790:U.S. Highway 95
782:
745:Peaceful Valley
654:
642:Palouse Indians
626:
594:Palouse Indians
557:Rocky Mountains
531:
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1111:woolly mammoth
1107:shoulder blade
1066:Columbia River
1046:Palouse Indian
1041:
1038:
1021:
1018:
921:
918:
850:
847:
833:
832:Marshall Creek
830:
809:
806:
781:
778:
717:West Fairfield
686:Moses Mountain
670:Benewah County
653:
650:
625:
622:
605:riparian zones
581:Whitman County
577:Spokane County
496:
495:
488:
482:
481:
475:Marshall Creek
471:
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450:Columbia River
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1865:0-295-98171-7
1862:
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1850:0-8061-2113-0
1847:
1843:
1839:
1838:
1819:on 2012-02-20
1815:
1811:
1804:
1797:
1783:on 2012-02-20
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1640:on 2012-03-05
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1549:on 2007-12-16
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1423:on 2015-09-24
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1413:"Latah Creek"
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1096:
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1080:
1075:
1074:Coeur d'Aléne
1071:
1067:
1063:
1059:
1055:
1051:
1047:
1037:
1030:
1026:
1017:
1015:
1011:
1010:St. Joe River
1007:
1003:
997:
995:
991:
987:
983:
979:
975:
974:Palouse River
971:
970:St. Joe River
967:
963:
958:
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951:
947:
943:
939:
935:
926:
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787:
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774:Spokane Falls
771:
767:
766:Spokane River
763:
759:
755:
754:Interstate 90
751:
746:
742:
738:
737:Latah/Hangman
734:
730:
724:
722:
718:
714:
710:
705:
703:
699:
695:
691:
687:
683:
682:Charles Butte
679:
675:
671:
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658:
649:
647:
643:
638:
635:
631:
621:
618:
617:water quality
614:
610:
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597:
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591:
586:
582:
578:
574:
570:
566:
565:Spokane River
562:
558:
554:
551:
550:north central
547:
544:
540:
539:Hangman Creek
536:
535:
526:
502:
493:
489:
483:
480:
476:
472:
466:
462:
458:
455:
454:Pacific Ocean
451:
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446:Spokane River
444:
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318:
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288:Spokane River
286:
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280:
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261:
233:
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220:
217:
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208:Charles Butte
207:
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154:United States
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128:
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117:
116:
114:
110:
86:
58:
48:
41:
36:
32:Hangman Creek
27:
19:
1856:
1841:
1821:. Retrieved
1814:the original
1809:
1796:
1785:. Retrieved
1778:the original
1773:
1760:
1749:. Retrieved
1739:
1728:. Retrieved
1723:
1714:
1705:
1700:Ruby, p. 164
1696:
1685:. Retrieved
1675:
1666:
1653:
1642:. Retrieved
1635:the original
1606:. Retrieved
1601:
1592:
1581:. Retrieved
1577:the original
1572:
1562:
1551:. Retrieved
1544:the original
1539:
1509:. Retrieved
1503:
1477:. Retrieved
1472:
1462:
1451:. Retrieved
1425:. Retrieved
1421:the original
1416:
1393:. Retrieved
1388:
1354:. Retrieved
1350:the original
1345:
1336:
1324:. Retrieved
1320:the original
1315:
1289:USGS website
1268:. Retrieved
1263:
1236:. Retrieved
1222:
1170:
1159:
1153:
1152:
1136:
1084:
1043:
1034:
998:
959:
931:
910:last ice age
864:
835:
811:
783:
725:
706:
663:
639:
627:
598:
538:
500:
499:
1835:Works cited
1709:Frey, p. 85
1264:fs.usda.gov
1166:Chiselmouth
1095:homesteader
887:groundwater
692:, entering
609:channelized
601:agriculture
501:Latah Creek
460:Tributaries
442:Progression
340: /
328:117°27′28″W
255: /
190:Spokane, WA
112:Native name
29:Latah Creek
1875:Categories
1823:2014-05-28
1787:2014-05-28
1751:2009-07-20
1730:2009-07-20
1687:2009-07-22
1644:2009-07-18
1608:2009-07-22
1583:2009-07-22
1553:2009-07-22
1511:2009-07-18
1479:2009-07-24
1453:2009-07-18
1427:2014-05-28
1395:2014-05-28
1356:2009-07-20
1326:2009-07-18
1238:2009-07-20
1194:References
1139:anadromous
1020:Streamflow
982:Deep Creek
960:The small
903:Clark Fork
808:Rock Creek
758:a railroad
741:West Hills
678:headwaters
546:Washington
492:Rock Creek
371:Basin size
325:47°39′36″N
308:Washington
243:116°43′0″W
240:47°06′53″N
178:DeSmet, ID
164:Washington
1147:whitefish
954:turbidity
920:Watershed
727:parallel
721:Fairfield
630:Nez Perce
590:Nez Perce
585:watershed
383:Discharge
186:Latah, WA
182:Tekoa, WA
134:Nez Perce
1389:Sccd.org
1346:Sccd.org
1316:Sccd.org
1177:See also
1155:species.
1103:vertebra
1058:blizzard
1050:Qualchan
1012:and the
968:and the
942:meanders
934:semiarid
891:alluvial
857:Exposed
842:Marshall
822:Rockford
698:farmland
613:meanders
573:Kootenai
145:Location
1091:Ice Age
1062:whites'
1054:cavalry
1040:History
950:erosion
938:Spokane
849:Geology
818:Plummer
786:Plummer
733:Spokane
713:Waverly
690:De Smet
666:Sanders
569:Benewah
561:Spokane
543:eastern
397:Spokane
300:Spokane
150:Country
1863:
1848:
1270:21 May
1143:sucker
1133:Fishes
1048:named
1029:Turbid
992:, and
883:basalt
859:Basalt
838:Cheney
826:Duncan
814:Worley
760:, and
676:. The
652:Course
463:
386:
363:Length
205:Source
174:Cities
130:
1817:(PDF)
1806:(PDF)
1781:(PDF)
1770:(PDF)
1638:(PDF)
1631:(PDF)
1547:(PDF)
1536:(PDF)
1385:(PDF)
1260:(PDF)
879:loess
770:mouth
709:Latah
702:Tekoa
674:Idaho
668:, in
553:Idaho
283:Mouth
223:Idaho
168:Idaho
160:State
127:Latah
1861:ISBN
1846:ISBN
1272:2022
1164:and
1145:and
1099:peat
952:and
944:and
796:and
743:and
684:and
624:Name
571:and
548:and
1087:bog
1070:war
559:to
534:-tə
532:LAY
1877::
1808:.
1772:.
1722:.
1680:.
1674:.
1617:^
1600:.
1571:.
1538:.
1520:^
1488:^
1471:.
1436:^
1415:.
1404:^
1387:.
1365:^
1344:.
1314:.
1295:^
1280:^
1262:.
1247:^
1231:,
1227:.
1221:.
1202:^
828:.
776:.
756:,
672:,
516:eɪ
477:,
452:→
448:→
306:,
302:,
221:,
188:,
184:,
180:,
166:,
1867:.
1852:.
1826:.
1790:.
1754:.
1733:.
1690:.
1647:.
1611:.
1586:.
1556:.
1514:.
1482:.
1456:.
1430:.
1398:.
1359:.
1329:.
1274:.
1241:.
525:/
522:ə
519:t
513:l
510:ˈ
507:/
503:(
136:)
132:(
20:.
Text is available under the Creative Commons Attribution-ShareAlike License. Additional terms may apply.