Big BeltsSpeciesGeographic BoundaryThis linkage area is primarily comprisedof the Big Belt Mountains. <strong>The</strong>y arebordered by the Canyon Ferry-HelenaValley on the west, and the Smith RiverValley on the east, the Bridger Mountainsto the south.Importance of Linkage <strong>Area</strong>This linkage area connects animalsmoving southeast out of the Sawtooths/Marysville area with the BridgerMountains and, ultimately, the northernend of the Greater Yellowstoneecosystem to the south. It could functionas a link between the Sawtooths (RockyMountain Front) and the Little BeltMountains.Mountain ranges connected in thislinkage: Sawtooths (Rocky MountainFront) and Bridgers.Ecological Setting<strong>The</strong> Big Belts are an isolated mountainrange on the east side of the MissouriRiver drainage, adjacent to Canyon Ferryreservoir. <strong>The</strong> linkage is mostly forestedby Douglas-fir (Pseudotsuga menziesii)and ponderosa pine (Pinus ponderosa)with lodgepole pine (P. contorta) andwhitebark pine (P. albicaulus) at higherelevations intermixed with open meadowsand riparian valleys. South-facing slopesare typically less heavily forested thannorth-facing slopes and higher elevations.Foothills are drier with scattered RockyMountain juniper (Juniperus scopulorum)and limber pine (P. flexilis) and a varietyof shrubs on some sites. At the lowestelevations, all tree cover gives way tograsslands and scattered big sagebrushstands (Artemisia tridentata spp.). Manyof these habitats have been convertedto dry land grain and irrigated cropland,57particularly on the alluvial flats on theeast side of Canyon Ferry Reservoir.Timber harvest has occurred throughoutthe linkage, particularly on the north end,using a high density road network, wherethere is a distinct checkerboard patternof land ownership. Extensive forestedareas remain intact and unroaded in thecentral part of the linkage. Highway12 crosses the south end of the linkage.Elevations in the linkage range from about3,500 feet adjacent to Canyon FerryReservoir to over 9,500 feet.<strong>Wildlife</strong>This area currently functions primarilyas a movement corridor for carnivoresand ungulates. <strong>The</strong> northern end ofthe Big Belts is the most likely linkagesto the Little Belt Mountains to the eastacross the Upper Smith River Valley fromthe Birch Creek drainage north to theMilligan Hill area, encompassing the DryRange.Grizzly bears: This area could serve as apotential north-south movement corridor.<strong>The</strong>re have been unconfirmed reports ofgrizzly bear around York.Black bear can be found throughout theBig Belts.Wolves have been reported in thislinkage area, particularly around theEdith Lake area. On a regional scale,this linkage is thought to be a potentialnorth-south corridor for wolves movingbetween the Greater Yellowstone andNorthern Continental Divide ecosystem.Wolverines have been sighted yeararoundin the Gates of the Mountainsarea; the area at Sweats Creek betweenYork and Nelson is potential denninghabitat, with many fallen trees fromstorms. <strong>The</strong> entire crest of the BigBelts, such as Boulder-Baldy, is potential
wolverine habitat.Lynx are present in very small numbers onHogback Mountain. <strong>The</strong> lynx habitat in thislinkage area is marginal.Elk thrive on good summertime forage habitatin the Big Belts. Elk Ridge and Jim Ball Basinare examples of summer range, composed ofvery productive, high quality habitat with alot of open grasslands. <strong>The</strong> west slopes of theBig Belts have several important winter rangeareas, such as White’s Creek and Deep Creek.<strong>The</strong> White’s Creek- White Gulch- ConfederateGulch to Duck Creek area is a distinct winterrange on private land. Elk migrate up the westslope winter range to summer on the Big BeltDivide at the head of Rock Creek and BeaverCreek. Elk at the Cottonwood Creek and RayCreek winter range are the southernmost elkherd in this linkage area. Elk also winter onthe east side of the Big Belts, particularly alongthe flanks of the mountains near Birch Creek.Pronghorn are found at Canyon Ferry to DeepCreek and from East Helena to Canyon Ferryduring the winter, spring, and fall. East ofCanyon Ferry, there is a herd of about 600antelope that are doing well on agriculturallands.Moose in this linkage area are found around thelower drainages of all the 2nd and 3rd orderstreams around Townsend. <strong>The</strong> Big Belts aredry habitat and therefore not “prime” moosehabitat. Moose can be found in the southwestBig Belts in the north fork of Deep Creek. Other“moosey” areas of this linkage are in CabinGulch, Sulphur Bar, and Hay Creek. On the eastside of the Big Belts, moose can be found inthe Gypsy Lake, Birch Creek and Camas Creekareas.Mountain goats were transplanted in thismountain range from the Sleeping Giant areafollowing a population die-off from pneumonia.Mountain goats can be found primarily in foursubpopulations located in the Beaver Creek,Avalanche-Hellgate, Boulder-Baldy, and Mt.Edith areas with scattered individuals foundelsewhere. <strong>The</strong> goats tend to come down tothe lower flat areas of the linkage during springgreen-up.58Mule deer can be found throughout the BigBelts, with important winter range in theWhite Creek area. Conversely, this is also animportant area for mountain lions, whoseprimary prey are mule deer.<strong>Conservation</strong> ThreatsDevelopment: Most of Jim Ball Basin is privateland. Within this linkage area, much of theungulate winter range is on private land. Iftheses lands were to be developed, it wouldnegatively impact the elk and mule deerpopulations.Recreation: the area between Trout Creek andMagpie Gulch is a bottleneck for wildlife dueto the high amount of motorized recreation inthe area. Avalanche Creek, which is importantfor mountain goats, is another high-use area formotorized recreation.Highways are a threat due to the fragmentationof habitat from both the roads and associateddevelopment, and from direct animal-vehiclecollisions. <strong>The</strong> Hellgate area on the east sideof Canyon Ferry is a hotspot for elk collisionson Highway 284. U.S. Highway 12 also crossesthe south end of the Big Belts and is a potentialsource of collisions and fragmentation.Loss of Access: Increasingly, access to publicand private lands is becoming more restricted.This leads to “privatization” of wildlife and aloss of ability for Montana Fish, <strong>Wildlife</strong> andParks to meet their target numbers for wildpopulations. In this linkage area, the White’sCreek- White Gulch- Confederate Gulch toDuck Creek elk winter range is on private land;Montana Fish, <strong>Wildlife</strong> and Parks is no longerable to manage this herd.Noxious Weeds, particularly Dalmatian toadflax,Spotted Knapweed, and Leafy Spurge, are a bigissue. <strong>The</strong>ir presence is negatively affectingungulate forage in grasslands and meadows.Fire suppression in the area has led to coniferencroachment, which is causing a loss ofvaluable montane parkland habitat. This couldeventually lead to a catastrophic fire.Disease: <strong>The</strong> mountain goat population hadto be transplanted after an initial die-off due
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Executive SummaryMaintaining the ec
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- Page 26 and 27: with mountainous wet meadows and ri
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- Page 38 and 39: may not provide functional connecti
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- Page 45 and 46: Photo by Denver Bryanpopulations. L
- Page 47 and 48: Mountain goat (Oreamnos americanus)
- Page 49 and 50: GUIDE TO READINGPRIORITY LINKAGE AS
- Page 51 and 52: Absaroka to CraziesSpeciesGeographi
- Page 53 and 54: BangtailsSpeciesGeographic Boundary
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- Page 65 and 66: Elk move within this linkage for wi
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- Page 80 and 81: Clinton to DrummondSpeciesGeographi
- Page 82 and 83: There has been a settlement with At
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- Page 96 and 97: FleecerSpeciesGeographic BoundaryFl
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- Page 104 and 105: Garnets to BouldersSpeciesGeographi
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persistent spring snow and may be k
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Garnets. The Clark Fork River Corri
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Horseshoe HillsSpeciesGeographic Bo
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Hound CreekSpeciesGeographic Bounda
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Jefferson SloughSpeciesGeographic B
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117
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Willow packs moved here from the po
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the high potential for conflict wit
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the Castle Mountains south of Whets
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Lolo to TurahSpeciesGeographic Boun
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path; this could further fragment w
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Lost TrailSpeciesGeographic Boundar
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MacDonald Pass toFleecer/Mt. Haggin
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claims within the area and 75 are b
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Conservation ThreatsDevelopment cou
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MaxvilleSpeciesGeographic BoundaryT
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Norris HillSpeciesGeographic Bounda
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PipestoneSpeciesGeographic Boundary
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144
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persistent snow pack.Lynx: Boles Cr
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Potter BasinSpeciesGeographic Bound
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150
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Mountain goats exist in small pocke
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Rocky Mountain Front to Big BeltMou
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Disease between bighorn sheep and d
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the linkage, grizzly bear forage in
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influencing how wildlife connectivi
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Several bighorn sheep herds form am
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Silver StarSpeciesGeographic Bounda
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166
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controlled. In recent years, approx
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esulting from livestock depredation
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StickneySpeciesGeographic BoundaryT
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SulaSpeciesGeographic BoundaryThe S
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Tom Miner to Mill CreekSpeciesGeogr
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development. Subdivision, fencing a
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Townsend from 1000 to 300 animals.
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These appear to be important for gr
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Other existing packs include the Wo
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Creek and the Boulder River south o
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192
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Harestad A.S., and F.L. Bunnell. 19
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Trakhtenbrot, A. R. Nathan, G. Perr
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Appendix 1 (cont.).Table 1Mammals o
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Appendix 2 (cont.).Table 2Home Rang
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Appendix 3 (cont.).Table 3Migration
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Appendix 4 (cont.).Table 4Dispersal
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Appendix 5 (cont.).Studies Demonstr
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American Wildlands ~ Winter 2008