Coyote Lake Lahontan Cutthroat Trout
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Beatys Butte Herd Management Area Description
Beatys Butte Herd Management Area Lakeview District LOCATION: The area is located 65 miles east of Lakeview, Oregon. It is adjacent to and southeast of the Hart Mountain Antelope Refuge, is southeast of Catlow Valley, and bordered on the South by the Charles Sheldon National Antelope Refuge. ACREAGE: 437,120 acres of federal, state and privately owned land. ELEVATION/LANDMARKS: Beatys Butte, located in the north‐central part of the area is the most prominent landmark. It’s elevation of 7,885 feet above sea level makes it the highest point in the Lakeview Resource Area. There is a complex of smaller buttes surrounding Beatys Butte. TOPOGRAPHY/VEGETATION: Vegetation consists primarily of big sagebrush and bunch grasses. Low sagebrush communities are interspersed throughout the area. Topography varies from gently rolling hills to steep rugged hills and buttes with a number of broad valleys and shallow or dry lake beds. Slopes range from 0 to 60%. Precipitation averages 9 inches annually, mainly from winter snowfall. Summers are short, warm and dry while winters are typically long and cold. WILDLIFE: The area has a wide diversity of wildlife habitats and species including resident, migratory and nomadic populations. Large mammals include California bighorn sheep, pronghorn antelope and mule deer. Animals typical in the area are coyote, raven, red‐tail hawk, American kestrel, prairie falcon, turkey vulture, rough‐legged hawk, chukar partridge, valley quail, morning dove, Northern harrier, common crow, magpie, great horned owl, mountain lion, bobcat, Great Basin fence lizard and rattlesnake. Also, there are numerous small mammals and wetland birds. HERD SIZE: 100‐250 head. -
Bonneville Cutthroat Trout (Oncorhynchus Clarki Utah) Bonneville Cutthroat Trout Is One of Three Cutthroat Trout Subspecies Native to Utah
FISH Bonneville Cutthroat Trout (Oncorhynchus clarki utah) Bonneville cutthroat trout is one of three cutthroat trout subspecies native to Utah. Bonneville cutthroat trout historically occurred in the Pleistocene Lake Bonneville basin, which included portions of Idaho, Nevada, Utah, and Wyoming (Kershner 1995). The desiccation of Lake Bonneville into the smaller Great Salt Lake and fragmentation of other stream and lake habitats may have led to three slightly differentiated groups of Bonneville cutthroat trout. These groups are found in the Bonneville basin proper, the Bear River drainage, and the Snake Valley (Behnke 1992). There are five known populations of pure strain Bonneville cutthroat trout on the Fishlake National Forest inhabiting approximately 38 miles of stream habitat. There are several recently reintroduced populations, and several small potential remnant populations. Habitat for the Bonneville cutthroat trout is widely distributed and variable. It ranges from high elevation (3,500 m mean sea level) streams with coniferous and deciduous riparian trees to low elevation (1,000 m mean sea level) streams in sage-steppe grasslands containing herbaceous riparian zones. As such, Bonneville cutthroat trout have adapted to a broad spectrum of habitat conditions throughout their range (Kershner 1995). Sexual maturity is typically reached during the second year for males and the third year for females (May et al. 1978). Both the age at maturity and the annual timing of spawning vary geographically with elevation, temperature, and life history strategy. Lake resident trout may begin spawning at two years of age and usually continue throughout their lives, while adfluvial individuals may not spawn for several years. -
The Native Trouts of the Genus Salmo of Western North America
CItiEt'SW XHPYTD: RSOTLAITYWUAS 4 Monograph of ha, TEMPI, AZ The Native Trouts of the Genus Salmo Of Western North America Robert J. Behnke "9! August 1979 z 141, ' 4,W \ " • ,1■\t 1,es. • . • • This_report was funded by USDA, Forest Service Fish and Wildlife Service , Bureau of Land Management FORE WARD This monograph was prepared by Dr. Robert J. Behnke under contract funded by the U.S. Fish and Wildlife Service, the Bureau of Land Management, and the U.S. Forest Service. Region 2 of the Forest Service was assigned the lead in coordinating this effort for the Forest Service. Each agency assumed the responsibility for reproducing and distributing the monograph according to their needs. Appreciation is extended to the Bureau of Land Management, Denver Service Center, for assistance in publication. Mr. Richard Moore, Region 2, served as Forest Service Coordinator. Inquiries about this publication should be directed to the Regional Forester, 11177 West 8th Avenue, P.O. Box 25127, Lakewood, Colorado 80225. Rocky Mountain Region September, 1980 Inquiries about this publication should be directed to the Regional Forester, 11177 West 8th Avenue, P.O. Box 25127, Lakewood, Colorado 80225. it TABLE OF CONTENTS Page Preface ..................................................................................................................................................................... Introduction .................................................................................................................................................................. -
Yucca Mountain Project Area Exists for Quality Data Development in the Vadose Zone Below About 400 Feet
< I Mifflin & Associates 2700 East Sunset Road, SufteInc. C2 Las Vegas, Nevada 89120 PRELIMINARY 7021798-0402 & 3026 FAX: 702/798-6074 ~ADd/tDaeii -00/( YUCCA MOUNTAIN PRO1. A Summary of Technical Support Activities January 1987 to June 1988 By: Mifflin & Associates, Inc. LaS Vegas, Nevada K) Submitted to: .State of Nevada Agency for Nuclear Projects Nuclear Waste Project Office Carson City, Nevada H E C El V E ii MAY 15 1989 NUCLEAR WASTE PROJECt OFFICE May 1989 Volume I 3-4:0 89110o3028905a, WASTE PLDR wM-11PDC 1/1 1 1 TABLE OF CONTENTS I. INTRO DUCTION ............................................................................................................................ page3 AREAS OF EFFORT A. Vadose Zone Drilling Program ............................................................................................. 4 Introduction .............................................................................................................................. 5 Issues ....................................................................................................................................... 7 Appendix A ............................................................................................................................... 9 B. Clim ate Change Program ....................................................................................................... 15 Introduction .............................................................................................................................. 16 Issues ...................................................................................................................................... -
History of Lahontan Cutthroat Trout in Spring Creek, Utah
Spring Creek Population History of the Pyramid Lake Rediscovery (Again) Unfortunately, given its small size, the trout Lahontan Cutthroat population at Spring Creek has a very low In October 2009, a team from Weber State probability of survival. It lacks the numbers The Lahontan cutthroat trout, Oncorhynchus University in conjunction with personnel and space necessary to maintain sufficient clarkii henshawi, is native to the Lahontan Basin from the DWR identified several specimens genetic diversity. It is believed that for a on the border between California and Nevada. believed to be of a pure or hybrid strain of mountain stream cutthroat population to For thousands of years it thrived and played the Pyramid Lake Lahontan cutthroat trout survive it must have a minimum of 3.3 km an important economic and cultural role in Spring Creek in Uintah, Utah. Using of habitat and an abundance in the area of among the Native American tribes of the electrofishers and dip nets, a 600 m stretch 0.3 fish per meter.3 Based on our region. The largest strain of this fish of the stream was sampled. A maximum observations, the Spring Creek population originated in Pyramid Lake, in western of 16 different individuals was collected in A Unique Environment has a maximum abundance of 0.1 fish/m Nevada and has reached recorded weights of two sampling trips. The fish appeared to Spring Creek’s unique vegetation and only 200 m of habitat. However, against up to 41 pounds, making it the largest “The Fish that Won’t Die” be restricted to a 200 m stretch. -
Spatially-Explicit Modeling of Modern and Pleistocene Runoff and Lake Extent in the Great Basin Region, Western United States
Spatially-explicit modeling of modern and Pleistocene runoff and lake extent in the Great Basin region, western United States Yo Matsubara1 Alan D. Howard1 1Department of Environmental Sciences University of Virginia P.O. Box 400123 Charlottesville, VA 22904-4123 Abstract A spatially-explicit hydrological model balancing yearly precipitation and evaporation is applied to the Great Basin Region of the southwestern United States to predict runoff magnitude and lake distribution during present and Pleistocene climatic conditions. The model iteratively routes runoff through, and evaporation from, depressions to find a steady state solution. The model is calibrated with spatially-explicit annual precipitation estimates and compiled data on pan evaporation, mean annual temperature, and total yearly runoff from stations. The predicted lake distribution provides a close match to present-day lakes. For the last glacial maximum the sizes of lakes Bonneville and Lahontan were well predicted by linear combinations of decrease in mean annual temperature from 0 to 6 °C and increases in precipitation from 0.8 to 1.9 times modern values. Estimated runoff depths were about 1.2 to 4.0 times the present values and yearly evaporation about 0.3 to 1 times modern values. 2 1. Introduction The Great Basin of the southwestern United States in the Basin and Range physiographic province contains enclosed basins featuring perennial and ephemeral lakes, playas and salt pans (Fig. 1). The Great Basin consists of the entire state of Nevada, western Utah, and portions of California, Idaho, Oregon, and Wyoming. At present it supports an extremely dry, desert environment; however, about 40 lakes (some reaching the size of present day Great Lakes) episodically occupied the Great Basin, most recently during the last glacial maximum (LGM) [Snyder and Langbein, 1962; Hostetler et al., 1994; Madsen et al., 2001]. -
Open-File/Color For
Questions about Lake Manly’s age, extent, and source Michael N. Machette, Ralph E. Klinger, and Jeffrey R. Knott ABSTRACT extent to form more than a shallow n this paper, we grapple with the timing of Lake Manly, an inconstant lake. A search for traces of any ancient lake that inundated Death Valley in the Pleistocene upper lines [shorelines] around the slopes Iepoch. The pluvial lake(s) of Death Valley are known col- leading into Death Valley has failed to lectively as Lake Manly (Hooke, 1999), just as the term Lake reveal evidence that any considerable lake Bonneville is used for the recurring deep-water Pleistocene lake has ever existed there.” (Gale, 1914, p. in northern Utah. As with other closed basins in the western 401, as cited in Hunt and Mabey, 1966, U.S., Death Valley may have been occupied by a shallow to p. A69.) deep lake during marine oxygen-isotope stages II (Tioga glacia- So, almost 20 years after Russell’s inference of tion), IV (Tenaya glaciation), and/or VI (Tahoe glaciation), as a lake in Death Valley, the pot was just start- well as other times earlier in the Quaternary. Geomorphic ing to simmer. C arguments and uranium-series disequilibrium dating of lacus- trine tufas suggest that most prominent high-level features of RECOGNITION AND NAMING OF Lake Manly, such as shorelines, strandlines, spits, bars, and tufa LAKE MANLY H deposits, are related to marine oxygen-isotope stage VI (OIS6, In 1924, Levi Noble—who would go on to 128-180 ka), whereas other geomorphic arguments and limited have a long and distinguished career in Death radiocarbon and luminescence age determinations suggest a Valley—discovered the first evidence for a younger lake phase (OIS 2 or 4). -
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Bildnachweis Im Bildnachweis verwendete Abkürzungen: With permission from the Geological Society of Ame- rica l – links; m – Mitte; o – oben; r – rechts; u – unten 4.65; 6.52; 6.183; 8.7 Bilder ohne Nachweisangaben stammen vom Autor. Die Autoren der Bildquellen werden in den Bildunterschriften With permission from the Society for Sedimentary genannt; die bibliographischen Angaben sind in der Literaturlis- Geology (SEPM) te aufgeführt. Viele Autoren/Autorinnen und Verlage/Institutio- 6.2ul; 6.14; 6.16 nen haben ihre Einwilligung zur Reproduktion von Abbildungen gegeben. Dafür sei hier herzlich gedankt. Für die nachfolgend With permission from the American Association for aufgeführten Abbildungen haben ihre Zustimmung gegeben: the Advancement of Science (AAAS) Box Eisbohrkerne Dr; 2.8l; 2.8r; 2.13u; 2.29; 2.38l; Box Die With permission from Elsevier Hockey-Stick-Diskussion B; 4.65l; 4.53; 4.88mr; Box Tuning 2.64; 3.5; 4.6; 4.9; 4.16l; 4.22ol; 4.23; 4.40o; 4.40u; 4.50; E; 5.21l; 5.49; 5.57; 5.58u; 5.61; 5.64l; 5.64r; 5.68; 5.86; 4.70ul; 4.70ur; 4.86; 4.88ul; Box Tuning A; 4.95; 4.96; 4.97; 5.99; 5.100l; 5.100r; 5.118; 5.119; 5.123; 5.125; 5.141; 5.158r; 4.98; 5.12; 5.14r; 5.23ol; 5.24l; 5.24r; 5.25; 5.54r; 5.55; 5.56; 5.167l; 5.167r; 5.177m; 5.177u; 5.180; 6.43r; 6.86; 6.99l; 6.99r; 5.65; 5.67; 5.70; 5.71o; 5.71ul; 5.71um; 5.72; 5.73; 5.77l; 5.79o; 6.144; 6.145; 6.148; 6.149; 6.160; 6.162; 7.18; 7.19u; 7.38; 5.80; 5.82; 5.88; 5.94; 5.94ul; 5.95; 5.108l; 5.111l; 5.116; 5.117; 7.40ur; 8.19; 9.9; 9.16; 9.17; 10.8 5.126; 5.128u; 5.147o; 5.147u; -
Species Fact Sheet Coastal Cutthroat Trout Oncorhynchus Clarkii
Species Fact Sheet Coastal Cutthroat Trout Oncorhynchus clarkii STATUS: SPECIES OF The Southwestern Washington/Lower Columbia CONCERN River Distinct Population Southwestern Segment of Coastal cutthroat Washington/Lower trout potentially occurs in these Washington counties: Thurston, Columbia River Distinct Lewis, Yakima, Mason, Pacific, Population Segment Grays Harbor, Wahkiakum, Cowlitz, Clark, Skaminia, Klickitat, (Map may reflect historical as well as recent sightings) In 1999, the southwestern Washington/lower Columbia River Distinct Population Segment of coastal cutthroat trout, Oncorhynchus clarkii clarkii, was listed as threatened by National Marine Fisheries Service and the U.S. Fish and Wildlife Service FR 64(64): 16397-414. Subsequently, the Fish and Wildlife Service assumed sole regulatory jurisdiction. Based on changes in forest management regulation, the latest information indicating better than expected total populations in a large portion of the area, and an improved understanding of the ability of freshwater forms to produce anadromous progeny, the Fish and Wildlife Service withdrew the listing proposal in 2002. Current and Historical Status This Distinct Population Segment (DPS) includes populations in the Columbia River and its tributaries downstream from the Klickitat River in Washington and Fifteenmile Creek in Oregon to the Columbia River estuary; and the Willamette River and its tributaries downstream from Willamette Falls, to its confluence with the Columbia River, as well as in tributaries of Gray's Harbor and Willapa Bay. The southwestern Washington-lower Columbia River region historically supported highly productive coastal cutthroat trout populations. Coastal cutthroat trout are well distributed in most river basins in this geographic region, although probably in lower numbers relative to historical population sizes. -
Market-Sized Cutthroat Trout Technical Report Western Regional Aquaculture Center
Feeds for Production of Market-sized Cutthroat Trout Technical Report WESTERN REGIONAL AQUACULTURE CENTER Gary Fornshell, University of Idaho Christopher Myrick, Colorado State University Madison Powell, University of Idaho Wendy Sealey, United States Fish and Wildlife Service United States Department of Agriculture National Institute of Food and Agriculture 1 PROJECT PARTICIPANTS Christopher Myrick, Colorado State University Cheyenne Owens, Colorado State University Biswamitra Patro, University of Idaho Madison Powell, University of Idaho Pat Blaufuss, University of Idaho Tracy Kennedy, University of Idaho Wendy Sealey, United States Fish and Wildlife Service Brian Ham, United States Fish and Wildlife Service Gary Fornshell, University of Idaho Jeremy Liley, Liley Fisheries, Inc. David Brock, Rangen, Inc. Jackie Zimmerman, Skretting USA Rick Barrows, Aquatic Feed Technologies, LLC Photo credits: Cover: Gary Fornshell Above: iStock.com/KaraGrubis 2 Table of Contents Introduction: Why Consider Cutthroat Trout? 1 Snake River Cutthroat Trout—A Culturable Cutthroat 2 Is Raising Fish for the Recreational Market Worthwhile? 3 Overcoming Challenges to Raising Cutthroat Trout 3 Fish Nutrition 101—A Primer on Feed Formulation 3 Feed Pellet Texture Matters 5 Cutthroat Trout Growth—Does It Match Rainbow Trout? 5 Thermal Growth Coefficient 5 Comparing Rainbow and Cutthroat Trout Performance 6 Suggested Readings 10 Acknowledgments 11 Figures 1. Snake River cutthroat trout. 1 2. Map showing the distribution of extant cutthroat trout 2 subspecies in the western United States. 3. Juvenile Snake River cutthroat trout ready for stocking. 3 4. Classic bell-shaped growth-temperature curve. 6 5. Sigmoid growth curve. Based on Fish Hatchery Management, Second Edition, Gary Wedemeyer, editor 7 6. -
Spatial Variation in Spawning Habitat of Cutthroat Trout in a Sediment
Transactions of the American Fisheries Society 125:768-779. 1996 © Copyright by the American Fisheries Society 1996 Spatial Variatio Spawninn i g Habita f Cutthroato t Troua n ti Sediment-Rich Stream Basin JAMES P. MAGEE' AND THOMAS E. McMAHON2 Biology Department, FishWildlifeand Program Montana State University, Bozeman, Montana 59717,USA RUSSELL E THUROW U.S. Forest Service, Intermountain Research Station 316 East Myrtle Street. Boise, Idaho 83702,USA Abstract.—We examined distributio habitad nan t characteristic f spawnino s g site f cutthroaso t trout Oncorhynchus clarki t varioua s spatial scale asseso st s effect f sedimentatioso n withi nlarga e basin in Montana. Redd density varied widely across the basin; nearly all (99%) of the 362 redds observed occurred in two high-elevation headwater tributaries. Redd density at the reach scale s positivelwa y correlate 0.001= 0.72= 2 P ,d(r ) with abundanc f spawnino e g gravels. Other habitat variables, such as gradient, width, depth, embeddedness, bank stability, and percent riffle, were not significantly correlated to redd density. Taylor Fork redds contained some of the highest proportions of fine sediments (<6.35 mm, mean = 41.6%; <0.85 mm, 17.9%) observed in egg pocket salmonif so d Rocke reddth n si y Mountain region. Cache Creek highl,a y disturbed subbasin, d significantlha y greater proportion f fino s e sediments smaller tha reddn i n 0.8m s m 5tha e nth undisturbed Wapiti Creek subbasin. High fine-sediment level vero reddestimaten t w i s d ylo sle d embryo survival (mean, 8.5%) t sedimentatiobu , t appeano limid o t r di n t recruitment r datOu a. -
Influence of Water Temperature and Beaver Ponds on Lahontan Cutthroat Trout in a High-Desert Stream, Southeastern Oregon
AN ABSTRACT OF THE THESIS OF Andrew G. Talabere for the degree of Master of Science in Fisheries Science presented on November 21. 2002. Title: Influence of Water Temperature and Beaver Ponds on Lahontan Cutthroat Trout in a High-Desert Stream, Southeastern Oregon Abstract approved Redacted for Privacy Redacted for Privacy The distribution of Lahontan cutthroat trout Oncorhynchus clarki henshawi was assessed in a high-desert stream in southeastern Oregon where beaver Castor canadensis are abundant. Longitudinal patterns of beaver ponds, habitat, temperature, and Lahontan cutthroat trout age group distribution were identified throughout Willow Creek. Three distinct stream segments were classified based on geomorphological characteristics. Four beaver-pond and four free-flowing sample sections were randomly located in each of the three stream segments. Beavers substantially altered the physical habitat of Willow Creek increasing the depth and width of available habitat. In contrast, there was no measurable effect on water temperature. The total number of Lahontan cutthroat trout per meter was significantly higher in beaver ponds than free-flowing sections. Although density (fish! m2) showed no statistically significant (P < 0.05) increase, values in beaver pondswere two-fold those of free-flowing sections. Age- 1 and young-of-the-year trout were absent or in very low numbers in lower Willow Creek because of elevated temperatures, but high numbers of age-2 and 3 (adults) Lahontan cutthroat trout were found in beaver ponds where water temperatures reached lethal levels (>24°C). Apparently survival is greater in beaver ponds than free-flowing sections as temperatures approach lethal limits. Influence of Water Temperature and Beaver Ponds on Lahontan Cutthroat Trout in a High- Desert Stream, Southeastern Oregon by Andrew G.