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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. -
Cui-Ui Recovery Plan
1 ESA 81 RECOVERY PLAN DRAWING BY: JOSETTECUILEY I CUI-UI RECOVERY PLAN Prepared by the Cui-ui Recovery Team December 1977 TEAM MEMBERS Earl Pyle, Team Leader, U.S. Fish and Wildlife Service, Reno, Nevada John Frazier, Pyramid Lake Paiute Indian Tribe, Nixon, Nevada Donald King, U.S. Fish and Wildlife Service, Reno, Nevada Kay Johnson, Nevada Department of Fish and Game, Reno, Nevada Dale Lockard, Nevada Department of Fish and Game, Reno, Nevada Thomas J.. Trelease, Team Advisor, Verdi , Nevada Published by U.S. Fish and Wildlife Service Endangered Species Program Region 1 Portland, Oregon Approved Director, U.S. Fish & Wildlife Service Title Date TABLE OF CONTENTS Page PART I. INTRODUCTION .................. 1 Former Status ................. 2 Reasons for Decline of the Fishery ....... 3 Figure 1 .................... 4 PART II . THE RECOVERY PLAN ............... Objectives and Rationale ............ Accomplishments ................ Specific Problem Areas ............. Recovery Plan Out1 ine ............. Action Diagram ................. Action Narrative ................ PART I11 . SCHEDULE OF PRIORITIES. RESPONSIBILITIES & COSTS APPENDIX A . REFERENCES CITED ................ APPENDIX B . PROPOSED ESSENTIAL HABITAT ........... Maps . Proposed Essential Habitat ....... APPENDIX C . LETTERS OF COMMENT ............... CUI-UI RECOVERY PLAN PART I INTRODUCTION The history of the cui-ui 1 (Chasmistes cujus) and the Pyramid Lake Paiute Indian Tribe is so intimately entwined that the unwritten, ancestral name for the tribe is Kuyuidokado (Wheeler, 1969) or Ku-yu-wi-kut-teh (Hermann, 1973) meaning "sucker eaters". Spawning runs of cui-ui and cutthroat trout (mclarki provided a readily available and dependable source of food. There can be no doubt the shores of Pyramid Lake were highly val- ued as a haven against the uncertainty and hardship of obtaining food in the arid and often inhospitable lands of the Great Basin. -
Truckee River 2007
NEVADA DEPARTMENT OF WILDLIFE STATEWIDE FISHERIES MANAGEMENT FEDERAL AID JOB PROGRESS REPORT F-20-54 2018 TRUCKEE RIVER WESTERN REGION NEVADA DEPARTMENT OF WILDLIFE, FISHERIES DIVISION ANNUAL PROGRESS REPORT Table of Contents SUMMARY ................................................................................................................... 1 BACKGROUND .............................................................................................................. 1 OBJECTIVES .................................................................................................................. 3 PROCEDURES ............................................................................................................... 3 FINDINGS ................................................................................................................... 5 MANAGEMENT REVIEW ............................................................................................. 17 RECOMMENDATIONS ................................................................................................. 18 NEVADA DEPARTMENT OF WILDLIFE, FISHERIES DIVISION ANNUAL PROGRESS REPORT State: Nevada Project Title: Statewide Fisheries Program Job Title: Truckee River Period Covered: January 1, 2018 through December 31, 2018 SUMMARY On April 1, 2018, the designated end of the snow-measuring season, the snowpack in the Truckee River Basin stood at 75% of the median for that date and the amount of precipitation for the year stood at 90% of average. While the 2017/18 winter was slightly -
Life History of the Cui-Ui, Chasmistes Cujus Cope, in Pyramid Lake, Nevada: a Review
Great Basin Naturalist Volume 45 Number 4 Article 1 10-31-1985 Life history of the cui-ui, Chasmistes cujus Cope, in Pyramid Lake, Nevada: a review William F. Sigler W.F. Sigler and Associates Inc., Logan, Utah Steven Vigg University of Nevada, Reno Mimi Bres George Washington University, Washington, D.C. Follow this and additional works at: https://scholarsarchive.byu.edu/gbn Recommended Citation Sigler, William F.; Vigg, Steven; and Bres, Mimi (1985) "Life history of the cui-ui, Chasmistes cujus Cope, in Pyramid Lake, Nevada: a review," Great Basin Naturalist: Vol. 45 : No. 4 , Article 1. Available at: https://scholarsarchive.byu.edu/gbn/vol45/iss4/1 This Article is brought to you for free and open access by the Western North American Naturalist Publications at BYU ScholarsArchive. It has been accepted for inclusion in Great Basin Naturalist by an authorized editor of BYU ScholarsArchive. For more information, please contact [email protected], [email protected]. The Great Basin Naturalist Published AT Provo, Utah, by Bricham Young University ISSN 0017-3614 Volume 45 31 October 1985 No. 4 LIFE HISTORY OF THE CUI-UI, CHASMISTES CUJUS COPE, IN PYRAMID LAKE, NEVADA: A REVIEW William F". Sigler', Steven Vigg", and Minii Bres' Abstract—The cui-ui, Chasmistcs ciijus Cope, a member of the .sucker family and endemic to Pyramid Lake, Nevada, is listed as endangered by the U.S. Fish and Wildlife Service. Cui-ui was once a major source of sustenance for native Americans, who have inhabited the Lahontan region for at least 11,000 years. The Northern Paiutes developed sophisticated fishing technology to harvest this resource. -
Water Budget and Salinity of Walker Lake,Western Nevada
ENT OF T TM H R E A IN P E T E D U.S. Geological Survey Water Budget and Salinity of R I O S. Fact Sheet FS-115-95 R U. G Walker Lake,Western Nevada E Y O E L V O R GICAL SU Walker Lake (fig. 1) is one of the rare although this site does not have the In some valleys, local streams also perennial, terminal lakes in the Great longest streamflow record, no upstream contribute surface-water flow. Thus, Basin of the western United States. The reservoirs or irrigation diversions exist and estimates of surface-water consumption in lake is the terminus for all surface-water streamflow has been measured contin- table 2 are minimum values, because local and ground-water flow in the Walker uously at the site since 1939. Long-term streamflow in valleys may not have been River Basin Hydrographic Region (fig. 2) average annual flows were estimated by measured. In Smith Valley, 8,700 acre- that is not consumed by evaporation, comparing the average annual flow at a ft/yr of Desert Creek flow has been in- sublimation, or transpiration. stream-gaging station with the average cluded in the water budget. In Antelope annual flow at site 4 for years of concur- Valley, the contribution from Mill and The concentration of dissolved solids rent record. Then, this partial record was Slinkard Creeks is unknown, so the difference of 15,000 acre-ft between (salts) in the lake and the lake-surface adjusted to a long-term average using the average inflow and outflow underesti- altitude fluctuate primarily in response 55-year average at site 4. -
Pyramid Lake Watercraft Inspection Station Environmental Assessment LO-2014-1035
Pyramid Lake Watercraft Inspection Station Environmental Assessment LO-2014-1035 U.S. Department of the Interior Bureau of Reclamation Lahontan Basin Area Office 705 North Plaza Street, Room 320 Carson City, Nevada 89701 Mission Statements The mission of the Department of the Interior is to protect and provide access to our Nation’s natural and cultural heritage and honor our trust responsibilities to Indian Tribes and our commitment to island communities. The mission of the Bureau of Reclamation is to manage, develop, and protect water and related resources in an environmentally and economically sound manner in the interest of the American public. Table of Contents Section 1 Introduction ..........................................................................................................1 1.1 Background ....................................................................................................................1 Pyramid Lake Reservation ...................................................................................................1 Pyramid Lake Fisheries Department ....................................................................................1 Anaho Island ........................................................................................................................1 Aquatic Invasive Species .....................................................................................................2 Environmental Assessment ..................................................................................................4 -
Salinity of Nevada's Terminal Lakes: History, Mystery, and Restoration
Salinity of Nevada’s Terminal Lakes: History, Mystery, and Restoration Kip K. Allander; Supervisory Hydrologist; NV Water Science Center ([email protected]) 2020 MSSC Summit: February 27, 2020, Las Vegas NV Nevada’s Remnants of Lake Lahontan Pyramid Lake Winnemucca Lake Benson (2013) Walker Lake Trump (2004) Pacific Flyway USFWS Fisheries USFWS Indigenous People and Culture Cui-Ui Dicutta Numu (Pyramid Lake Paiute Tribe) Problem with Terminal Lakes. Salinity is highly sensitive to changes in storage. Truckee, Carson, Walker River systems Trionfante and Peltz (1993) Geologic Investigation by Israel C. Russell 1882 - 1883 USGS Russell (1885) Historic Lake Levels Pyramid Lake Walker Lake Winnemucca Lake Pyramid and Winnemucca Lakes Mud Slough Sill Russell (1885) Major events effecting water supply of Pyramid Lake Mud Slough Sill Pyramid Lake 1903 – 1915 Newlands Project Winnemucca Lake Newlands Project USBR (Simpson and others, 2015) Major events effecting water supply of Pyramid Lake Pyramid Lake 19671973 GeselleOCAPopinion & Endangered Species Act Winnemucca Lake Walker Lake Russell (1885) Major events effecting water supply of 1922 - 1924 Walker Lake Bridgeport and Topaz Reservoirs 20092019 LastRestoration LCT caught flows begin 1860 – 1920 Upstream agriculture is established Walker Lake Salinity Effects on Key Indicator Species The Nature Conservancy (2013) Restoration targets: 12,000 mg/L TDS; 3,951 foot level Walker Basin Hydro Mapper https://webapps.usgs.gov/walkerbasinhydromapper Walker Lake and the Mystery of the Missing Salt Walker -
Life History and Status of the Endangered Cui-Ui of Pyramid Lake, Nevada
Fish and Wildlife Research 1 Life History and Status of the Endangered Cui-ui of Pyramid Lake, Nevada By G. Gary Scoppettone Mark Coleman Gary A. Wedemeyer UNITED STATES DEPARTMENT OF THE INTERIOR FISH AND WILDLIFE SERVICE Washington, D.C. • 1986 Contents Page Abstract ................................................................................................................................... 1 Study Area .............................................................................................................................. 3 Spawning Migration ............................................................................................................ Prespawning Aggregation ............................................................................................. History of Recent Spawning Migrations ............................................................... 6 Upstream Migration ....................................................................................................... Reproduction ......................................................................................................................... 8 Fecundity ............................................................................................................................ 9 Spawning Habitat ............................................................................................................. 9 Emigration of Larvae .......................................................................................................... 10 Timing of -
COE Feasibility Level Fish Bypass Design at Marble Bluff Dam
Hydraulic Laboratory Report HL-2011-01 COE Feasibility Level Fish Bypass Design at Marble Bluff Dam Subtitle, 16 pt Arial, Bold (optional…consider if title is very long) Optional Auxiliary Text, and/or photograph, or leave blank (13 pt Arial, Bold) Visual Identity program requires photographs to align with a 6-column grid layout which uses 1 inch columns and 0.2 inch gutters. Left edge of photo should be placed on left edge of one of the 6 columns (i.e., at 0, 1.2, 2.4, 3.6, 4.8, 6.0 inches from left margin), and the right edge should be on the right edge of one of the 6 columns (1.0, 2.2, 3.4, 4.6, 5.8, or 7.0 inches from left margin). A transparent template can assist in laying out photos. Margins of this page should be 0.5 inches top and bottom, 0.75 inches left and right. This form has the grid overlay on it. To remove it, use the Format | Background | Printed Watermark command and select No watermark. You will not be able to restore it once it is removed (except by using Undo). U.S. Department of the Interior Bureau of Reclamation Technical Service Center Hydraulic Investigations and Laboratory Services Group Denver, Colorado April 2011 Form Approved REPORT DOCUMENTATION PAGE OMB No. 0704-0188 The public reporting burden for this collection of information is estimated to average 1 hour per response, including the time for reviewing instructions, searching existing data sources, gathering and maintaining the data needed, and completing and reviewing the collection of information. -
Hydrologic Fluctuations at Pyramid Lake, Walker Lake, and the Carson Sink, Nevada During the Medieval Climate Anomaly
HYDROLOGIC FLUCTUATIONS AT PYRAMID LAKE, WALKER LAKE, AND THE CARSON SINK, NEVADA DURING THE MEDIEVAL CLIMATE ANOMALY KENNETH D. ADAMS Desert Research Institute, 2215 Raggio Parkway, Reno, NV 89512 [email protected] Lake levels in the western Great Basin have fluctuated throughout the Holocene in response to changes in the hydrologic balance of their watersheds. The magnitudes of lake-level fluctuations are not only based on changes in climate but are also controlled by the hypsometries of individual basins, the presence and elevations of surrounding sills, and in the case of Walker Lake, through river diversions. This presentation focuses on the lake-level histories of Walker Lake, the Carson Sink, and Pyramid Lake through the Medieval Climate Anomaly (MCA; A.D. 900-1350), a time period characterized by severe and sustained droughts as well as periods wetter than modern. Although not as temporally precise as tree-ring studies, lake-level histories help discern the severity of droughts as well as the magnitude of wet periods. Despite differences in hydrology, hypsometry, and the effects of sills, there are commonalities in the three records. Walker Lake was low at A.D. 950 (<1,205 m), A.D. 1150 (<1,224 m), and at A.D. 1650 (<1,215 m). The first and last of these low periods, however, are associated with evidence for diversion of the Walker River into the Carson Sink. Walker Lake also reached relative highstands at about A.D. 1030 (~1,245m) and A.D. 1290 (~1,255 m), the latter level being several meters above the historic highstand (A.D. -
AN OPERATIONS MODEL for TEMPERATURE MANAGEMENT of the TRUCKEE RIVER ABOVE RENO, NEVADA by DAVID W
AN OPERATIONS MODEL FOR TEMPERATURE MANAGEMENT OF THE TRUCKEE RIVER ABOVE RENO, NEVADA by DAVID W. NEUMANN B.S., University of Colorado, 2001 A thesis submitted to the University of Colorado in partial fulfillment of the requirement for the degree of Master of Science Department of Civil, Environmental, and Architectural Engineering 2001 This thesis entitled: AN OPERATIONS MODEL FOR TEMPERATURE MANAGEMENT OF THE TRUCKEE RIVER ABOVE RENO, NEVADA written by David W. Neumann has been approved for the Department of Civil, Environmental, and Architectural Engineering Rajagopalan Balaji Edith Zagona Date The final copy of this thesis has been examined by the signators, and we find that both the content and the form meet acceptable presentation standards of scholarly work in the above mentioned discipline. Neumann, David (M.S., Civil, Environmental, and Architectural Engineering) An Operations Model for Temperature Management of the Truckee River above Reno, NV Thesis directed by Edith Zagona and Assistant Professor Rajagopalan Balaji This thesis develops and presents a decision support system (DSS) to manage the temperature of the Truckee River at Reno, Nevada. Warm summer river tempera- tures adversely affect threatened and endangered fish. Water rights are anticipated to be purchased by the federal government and local entities as part of the Water Quality Settlement Agreement (WQSA). The acquired water will be stored in upstream reser- voirs and released to improve downstream water quality. The DSS implements an empirical model to predict maximum daily Truckee River water temperatures in June, July and August given predicted maximum daily air temperature and modeled average daily flow. The empirical model (R2 = 0.9) is cre- ated using a step-wise linear regression selection process using 1993 and 1994 data. -
The Tufas of Pyramid Lake, Nevada
Prepared in cooperation with the Pyramid Lake Paiute Tribe and the Pyramid Lake Museum Visitor Center The Tufas of Pyramid Lake, Nevada U.S. Geological Survey Circular 1267 U.S. Department of the Interior U.S. Geological Survey The Tufas of Pyramid Lake, Nevada By Larry Benson Prepared in cooperation with the Pyramid Lake Paiute Tribe and the Pyramid Lake Museum Visitor Center U.S. Geological Survey Circular 1267 U.S. Department of the Interior U.S. Geological Survey ii U.S. Department of the Interior Gale A. Norton, Secretary U.S. Geological Survey Charles G. Groat, Director U.S. Geological Survey, Reston, Virginia, 2004 Free on application to: U.S. Geological Survey, Information Services Box 25286, Denver Federal Center Denver, CO 80225 For more information about the USGS and its products: Telephone: 1-888-ASK-USGS World Wide Web: http://www.usgs.gov/ Any use of trade, product, or firm names in this publication is for descriptive purposes only and does not imply endorsement by the U.S. Government. Suggested citation: Benson, L.V., 2004, The Tufas of Pyramid Lake, Nevada: U.S. Geological Survey Circular 1267, 14p. Library of Congress Cataloging-in-Publication Data Benson, Larry V. The tufas of Pyramid Lake, Nevada I by Larry Benson p. em/ -- (U.S. Geological Survey circular ; 1267) "Prepared in cooperation with the Pyramid Lake Paiute Tribe and the Pyramid Lake Museum Visitor Center." ISBN 0-607-97555-5 (alk. paper) 1. Rocks, Carbonate--Nevada--Pyramid Lake. 2. Calcium carbonate--Nevada--Pyramid Lake. 3. Geology, Stratigraphic--Quaternary. 4. Geology--Nevada--Pyramid Lake.