March 2021 Litigation Report
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West Walker Watershed Management Plan
West Walker River Watershed Plan Management Plan March-2007 West Walker River Watershed Management Plan 1 Context Watershed approach California’s watershed programs and Mono County’s involvement Overview of issues and problems Problems linked to potential causes Water quantity Water quality Vegetation change Potential watershed problems and risks Knowledge and information gaps General principles of this watershed plan Main issues and potential solutions List of issues and solutions Potential problems of the future Recommended policies and programs List of goals, objectives, possible actions, and details Applicable best management practices Opportunities for governmental agencies and citizens groups Public education and outreach Monitoring Summary and conclusions Literature cited CONTEXT Watershed Approach The natural unit for considering most water-related issues and problems is the watershed. A watershed can be simply defined as the land contributing water to a stream or river above some particular point. Natural processes and human activities in a watershed influence the quantity and quality of water that flows to the point of interest. Despite the obvious connections between watersheds and the streams that flow from them, water problems are typically looked at and dealt with in an isolated manner. Many water West Walker River Watershed Management Plan 2 problems have been treated within the narrow confines of political jurisdictions, property boundaries, technical specialties, or small geographic areas. Many water pollution problems, flood hazards, or water supply issues have only been examined within a short portion of the stream or within the stream channel itself. What happens upstream or upslope has been commonly ignored. The so-called watershed approach merely attempts to look at the broad picture of an entire watershed and how processes and activities within that watershed affect the water that arrives at the defining point. -
Numaga Indian Days Pow Wow Enters Its 28Th Year
VOLUME IX ISSUE 12 August 22, 2014 Numaga Indian Days Pow Wow Enters Its 28th Year Hundreds expected for nationally known event held in Hungry Valley Each Labor Day weekend, the stunning handcrafted silver- from Frog Lake, Alberta Reno-Sparks Indian Colony work, beadwork, baskets and Canada. hosts its nationally acclaimed other American Indian art. Carlos Calica of Warm Numaga Pow Wow. This year, the 28th annual Springs, Oregon will serve as This family event features event, will be August 29-31 in the master of ceremonies, while some of the best Native Hungry Valley. Hungry Valley is the arena director will be Tom American dancers, singers and 19 miles north of downtown Phillips, Jr., from Wadsworth, drummers in the country. Reno and west of Spanish Nev. Besides the memorable pow Springs, nestled in scenic Eagle The Grand Entry will start wow entertainment, over 25 Canyon. at 7 p.m., on Friday, noon and vendors will be selling The host drum for this year‘s again at 7 p.m., on Saturday, traditional native foods and pow wow will be Young Spirit then at noon on Sunday. The pow wow is named after Chief Numaga, the famous Paiute Chief, known for peace. Chief Numaga was a great 19th century leader who had the courage and the vision to counsel against war. Facing severe threats to his people by invading white forces, Numaga repeatedly chose peace. His successful peace negotia- tions, helped set a precedent for future disputes. However, despite consistent calls for peace, an 1860 incident so severe forced Numaga to call for force. -
Walkerriverdecree.Pdf
Filed__________ 191W J IN EQUITY --___________, Clerk NO. C-125 By____________, Deputy IN THE DISTRICT COURT OF THE UNITED STATES OF AMERICA, IN AND FOR THE DISTRICT OF NEVADA UNITED STATES OF AMERICA, ~ t! Plainttff, ) ·vs- ( WALKER RIVER IRRIGATION l DISTRICT, a corporation, () et al, ) Defendants. ( ORDER FOR ENT::rl OF AttEHDED FINAL DECREE ~6----------'CONFD'RM"rT'OWRITOFMANDATE E'Tc.--:- The court entered its final decree in the above cause on the 15th day of April, 1936, and thereafter plaintiff having appealed, the United States Circuit Court of Appeals - Ninth Circuit - issued, on the 19th day of October, 1939, its Mandate, Order and Decree reversing in certain respects the trder and Decree of this Court entered herein, as aforesaid, on April 15, 1936, and Plaintiff having duly filed and noticed its Motion for an order directine the Clerk to file said Writ of Mandate and for an order amending said final Decree to conform with said \-lrit, and It appearing to the Court that plaintiff and defendants, through their respective attorneys, desire to clarify certain other provisions of the said Decree entered herein on April 15, 1936 as aforesaid, in order that the same will conform to the record, and ( Plaintiff and defendants, through their respec tive attorneys, having presented to this Court a stipulation in writing, s i gne d b y a 11 of the attorneys now of record, that the Court may enter the following ,Order, and good cause appearing therefor. IT IS ORDERED that the Clerk of this Court be, and he is hereby directed ,to file the Mandate, Order and Decree issued by the United States Circuit Court of Appeals - Ninth Circuit - on the 19th day of October, 1939 and received by the Clerk of this Court on October 22, 1939, and IT IS FURTHER ORDERED that page 10 of the final Decree of this Court entered herein on April 15, 1936, be and the same is hereby amended so as to read as follows: "argued before the Court in San Francisco, California and finally submitted on January 10, 1936. -
The Walker Basin, Nevada and California: Physical Environment, Hydrology, and Biology
EXHIBIT 89 The Walker Basin, Nevada and California: Physical Environment, Hydrology, and Biology Dr. Saxon E. Sharpe, Dr. Mary E. Cablk, and Dr. James M. Thomas Desert Research Institute May 2007 Revision 01 May 2008 Publication No. 41231 DESERT RESEARCH INSTITUTE DOCUMENT CHANGE NOTICE DRI Publication Number: 41231 Initial Issue Date: May 2007 Document Title: The Walker Basin, Nevada and California: Physical Environment, Hydrology, and Biology Author(s): Dr. Saxon E. Sharpe, Dr. Mary E. Cablk, and Dr. James M. Thomas Revision History Revision # Date Page, Paragraph Description of Revision 0 5/2007 N/A Initial Issue 1.1 5/2008 Title page Added revision number 1.2 “ ii Inserted Document Change Notice 1.3 “ iv Added date to cover photo caption 1.4 “ vi Clarified listed species definition 1.5 “ viii Clarified mg/L definition and added WRPT acronym Updated lake and TDS levels to Dec. 12, 2007 values here 1.6 “ 1 and throughout text 1.7 “ 1, P4 Clarified/corrected tui chub statement; references added 1.8 “ 2, P2 Edited for clarification 1.9 “ 4, P2 Updated paragraph 1.10 “ 8, Figure 2 Updated Fig. 2007; corrected tui chub spawning statement 1.11 “ 10, P3 & P6 Edited for clarification 1.12 “ 11, P1 Added Yardas (2007) reference 1.13 “ 14, P2 Updated paragraph 1.14 “ 15, Figure 3 & P3 Updated Fig. to 2007; edited for clarification 1.15 “ 19, P5 Edited for clarification 1.16 “ 21, P 1 Updated paragraph 1.17 “ 22, P 2 Deleted comma 1.18 “ 26, P1 Edited for clarification 1.19 “ 31-32 Clarified/corrected/rearranged/updated Walker Lake section 1.20 -
Mountain Whitefish Chances for Survival: Better 4 Prosopium Williamsoni
Mountain Whitefish chances for survival: better 4 Prosopium williamsoni ountain whitefish are silvery in color and coarse-scaled with a large and the mackenzie and hudson bay drainages in the arctic. to sustain whatever harvest exists today. mountain whitefish in California and Nevada, they are present in the truckee, should be managed as a native salmonid that is still persisting 1 2 3 4 5 WHITEFISH adipose fin, a small mouth on the underside of the head, a short Carson, and Walker river drainages on the east side of in some numbers. they also are a good indicator of the dorsal fin, and a slender, cylindrical body. they are found the sierra Nevada, but are absent from susan river and “health” of the Carson, Walker, and truckee rivers, as well as eagle lake. lake tahoe and other lakes where they still exist. Whitefish m Mountain Whitefish Distribution throughout western North america. While mountain whitefish are regarded aBundanCe: mountain whitefish are still common in populations in sierra Nevada rivers and tributaries have California, but they are now divided into isolated popula- been fragmented by dams and reservoirs, and are generally as a single species throughout their wide range, a thorough genetic analysis tions. they were once harvested in large numbers by Native scarce in reservoirs. a severe decline in the abundance of americans and commercially harvested in lake tahoe. mountain whitefish in sagehen and prosser Creeks followed would probably reveal distinct population segments. the lahontan population there are still mountain whitefish in lake tahoe, but they the construction of dams on each creek. -
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. -
Late Holocene Lake-Level Fluctuations in Walker Lake, Nevada, USA
Cleveland State University EngagedScholarship@CSU Biological, Geological, and Environmental Biological, Geological, and Environmental Faculty Publications Sciences Department 10-19-2006 Late Holocene Lake-Level Fluctuations in Walker Lake, Nevada, USA Fasong Yuan Cleveland State University, [email protected] Braddock K. Linsley University at Albany-State University of New York Stephen S. Howe University at Albany, State University of New York SteFollowve Pthis. Lund and additional works at: https://engagedscholarship.csuohio.edu/scibges_facpub University of Southern California Part of the Biology Commons JohnHow doesP. McGeehin access to this work benefit ou?y Let us know! PublisherU.S. Geological's SurStatementvey NOTICE: this is the author’s version of a work that was accepted for publication in Palaeogeography, Palaeoclimatology, Palaeoecology. Changes resulting from the publishing process, such as peer review, editing, corrections, structural formatting, and other quality control mechanisms may not be reflected in this document. Changes may have been made to this work since it was submitted for publication. A definitive version was subsequently published in Palaeogeography, Palaeoclimatology, Palaeoecology, [240, 3-4, (October 19, 2006)] DOI: 10.1016/j.palaeo.2006.03.003 Recommended Citation Yuan F, Linsley BK, Howe SS, Lund SP, McGeehin JP. 2006. Late Holocene lake-level fluctuations in alkW er Lake, Nevada, USA. Palaeogeogr , Palaeoclimatol , Palaeoecol. 240(3):497-507. This Article is brought to you for free and open access by the Biological, Geological, and Environmental Sciences Department at EngagedScholarship@CSU. It has been accepted for inclusion in Biological, Geological, and Environmental Faculty Publications by an authorized administrator of EngagedScholarship@CSU. For more information, please contact [email protected]. -
Robert C. Bryan, General Manager Walker River
Walker River Irrigation District ROBERT C. BRYAN, GENERAL MANAGER WALKER RIVER IRRIGATION DISTRICT (WRID) 410 N. MAIN ST YERINGTON, NV 89447 WRID Walker River Irrigation District (WRID) was formed in April 1919 under the authority of the Nevada Irrigation District Act, now NRS Chapter 539. WRID encompasses approximately 235,000 acres of which 80,000 are irrigated. WRID owns and operates two storage reservoirs; east fork storage is located in Bridgeport, CA and west fork storage is located at Topaz Reservoir, a bi-state facility. WRID operates and maintains extensive, approximately 200 miles, drainage systems in both Smith and Mason Valleys. WRID is an independent (not a Reclamation Project) irrigation district. WRID is governed by a 5-member Board of Directors. Directors are water right holders elected at Large, but must reside within a division of the district. They are elected to a four-year term. An elector of the district must own a water right. Bridgeport Reservoir • Bridgeport Reservoir was completed in the early 1920’s. • WRID storage right is recognized by a California water right license and by the Walker river Decree right. • Capacity of approximately 42,500 AF with refill rights. • Bridgeport Reservoir is also used extensively for recreation with fishing, boating and swimming. Topaz Reservoir • Topaz Reservoir was completed in the early 1920’s. • WRID storage right is recognized by a California water right license and in the Walker river Decree. • Capacity of approximately 59,000 AF with refill rights. • Topaz Reservoir is also used extensively for recreation with fishing, boating and swimming WRID Drains • Along with owning and operating Bridgeport and Topaz Reservoirs the District owns approximately 200 miles of drains. -
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. -
Walker Lake Tui Chub Genetics Report
1 Genomic Variation Laboratory Department of Animal Science University of California, Davis One Shields Avenue Davis, California 95616 Walker Lake Tui Chub Genetics Report Project Title: Genetic analysis of tui chub in Walker Lake, Nevada Contract: Task order 84240-9-J002; CESU 81332-5-G004 Grantee: University of California, Davis Authors: Amanda J. Finger and Bernie May Date: September 30, 2010 2 Executive Summary of Work This report details the research and findings of the Genomic Variation Laboratory (GVL) at the University of California, Davis, for Lahontan tui chubs (Siphateles bicolor pectinifer; Siphateles bicolor obesa) in Walker Lake, Nevada. Tui chubs in Walker Lake have experienced declines in recruitment as total dissolved salts (TDS) have increased over the last century. This work investigates how genetically differentiated the population in Walker Lake is relative to other populations of Lahontan tui chubs throughout the Walker, Carson and Truckee river basins. To assess the genetic diversity and the genetic distinctiveness of Lahontan tui chubs in Walker Lake, nine microsatellite loci were used to genotype tui chubs from Topaz Lake, NV, Little Soda Lake, NV, Pyramid Lake, NV, Spooner Lake, NV, Twin Lakes, CA, Tahoe Keys, CA, East Fork Walker River, CA and Stillwater National Wildlife Refuge, NV. Three additional populations from Nevada were analyzed for comparison: South Fork Reservoir, Independence Valley, and Dixie Valley. Funding in the amount of $40,000.00 was allocated by U.S. Fish and Wildlife Service-Lahontan National Fish Hatchery Complex to complete two objectives: 1) use genetic data to determine if the population of tui chubs in Walker Lake is genetically distinct and 2) identify a suitable source population for tui chub if it is necessary to create refugial populations. -
Late Holocene Paleohydrology of Walker Lake and the Carson Sink in the Western Great Basin, Nevada, USA
Quaternary Research Copyright © University of Washington. Published by Cambridge University Press, 2019. doi:10.1017/qua.2018.151 Late Holocene paleohydrology of Walker Lake and the Carson Sink in the western Great Basin, Nevada, USA Kenneth D. Adamsa*, Edward J. Rhodesb aDivision of Earth and Ecosystem Sciences, Desert Research Institute, 2215 Raggio Parkway, Reno, Nevada 89512, USA bDepartment of Geography, University of Sheffield, Sheffield, S10 2TN, United Kingdom *Corresponding author e-mail address: [email protected] (RECEIVED June 8, 2018; ACCEPTED December 6, 2018) Abstract The late Holocene histories of Walker Lake and the Carson Sink were reconstructed by synthesizing existing data in both basins along with new age constraints from key sites, supplemented with paleohydrologic modeling. The repeated diversions of the Walker River to the Carson Sink and then back to Walker Lake caused Walker Lake–level fluctuations spanning ± 50 m. Low lake levels at about 1000, 750, and 300 cal yr BP are time correlative to the ages of fluvial deposits along the Walker River paleochannel, when flow was directed toward the Carson Sink. The timing and duration of large lakes in the Carson Sink were further refined using moisture-sensitive tree-ring chronologies. The largest lakes required a fourfold to fivefold increase in discharge spanning decades. Addition of Walker River flow to the Carson Sink by itself is inadequate to account for the required discharge. Instead, increases in the runoff coefficient and larger areas of the drainage basin contributing surface runoff may explain the enhanced discharge required to create these large lakes. Keywords: Carson Sink; Holocene; Lake Lahontan; Paleohydrologic modeling; Walker Lake INTRODUCTION of the Walker River, which periodically switched course from one terminal basin to the other (Russell, 1885; Benson and Paleohydrologic records from Great Basin pluvial lakes pro- Thompson, 1987a, 1987b; Benson et al., 1991; King, 1993, vide a rich source of information enhancing understanding of 1996; Adams, 2003, 2007). -
Life History of the Lahontan Cutthroat Trout, Salmo Clarki Henshawi, in Pyramid Lake, Nevada
Great Basin Naturalist Volume 43 Number 1 Article 1 1-31-1983 Life history of the Lahontan cutthroat trout, Salmo clarki henshawi, in Pyramid Lake, Nevada William F. Sigler W. F. Sigler and Associates, Inc., Logan, Utah William T. Helm Utah State University Paul A. Kucera Nez perce Tribe, Lapwai, Idaho Steven Vigg University of Nevada System, Reno Gar W. Workman Utah State University Follow this and additional works at: https://scholarsarchive.byu.edu/gbn Part of the Anatomy Commons, Botany Commons, Physiology Commons, and the Zoology Commons Recommended Citation Sigler, William F.; Helm, William T.; Kucera, Paul A.; Vigg, Steven; and Workman, Gar W. (1983) "Life history of the Lahontan cutthroat trout, Salmo clarki henshawi, in Pyramid Lake, Nevada," Great Basin Naturalist: Vol. 43 : No. 1 , Article 1. Available at: https://scholarsarchive.byu.edu/gbn/vol43/iss1/1 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 Brigham Young University ISSN 0017-3614 Volume 43 January 31, 1983 No. 1 LIFE HISTORY OF THE LAHONTAN CUTTHROAT TROUT, SALMO CLARKI HENSHAWI, IN PYRAMID LAKE, NEVADA William F. Sigler', William T. Helm^ Paul A. Kucera\ Steven Vigg*, and Gar W. Workman' Abstract.— The Pyramid Lake Lahontan cutthroat trout (Salmo clarki henshawi) population was sampled on a monthly basis from November 1975 through December 1977.