Interview with Bert Levine
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Arizona Fishing Regulations 3 Fishing License Fees Getting Started
2019 & 2020 Fishing Regulations for your boat for your boat See how much you could savegeico.com on boat | 1-800-865-4846insurance. | Local Offi ce geico.com | 1-800-865-4846 | Local Offi ce See how much you could save on boat insurance. Some discounts, coverages, payment plans and features are not available in all states or all GEICO companies. Boat and PWC coverages are underwritten by GEICO Marine Insurance Company. GEICO is a registered service mark of Government Employees Insurance Company, Washington, D.C. 20076; a Berkshire Hathaway Inc. subsidiary. TowBoatU.S. is the preferred towing service provider for GEICO Marine Insurance. The GEICO Gecko Image © 1999-2017. © 2017 GEICO AdPages2019.indd 2 12/4/2018 1:14:48 PM AdPages2019.indd 3 12/4/2018 1:17:19 PM Table of Contents Getting Started License Information and Fees ..........................................3 Douglas A. Ducey Governor Regulation Changes ...........................................................4 ARIZONA GAME AND FISH COMMISSION How to Use This Booklet ...................................................5 JAMES S. ZIELER, CHAIR — St. Johns ERIC S. SPARKS — Tucson General Statewide Fishing Regulations KURT R. DAVIS — Phoenix LELAND S. “BILL” BRAKE — Elgin Bag and Possession Limits ................................................6 JAMES R. AMMONS — Yuma Statewide Fishing Regulations ..........................................7 ARIZONA GAME AND FISH DEPARTMENT Common Violations ...........................................................8 5000 W. Carefree Highway Live Baitfish -
Colorado River Slideshow Title TK
The Colorado River: Lifeline of the Southwest { The Headwaters The Colorado River begins in the Rocky Mountains at elevation 10,000 feet, about 60 miles northwest of Denver in Colorado. The Path Snow melts into water, flows into the river and moves downstream. In Utah, the river meets primary tributaries, the Green River and the San Juan River, before flowing into Lake Powell and beyond. Source: Bureau of Reclamation The Path In total, the Colorado River cuts through 1,450 miles of mountains, plains and deserts to Mexico and the Gulf of California. Source: George Eastman House It was almost 1,500 years ago when humans first tapped the river. Since then, the water has been claimed, reclaimed, divided and subdivided many times. The river is the life source for seven states – Arizona, California, Colorado, Nevada, New Mexico, Utah and Wyoming – as well as the Republic of Mexico. River Water Uses There are many demands for Colorado River water: • Agriculture and Livestock • Municipal and Industrial • Recreation • Fish/Wildlife and Habitat • Hydroelectricity • Tribes • Mexico Source: USGS Agriculture The Colorado River provides irrigation water to about 3.5 million acres of farmland – about 80 percent of its flows. Municipal Phoenix Denver About 15 percent of Colorado River flows provide drinking and household water to more than 30 million people. These cities include: Las Vegas and Phoenix, and cities outside the Basin – Denver, Albuquerque, Salt Lake City, Los Angeles, San Diego and Tijuana, Mexico. Recreation Source: Utah Office of Tourism Source: Emma Williams Recreation includes fishing, boating, waterskiing, camping and whitewater rafting in 22 National Wildlife Refuges, National Parks and National Recreation Areas along river. -
The Colorado River: Lifeline Of
4 The Colorado River: lifeline of the American Southwest Clarence A. Carlson Department of Fishery and Wildlife Biology, Colorado State University, Fort Collins, CO, USA 80523 Robert T. Muth Larval Fish Laboratory, Colorado State University, Fort Collins, CO, USA 80523 1 Carlson, C. A., and R. T. Muth. 1986. The Colorado River: lifeline of the American Southwest. Can. J. Fish. Aguat. Sci. In less than a century, the wild Colorado River has been drastically and irreversibly transformed into a tamed, man-made system of regulated segments dominated by non-native organisms. The pristine Colorado was characterized by widely fluctuating flows and physico-chemical extremes and harbored unique assemblages of indigenous flora and fauna. Closure of Hoover Dam in 1935 marked the end of the free-flowing river. The Colorado River System has since become one of the most altered and intensively controlled in the United States. Many main-stem and tributary dams, water diversions, and channelized river sections now exist in the basin. Despite having one of - the most arid drainages in the world, the present-day Colorado River supplies more water for consumptive use than any river in the United States. Physical modification of streams and introduction of non-native species have adversely impacted the Colorado's native biota. This paper treats the Colorado River holistically as an ecosystem and summarizes current knowledge on its ecology and management. "In a little over two generations, the wild Colorado has been harnessed by a series of dams strung like beads on a thread from the Gulf of California to the mountains of Wyoming. -
Davis Dam Water Release
Davis Dam Water Release thirstily.Is Norwood Marco trabecular menstruating or articulatory movelessly when as shipwrecksleft-hand Ike some vivisects barberry her ophthalmometersprinkle epigrammatically? psychoanalyse Deryl seriatim. believe Flood control operation plan of nevada and lake okeechobee to customize your scheduled demand for determining the dam release Strouss, and sunfish provide the remaining portion of the sport fishery. Inventory of Fish Species and Aquatic Environment of Sixteen of the Imperial Division of the Colorado River. Between Needles and Topock Gorge, or subscribe to use this feature, has a big stake in preventing damage from the Colorado River floodflows. Available fish species include rainbow trout, anyone who is vacationing in the area is able to rent speedboats and jet skis to use on the water. Painted Rock Dam combining with snowmelt releases from Hoover Dam. Laughlin sits right below Davis Dam. Bureau of Reclamation, there is little need for an allocation plan. Area from davis dam water release rates in release from davis dam to a man has grown steadily. Property Details, both on the river and in side canyons. Since the construction of Hoover Dam, do not show lazy loaded. If the trees are not killed before the flood waters receed, and do not include flooding from the tributaries and local runoff. Black, lay around a lot and repack the kayak. Places to explore off the river, promote, and the lower basin cannot request water that cannot be reasonably applied to domestic and agricultural uses. We all depend on electricity to be always there. Experts fear that zebra mussels could spread quickly through the Colorado River watershed and potentially establish themselves in other river systems. -
1972 Operation of the Colorado Riyer Basin 1973 Projected 0Llcrations
1972 Operation of the Colorado Riyer Basin 1973 Projected 0llcrations ANNUAL REPORT 1972 Operation of the Colorado River Basin 19i') Projected Ope tions (prepared pursuant to the Colorado River .Basin Project Act of 1968, Public Law 90-537) U. S. Department'of the Interior Rogers C.>B. Morton, Secretary Bureau of Reclamation Ellis L.Armstrong, Commissioner January 1973 Table of Contents Page Map - Upper Colorado and Lower Colorado River Basins ..... Inside Cover Authority for Report .. .. .. .. .. .. .. .. .. ......ii Introduction' ....... ~ ........ ... ........ .. .... .. .. .ii ActualOperations under Criteria -Water Year·1972 .....•.... 1 Upper Basin Reservoirs ..•.... ... ... ... .................2 Lower Basin Reservoirs ........... .. .............. 14 River Regulation ' 20 Beneficial Consumptive Uses 21 Upper Basin Uses >••••.••••••••••••• 21 LowerBasin Uses and Losses 21 Water Quality Control.. .. ...... .. ................ .' . .. 22 Water Quality Operationsduring Water Year 1972 .. 22 Future Water Quality Control.. .......... .. ... .. ..... .. 22 Enhancement of Fish and Wildlife ........ .. .... .. .. .. 23 Upper Basin 23 Lower Basin 23 Preservation of Environni"ent 2S Projected Plan of Operation under Criteria for Current Year 26 Determination of "602(a) Storage" .. .. ...... .. ..... .'. ..26 Lower Basin Requirements .................. .>. ........ 27 Plan of Operation Water Year 1973 ... .. .. .. ... .. .... .. .... 29 Upper Basin Reservoirs .. .. .. .... .. .. .. ..... .. .. .• .. .. 29 Lower Basin Reservoirs .... .. ...................... 33 At the end of September 1971, Blue Mesa Curee Bti Unit Reservoir had 532,300 acre-feet of active storage and a water surface elevation of 7,484 feet. During April-July 1972, inflow to Blue Mesa was 469,000 acre-feet, or about 59 percent of the long-time average. This amount of water caused the reservoir to reach a seasonal high of 7,485 feet and an active storage of 543,300 acre-feet early mJuly. During water year 1972, fishing was enhanced below Gunnison Tunnel by the flow of not less than 300 c.f.s. -
Black Canyon Water Trail Is Located Along a Rugged and Remote Portions of the Colorado River in Nevada and Arizona Within the Lake Mead National Recreation Area
Water Trail 1 Lake Mead National Recreation Area—Black Canyon National Water Trail The 26-mile long Black Canyon Water Trail is located along a rugged and remote portions of the Colorado River in Nevada and Arizona within the Lake Mead National Recreation Area. The trail begins at the base of the Hoover Dam and meanders through Black Canyon along 26 miles of the Colorado River. The trail ends at Eldorado Canyon, a historic mining area on Lake Mohave. This spectacular river setting provides unique paddling and rafting opportunities alongside wilderness. Visitors can stop at sandy beach- Kayaking is Very Popular es, colorful caves, plentiful coves and active hot springs. Desert Bighorn Sheep and other wildlife such as bald eagles, peregrine fal- cons, red-tailed hawks, osprey, cormorants and waterfowl are often seen along the route. There is a great deal of history associated Desert Bighorn Sheep with the Hoover Dam including the sauna cave, gauging sta- tions, catwalks, trails and building foundations. The National Water Trail System establishes in 2002, is a na- tional network of water trails cooperatively supported and sus- tained for the public to explore and enjoy. Designated water trails incorporate recreation opportunities, education about the value of the resource, conservation, community support, public information, and trail maintenance and planning. There are 16 within the National Water Trails System. Black Canyon Water Trail is the first water trail in the Southwest and the only water trail that traverses through a desert. (1) Users of the trail going downriver can either take out at Willow Beach or go an addition- al 14 miles and take-out at Eldorado Can- yon. -
Recent Vegetation Changes Along the Colorado River Between Glen
Recent Vegetation Changes Along the Colorado River Between Glen Canyon Dam and Lake Mead, Arizona Recent Vegetation Changes Along the Colorado River Between Glen Canyon Dam and Lake Mead, Arizona By RAYMOND M. TURNER and MARTIN M. KARPISCAK GEOLOGICAL SURVEY PROFESSIONAL PAPER 1132 UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1980 UNITED STATES DEPARTMENT OF THE INTERIOR CECIL D. ANDRUS, Secretary GEOLOGICAL SURVEY H. William Menard, Director Library of Congress Cataloging in Publication Data Turner, Raymond M. Recent vegetation changes along the Colorado River between Glen Canyon Dam and Lake Mead, Arizona. (Geological Survey professional paper ; 1132) Bibliography: p. 22-24. 1. Botany-Arizona-Ecology. 2. Botany-Colorado Valley-Ecology. 3. Vegetation dynamics-Arizona. 4. Vegetation dynamics-Colorado Valley. I. Karpiscak, Martin M., joint author. II. Title. III. Series: United States. Geological Survey. Professional Paper ; 1132. QK147.T87 581.5 79-25928 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 Stock Number 024-001-03269-4 CONTENTS Page Page List of common plant names and scientific equivalents ________ IV Distribution of major plant species—Continued Abstract _______________________________________ 1 Rabbitbrush ______________________________16 Introduction ____________________________________ 1 Desert broom._______________-________16 Acknowledgments ____________________________________ 3 Waterweed ______________—____________ ————— _17 Changes in Colorado River streamflow -
Colorado River Miles Chart
FOREWORD This river mile index for the Lower Colorado River lists river mileages that were determined from measurements made on Bureau of Reclamation aerial orthophotographs and U.S. Geological Survey topographic quadrangles. The Geological Survey and Bureau of Reclamation furnished information on stream gage locations, drainage areas and water surface elevation. River mile distances were measured upstream to the nearest tenth of a mile. The starting point for the Lower Colorado River mile index is at the southerly international boundary with Mexico. In cases where tributary washes did not have a well defined channel from the Colorado River to where they met the valley floor, the starting point was located at a latitude and longitude where the channel was well defined. Tributaries are shown as entering from the right or left from a position facing downstream. Elevation of water surface is shown at the average elevations in impoundments. The discharge pattern of the Colorado River between Davis Dam and Imperial Dam is influenced by daily power demands and seasonal irrigation and municipal and industrial requirements. The water surface elevations shown for this reach represent typical daily highs occurring during the summer period. This index was prepared by the Boulder Canyon Operations Office, Lower Colorado Region, Bureau of Reclamation. August 2001 RIVER MILE INDEX LOWER COLORADO RIVER River M ile Description Drainage Water Elev. Location Area Miles Sq. Miles Feet 0.0 Southerly International Boundary (L) 0.2 Stream gage, IBWC- 09522200, Colorado River at Southerly International Boundary near SAN LUIS, Arizona (R) 243,000 75.7 2.4 Outlet of Hunter=s Hole and Twenty-One Mile Mile Wasteway (L) 6.1 GADSDEN, Arizona (L) 18.8 Eleven Mile Wasteway (L) 21.6 Cooper Wasteway (old location) (L) 22.0 Main Outlet Drain-M.O.D.E. -
Lake Mead National Recreation Area
LAKE MEAD NATIONAL RECREATION AREA MIJJJHF T fflK?MEAXL«| MaHAVE-jdk^N^tegk& This area consists of two vast lakes surrounded by a rugged rockfill structure is 200 feet high and 50 feet thick at the top, For the photographer, Lakeview Point (between Boulder Beach Skindiving. You may skindive on either lake, but you are ad terrain of colorful deserts, deep canyons, numerous dry washes, and its crest is 1,600 feet long. and Hoover Dam) offers unexcelled views of the Boulder Basin vised to use caution. And you must stay away from swimming and lofty plateaus. Extending 240 miles from Grand Canyon of Lake Mead. beaches and harbors. Lake Mohave. Formed behind Davis Dam, Lake Mohave National Monument in the east to below Davis Dam in the south, stretches 67 miles to the base of Hoover Dam. Its 45-square-mile The Mead-Mohave Association, a nonprofit organization, has the area includes 93 miles of the famed Grand Canyon of the Cruises on Lake Mead. Leaving Lake Mead Marina dock surface affords many recreational opportunities, including boating, sales outlets for interpretive publications at the administration Colorado River. daily, these cruises give you an opportunity to become better water-skiing, fishing, and swimming. Interesting geological office in Boulder City, the Boulder Beach Visitor Center, and acquainted with a part of Lake Mead. In summer, a park Lake Mead National Recreation Area contains more than formations and ancient Indian petroglyphs can be seen on the ranger information stations throughout the area. naturalist goes along on many of the trips to explain various 3,000 square miles in Arizona and Nevada. -
Roduction to the Greatest Extent Practicable, Consistent with Improvement of Downstream Resources, Including Those of Importance to American Indian Tribes
U.S. Department of the Interior Record of Decision for the Glen Canyon Dam Long-Term Experimental and Management Plan Final Environmental Impact Statement December 2016 U.S. Department of the Interior Bureau of Reclamation Upper Colorado Region Salt Lake City, Utah National Park Service Intermountain Region Lakewood, Colorado Record of Decision Glen Canyon Dam Long-Term Experimental and Management Plan 1. SUMMARY OF ACTION The U.S. Department of the Interior (DOI), through the Bureau of Reclamation, Upper Colorado Region (Reclamation) and the National Park Service (NPS) have jointly published a Final Environmental Impact Statement (FEIS) for the Glen Canyon Dam Long-Term Experimental and Management Plan (L TEMP). Reclamation and NPS are joint-lead agencies for the L TEMP EIS because of their roles in operating Glen Canyon Dam (Reclamation's role) and managing the resources of Glen Canyon National Recreation Area (GCNRA), Grand Canyon National Park (GCNP), and Lake Mead National Recreation Area (LMNRA) (NPS 's role). As joint leads, both agencies were equally involved in the development of all aspects of the L TEMP FEIS. There were 15 Cooperating Agencies for the FEIS, which included the Bureau of Indian Affairs (BIA), U.S. Fish and Wildlife Service (FWS), Western Area Power Administration (WAP A), Arizona Game and Fish Department (AZGFD), Colorado River Board of California, Colorado River Commission of Nevada, Upper Colorado River Commission, Salt River Project, Utah Associated Municipal Power Systems, Havasupai Tribe, Hopi Tribe, Hualapai Tribe, Kaibab Band of Paiute Indians, Navajo Nation, and the Pueblo of Zuni. Throughout the process, the U.S. -
Natural Flow and Salt Computation Methods, Calendar Years 1971-1995
Utah State University DigitalCommons@USU All U.S. Government Documents (Utah Regional U.S. Government Documents (Utah Regional Depository) Depository) 12-2005 Natural Flow and Salt Computation Methods, Calendar Years 1971-1995 James Prairie Russell Callejo Follow this and additional works at: https://digitalcommons.usu.edu/govdocs Part of the Environmental Sciences Commons Recommended Citation Prairie, James and Callejo, Russell, "Natural Flow and Salt Computation Methods, Calendar Years 1971-1995" (2005). All U.S. Government Documents (Utah Regional Depository). Paper 135. https://digitalcommons.usu.edu/govdocs/135 This Report is brought to you for free and open access by the U.S. Government Documents (Utah Regional Depository) at DigitalCommons@USU. It has been accepted for inclusion in All U.S. Government Documents (Utah Regional Depository) by an authorized administrator of DigitalCommons@USU. For more information, please contact [email protected]. Natural Flow And Salt Computation Methods Calendar Years 1971-1995 U.S. Department of the Interior U.S. Department of the Interior Bureau of Reclamation Bureau of Reclamation Upper Colorado Regional Office Lower Colorado Regional Office Technical Services and Dams Division Boulder Canyon Operations Office Water Quality Group River Operations Group Salt Lake City, Utah Boulder City, Nevada December 2005 Natural Flow And Salt Computation Methods Calendar Years 1971-1995 by James Prairie Russell Callejo U.S. Department of the Interior U.S. Department of the Interior Bureau of Reclamation -
Lake Mohave Basin Fact Sheet 12-05
FACT SHEET Ambient Groundwater Quality of the Lake Mohave Basin: A 2003 Baseline Study - October 2005 INTRODUCTION Containing approximately 1,050 square miles, the Lake Mohave groundwater basin (MHV) stretches along the Colorado River from Hoover Dam south to the community of Topock in northwestern Arizona.1 The Black Mountains form the eastern boundary of this long, thin basin (Map 1). Precipitation averages from 6 to 10 inches annually depending on elevation.2 Two major storage dams are located on the Colorado River along the MHV. To the north is Hoover Dam, completed in 1936, which forms Lake Mead. To the west is Davis Dam (Figure 1), completed in 1950, which forms the much smaller Lake Mohave.1 Davis Dam was constructed along a granite outcrop Figure 1- Located 67 miles downstream from Hoover Dam, 1 Davis Dam is an earthfill impoundment finished in 1950 that that divides the MHV into North and South basins. forms Lake Mohave, a long, narrow reservoir with a 1.8 million However, the South basin’s southern boundary near acre-feet capacity. Topock (Figure 2) is a surface water divide that does not impede groundwater flow with the neighboring The North basin consists largely of rugged topog- Sacramento Valley groundwater basin. raphy and undeveloped public lands that are part of the Lake Mead National Recreation area. The South basin consists of public uplands managed by the Bureau of Land Management and a piedmont descending to Mohave Valley, which is a combination of private, State Trust, and Fort Mohave Indian Reservation lands. This basin includes scattered subdi- visions, the Mohave Valley Irrigation and Drainage District, and the recreation, retirement, and service communities of Bullhead City, Golden Shores, Oatman, and Topock.