Colorado River Miles Chart
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Arizona TIM PALMER FLICKR
Arizona TIM PALMER FLICKR Colorado River at Mile 50. Cover: Salt River. Letter from the President ivers are the great treasury of noted scientists and other experts reviewed the survey design, and biological diversity in the western state-specific experts reviewed the results for each state. RUnited States. As evidence mounts The result is a state-by-state list of more than 250 of the West’s that climate is changing even faster than we outstanding streams, some protected, some still vulnerable. The feared, it becomes essential that we create Great Rivers of the West is a new type of inventory to serve the sanctuaries on our best, most natural rivers modern needs of river conservation—a list that Western Rivers that will harbor viable populations of at-risk Conservancy can use to strategically inform its work. species—not only charismatic species like salmon, but a broad range of aquatic and This is one of 11 state chapters in the report. Also available are a terrestrial species. summary of the entire report, as well as the full report text. That is what we do at Western Rivers Conservancy. We buy land With the right tools in hand, Western Rivers Conservancy is to create sanctuaries along the most outstanding rivers in the West seizing once-in-a-lifetime opportunities to acquire and protect – places where fish, wildlife and people can flourish. precious streamside lands on some of America’s finest rivers. With a talented team in place, combining more than 150 years This is a time when investment in conservation can yield huge of land acquisition experience and offices in Oregon, Colorado, dividends for the future. -
The Lower Gila Region, Arizona
DEPARTMENT OF THE INTERIOR HUBERT WORK, Secretary UNITED STATES GEOLOGICAL SURVEY GEORGE OTIS SMITH, Director Water-Supply Paper 498 THE LOWER GILA REGION, ARIZONA A GEOGBAPHIC, GEOLOGIC, AND HTDBOLOGIC BECONNAISSANCE WITH A GUIDE TO DESEET WATEEING PIACES BY CLYDE P. ROSS WASHINGTON GOVERNMENT PRINTING OFFICE 1923 ADDITIONAL COPIES OF THIS PUBLICATION MAT BE PROCURED FROM THE SUPERINTENDENT OF DOCUMENTS GOVERNMENT PRINTING OFFICE WASHINGTON, D. C. AT 50 CENTS PEE COPY PURCHASER AGREES NOT TO RESELL OR DISTRIBUTE THIS COPT FOR PROFIT. PUB. RES. 57, APPROVED MAT 11, 1822 CONTENTS. I Page. Preface, by O. E. Melnzer_____________ __ xr Introduction_ _ ___ __ _ 1 Location and extent of the region_____._________ _ J. Scope of the report- 1 Plan _________________________________ 1 General chapters _ __ ___ _ '. , 1 ' Route'descriptions and logs ___ __ _ 2 Chapter on watering places _ , 3 Maps_____________,_______,_______._____ 3 Acknowledgments ______________'- __________,______ 4 General features of the region___ _ ______ _ ., _ _ 4 Climate__,_______________________________ 4 History _____'_____________________________,_ 7 Industrial development___ ____ _ _ _ __ _ 12 Mining __________________________________ 12 Agriculture__-_______'.____________________ 13 Stock raising __ 15 Flora _____________________________________ 15 Fauna _________________________ ,_________ 16 Topography . _ ___ _, 17 Geology_____________ _ _ '. ___ 19 Bock formations. _ _ '. __ '_ ----,----- 20 Basal complex___________, _____ 1 L __. 20 Tertiary lavas ___________________ _____ 21 Tertiary sedimentary formations___T_____1___,r 23 Quaternary sedimentary formations _'__ _ r- 24 > Quaternary basalt ______________._________ 27 Structure _______________________ ______ 27 Geologic history _____ _____________ _ _____ 28 Early pre-Cambrian time______________________ . -
The Gila and Little Colorado General Stream Adjudications
THE GILA AND LITTLE COLORADO GENERAL STREAM ADJUDICATIONS Cynthia M. Chandley 1 ©© 2014 2014 Snell Snell & & Wilmer Wilmer Arizona’s Watersheds 2 © 2014 Snell & Wilmer Scope of Adjudications Gila Adjudication Little Colorado River Adjudication 30,000 5,000 SOCs SOCs Claimants 85,000 14,000 Claimants 3 © 2014 Snell & Wilmer Initiation of Arizona’s Adjudications SRP initiates U.S. Supreme Court Phelps Dodge Verde River Buckeye Irrigation decides jurisdiction in on- initiates Little Adjudication District intervenes going state adjudications. Colorado River Ariz. v. San Carlos Adjudication Apache Tribe (U.S. 1983) 1974 1976 1978 1979 1980 1981 1983 1985 Arizona Supreme SRP initiates Phelps Dodge initiates Court consolidates Salt River Gila River Adjudication Arizona Arizona Supreme Court Gila River cases Adjudication Adjudication statues decides state jurisdiction ASARCO initiates San revised over federal and Indian Pedro River Adjudication water rights. U.S. v. Superior Court (Ariz. 1985) 4 © 2014 Snell & Wilmer Maricopa County Court Proceedings • 1986 – Judge Goodfarb issues Pretrial Order No. 1 • 1990 – Arizona Supreme Court grants interlocutory review of six key issues 5 © 2014 Snell & Wilmer Arizona Supreme Court Rulings • Issue 1: Service of process – Gila I (1992) • Issue 2: Subflow – Gila II (1993) & Gila IV (2000) • Issue 3: Indian reserved water rights – Gila V (2001) • Issues 4 & 5: Federal reserved groundwater rights – Gila III (1999) • Issue 6: To be decided. 6 © 2014 Snell & Wilmer Major Adjudication Issues Subflow Trial No. 1; Adjudication Gila III and San Subflow Order Carlos Apache Court defines ADWR Subflow defines saturated Tribe, et al. v. ADWR Subflow 50%/90-day test Technical Report floodplain Holocene Superior Court Delineation ADWR Revised alluvium and evidentiary Report Subflow Report hearing 1986 1988 1993 1994 1995 1999 2000 2002 2005 2009 2012 2014 2014 2012 20142014 Pretrial Order Gila IV – affirms Gila II: rejects Subflow Subflow trial No. -
Tectonic Influences on the Spatial and Temporal Evolution of the Walker Lane: an Incipient Transform Fault Along the Evolving Pacific – North American Plate Boundary
Arizona Geological Society Digest 22 2008 Tectonic influences on the spatial and temporal evolution of the Walker Lane: An incipient transform fault along the evolving Pacific – North American plate boundary James E. Faulds and Christopher D. Henry Nevada Bureau of Mines and Geology, University of Nevada, Reno, Nevada, 89557, USA ABSTRACT Since ~30 Ma, western North America has been evolving from an Andean type mar- gin to a dextral transform boundary. Transform growth has been marked by retreat of magmatic arcs, gravitational collapse of orogenic highlands, and periodic inland steps of the San Andreas fault system. In the western Great Basin, a system of dextral faults, known as the Walker Lane (WL) in the north and eastern California shear zone (ECSZ) in the south, currently accommodates ~20% of the Pacific – North America dextral motion. In contrast to the continuous 1100-km-long San Andreas system, discontinuous dextral faults with relatively short lengths (<10-250 km) characterize the WL-ECSZ. Cumulative dextral displacement across the WL-ECSZ generally decreases northward from ≥60 km in southern and east-central California, to ~25 km in northwest Nevada, to negligible in northeast California. GPS geodetic strain rates average ~10 mm/yr across the WL-ECSZ in the western Great Basin but are much less in the eastern WL near Las Vegas (<2 mm/ yr) and along the northwest terminus in northeast California (~2.5 mm/yr). The spatial and temporal evolution of the WL-ECSZ is closely linked to major plate boundary events along the San Andreas fault system. For example, the early Miocene elimination of microplates along the southern California coast, southward steps in the Rivera triple junction at 19-16 Ma and 13 Ma, and an increase in relative plate motions ~12 Ma collectively induced the first major episode of deformation in the WL-ECSZ, which began ~13 Ma along the N60°W-trending Las Vegas Valley shear zone. -
Lake Mead National Recreation Area Lake Meadsummer 2013 National Recreation Area
National Park Service Park Newspaper U.S. Department of the Interior Lake Mead National Recreation Area Lake MeadSummer 2013 National Recreation Area Borrow a Lifejacket insure the proper size. The loaner lifejackets including education, warnings and citations. The point of the rule isn't to ticket boaters, but to Drowning is the number one cause of fatalities at must be returned before dusk to allow ensure that the most polluting engines are kept Lake Mead National Recreation Area. This loss rangers to inspect and properly store them. off the lake. As time passes, the number of non- of life can be prevented by wearing a lifejacket. Please remember to never leave children compliant PWCs will decline through attrition. unattended. Drowning is preventable if you put on a lifejacket. Wear One for Life! PWCs that meet the standards through the use of direct-injection two-stroke or New Personal Watercraft four-stroke engines are not subject to this prohibition and are still allowed on the lakes. Regulation in Effect Engines that meet the regulations should have an In an effort to safeguard the waters within Lake emission control information label that clearly Mead National Recreation Area, personal water- states that they conform to clean emissions stan- craft (PWC) must now meet 2006 Environmental dards. Boats are not impacted by this regulation. Protection Agency emission standards in order to operate within the park. This includes the waters of A list of frequently asked questions and PWC Lake Mead, Lake Mohave and the Colorado River. models that meet the emissions standards can be This year there are new Lifejacket Loaner found online at: Stations at Boulder Beach and Cottonwood “Lake Mead supplies drinking water for millions www.nps.gov/lake/parkmgmt/twostroke.htm. -
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 -
Water Resources of Bill Williams River Valley Near Alamo, Arizona
Water Resources of Bill Williams River Valley Near Alamo, Arizona GEOLOGICAL SURVEY WATER-SUPPLY PAPER 1360-D DEC 10 1956 Water Resources of Bill Williams River Valley Near Alamo, Arizona By H. N. WOLCOTT, H. E. SKIBITZKE, and L. C. HALPENNY CONTRIBUTIONS TO THE HYDROLOGY OF THE UNITED STATES GEOLOGICAL SURVEY WATER-SUPPLY PAPER 1360-D An investigation of the availability of water in the area of the Artillery Mountains manganese deposits UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1956 UNITED STATES DEPARTMENT OF THE INTERIOR Fred A. Seaton, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director For sale by the Superintendent of Documents, U. S. Government Printing Office Washington 25, D. C. - Price 45 cents (paper cover) CONTENTS Page Abstract....................................................................................................................................... 291 Introduction................................................................................................................................. 292 Purpose.................................................................................................................................... 292 Location................................................................................................................................... 292 Climatological data............................................................................................................... 292 History of development........................................................................................................ -
Petition to List the Relict Leopard Frog (Rana Onca) As an Endangered Species Under the Endangered Species Act
BEFORE THE SECRETARY OF INTERIOR PETITION TO LIST THE RELICT LEOPARD FROG (RANA ONCA) AS AN ENDANGERED SPECIES UNDER THE ENDANGERED SPECIES ACT CENTER FOR BIOLOGICAL DIVERSITY SOUTHERN UTAH WILDERNESS ALLIANCE PETITIONERS May 8, 2002 EXECUTIVE SUMMARY The relict leopard frog (Rana onca) has the dubious distinction of being one of the first North American amphibians thought to have become extinct. Although known to have inhabited at least 64 separate locations, the last historical collections of the species were in the 1950s and this frog was only recently rediscovered at 8 (of the original 64) locations in the early 1990s. This extremely endangered amphibian is now restricted to only 6 localities (a 91% reduction from the original 64 locations) in two disjunct areas within the Lake Mead National Recreation Area in Nevada. The relict leopard frog historically occurred in springs, seeps, and wetlands within the Virgin, Muddy, and Colorado River drainages, in Utah, Nevada, and Arizona. The Vegas Valley leopard frog, which once inhabited springs in the Las Vegas, Nevada area (and is probably now extinct), may eventually prove to be synonymous with R. onca. Relict leopard frogs were recently discovered in eight springs in the early 1990s near Lake Mead and along the Virgin River. The species has subsequently disappeared from two of these localities. Only about 500 to 1,000 adult frogs remain in the population and none of the extant locations are secure from anthropomorphic events, thus putting the species at an almost guaranteed risk of extinction. The relict leopard frog has likely been extirpated from Utah, Arizona, and from the Muddy River drainage in Nevada, and persists in only 9% of its known historical range. -
MS4 Route Mapping PRIORITIZATION PARAMETERS
MS4 Route Mapping PRIORITIZATION PARAMETERS Approx. ADOT Named or Average Annual Length Year Age OAW/Impaired/ Not‐ Within 1/4 Pollutants ADOT Designated Pollutants Route ADOT Districts Annual Traffic Receiving Waters TMDL? Given Precipitation (mi) Installed (yrs) Attaining Waters? Mile? (per EPA) Pollutant? Uses (per EPA) (Vehicles/yr) WLA? (inches) SR 24 (802) 1.0 2014 5 Central 11,513,195 Queen Creek N ‐‐ ‐‐ ‐‐ ‐‐ ‐‐ ‐‐ ‐‐ 6 SR 51 16.7 1987 32 Central 61,081,655 Salt River N ‐‐ ‐‐ ‐‐ ‐‐ ‐‐ ‐‐ ‐‐ 6 SR 61 76.51 1935 84 Northeast 775,260 Little Colorado River Y (Not attaining) N E. Coli N FBC Y E. Coli N 7 Sediment Y A&Wc Y Sediment N SR 64 108.31 1932 87 Northcentral 2,938,250 Colorado River Y (Impaired) N Sediment Y A&Wc N ‐‐ ‐‐ 8.5 Selenium Y A&Wc N ‐‐ ‐‐ SR 66 66.59 1984 35 Northwest 5,154,530 Truxton Wash N ‐‐ ‐‐ ‐‐ ‐‐ ‐‐ ‐‐ ‐‐ 7 SR 67 43.4 1941 78 Northcentral 39,055 House Rock Wash N ‐‐ ‐‐ ‐‐ ‐‐ ‐‐ ‐‐ ‐‐ 17 Kanab Creek N ‐‐ ‐‐ ‐‐ ‐‐ ‐‐ ‐‐ ‐‐ SR 68 27.88 1941 78 Northwest 5,557,490 Colorado River Y (Impaired) Y Temperature N A&Ww N ‐‐ ‐‐ 6 SR 69 33.87 1938 81 Northwest 17,037,470 Granite Creek Y (Not attaining) Y E. Coli N A&Wc, FBC, FC, AgI, AgL Y E. Coli Y 9.5 Watson Lake Y (Not attaining) Y TN Y ‐‐ Y TN Y DO N A&Ww Y DO Y pH N A&Ww, FBC, AgI, AgL Y pH Y TP Y ‐‐ Y TP Y SR 71 24.16 1936 83 Northwest 296,015 Sols Wash/Hassayampa River Y (Impaired, Not attaining) Y E. -
The Colorado River Aqueduct
Fact Sheet: Our Water Lifeline__ The Colorado River Aqueduct. Photo: Aerial photo of CRA Investment in Reliability The Colorado River Aqueduct is considered one of the nation’s Many innovations came from this period in time, including the top civil engineering marvels. It was originally conceived by creation of a medical system for contract workers that would William Mulholland and designed by Metropolitan’s first Chief become the forerunner for the prepaid healthcare plan offered Engineer Frank Weymouth after consideration of more than by Kaiser Permanente. 50 routes. The 242-mile CRA carries water from Lake Havasu to the system’s terminal reservoir at Lake Mathews in Riverside. This reservoir’s location was selected because it is situated at the upper end of Metropolitan’s service area and its elevation of nearly 1,400 feet allows water to flow by gravity to the majority of our service area The CRA was the largest public works project built in Southern California during the Great Depression. Overwhelming voter approval in 1929 for a $220 million bond – equivalent to a $3.75 billion investment today – brought jobs to 35,000 people. Miners, engineers, surveyors, cooks and more came to build Colorado River the aqueduct, living in the harshest of desert conditions and Aqueduct ultimately constructing 150 miles of canals, siphons, conduits and pipelines. They added five pumping plants to lift water over mountains so deliveries could then flow west by gravity. And they blasted 90-plus miles of tunnels, including a waterway under Mount San Jacinto. THE METROPOLITAN WATER DISTRICT OF SOUTHERN CALIFORNIA // // JULY 2021 FACT SHEET: THE COLORADO RIVER AQUEDUCT // // OUR WATER LIFELINE The Vision Despite the city of Los Angeles’ investment in its aqueduct, by the early 1920s, Southern Californians understood the region did not have enough local supplies to meet growing demands. -
Index 1 INDEX
Index 1 INDEX A Blue Spring 76, 106, 110, 115 Bluff Spring Trail 184 Adeii Eechii Cliffs 124 Blythe 198 Agate House 140 Blythe Intaglios 199 Agathla Peak 256 Bonita Canyon Drive 221 Agua Fria Nat'l Monument 175 Booger Canyon 194 Ajo 203 Boundary Butte 299 Ajo Mountain Loop 204 Box Canyon 132 Alamo Canyon 205 Box (The) 51 Alamo Lake SP 201 Boyce-Thompson Arboretum 190 Alstrom Point 266, 302 Boynton Canyon 149, 161 Anasazi Bridge 73 Boy Scout Canyon 197 Anasazi Canyon 302 Bright Angel Canyon 25, 51 Anderson Dam 216 Bright Angel Point 15, 25 Angels Window 27 Bright Angel Trail 42, 46, 49, 61, 80, 90 Antelope Canyon 280, 297 Brins Mesa 160 Antelope House 231 Brins Mesa Trail 161 Antelope Point Marina 294, 297 Broken Arrow Trail 155 Apache Junction 184 Buck Farm Canyon 73 Apache Lake 187 Buck Farm Overlook 34, 73, 103 Apache-Sitgreaves Nat'l Forest 167 Buckskin Gulch Confluence 275 Apache Trail 187, 188 Buenos Aires Nat'l Wildlife Refuge 226 Aravaipa Canyon 192 Bulldog Cliffs 186 Aravaipa East trailhead 193 Bullfrog Marina 302 Arch Rock 366 Bull Pen 170 Arizona Canyon Hot Springs 197 Bush Head Canyon 278 Arizona-Sonora Desert Museum 216 Arizona Trail 167 C Artist's Point 250 Aspen Forest Overlook 257 Cabeza Prieta 206 Atlatl Rock 366 Cactus Forest Drive 218 Call of the Canyon 158 B Calloway Trail 171, 203 Cameron Visitor Center 114 Baboquivari Peak 226 Camp Verde 170 Baby Bell Rock 157 Canada Goose Drive 198 Baby Rocks 256 Canyon del Muerto 231 Badger Creek 72 Canyon X 290 Bajada Loop Drive 216 Cape Final 28 Bar-10-Ranch 19 Cape Royal 27 Barrio -
Chemehuevi Valley Groundwater Basin Bulletin 118
Hydrologic Region Colorado River California’s Groundwater Chemehuevi Valley Groundwater Basin Bulletin 118 Chemehuevi Valley Groundwater Basin • Groundwater Basin Number: 7-43 • County: San Bernardino • Surface Area: 273,000 acres (427 square miles) Basin Boundaries and Hydrology This basin underlies Chemehuevi Valley in eastern San Bernardino County. The basin is bounded by Havasu Lake on the east and by nonwater-bearing rocks of the Sacramento Mountains on the north, of the Chemehuevi Mountains on the northeast, of the Whipple Mountains on the southeast, of the Turtle Mountains on the west and south (Bishop 1963). The valley is drained by Chemehuevi Wash to Havasu Lake. Annual average precipitation ranges from about 4 to 6 inches. Hydrogeologic Information Water Bearing Formations Groundwater in the basin is found in alluvium and the Bouse Formation. Alluvium. Holocene age younger alluvium, which is found in washes and the floodplain of the Colorado River, is composed of sand, silt and gravel (Metzger and Loeltz 1973). Older alluvium consists of unconsolidated, fine- to coarse-grained sand, pebbles, and boulders with variable amounts of silt and clay. Bouse Formation. The Pliocene age Bouse Formation is composed of a basal limestone bed overlain by interbedded clay, silt, and sand. Thickness of the formation reaches 254 feet (Metzger and Loeltz 1973). The formation is underlain by locally derived fanglomerate and overlain by alluviums of the Colorado River and its tributaries. Restrictive Structures An unnamed fault crosses a portion of the southern side of the basin (Bishop 1963), but it is not known whether or not this fault impedes groundwater flow in the basin.