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BIBLIOGRAPHY for VERDE RIVER WATERSHED PROJECT. Originally Compiled by Jim Byrkit, Assisted by Bruce Hooper, Both of Northern Arizona University
BIBLIOGRAPHY FOR VERDE RIVER WATERSHED PROJECT. Originally compiled by Jim Byrkit, assisted by Bruce Hooper, both of Northern Arizona University. Abbey, Edward.(1) 1968. Desert Solitaire: A Season in the Wilderness. New York, NY: Ballantine; McGraw- Hill. NAU PS3551.B225. Also in SC. Abbey, Edward.(1) 1986. "Even the Bad Guys Wear White Hats: Cowboys, Ranchers, and Ruin of the West." Harper's, Vol. 272, No. 1628 (January), pp. 51-55. NAU AP2.H3.V272. Abeytia, Lt. Antonio.(1) 1865. "Letter to the Assistant Adjutant General of the District of Arizona for transmission to Brigadier General John S. Mason from Rio Verde, Arizona." Published in the 17th Annual Fort Verde Day Brochure, October 13, 1973, p. 62. (August 29) (Files of the Camp Verde Historical Society) NAU SC F819.C3C3 1973. ("1st Lt. A. Abeytia's Letter.") Adamus, Paul R.(1) 1986. Final Work Plan, Mendenhall Valley Wetland Assessment Project Calibration Studies. Adamus Resource Assessment, Inc. (NAU no) Adamus, Paul R., and L. T. Stockwell.(1) 1983. A Method for Wetland Functional Assessment, Vol. 1. Report No. FHWA-IP-82 23. U.S. Department of Transportation, Federal Highway Administration, Offices of Research and Development. 2 Vols. NAU Gov. Docs. TD 2.36:82-24. Adamus, Paul R., et al. (Daniel R. Smith?)(1) 1987. Wetland Evaluation Technique (WET); Volume II: Methodology. Operational Draft Technical Report Y-87- (?). Vicksburg, MS: U.S. Army Engineer Waterways Experiment Station. (NAU no) Ahmed, Muddathir Ali.(2) 1965. "Description of the Salt River Project and Impact of Water Rights on Optimum Farm Organization and Values." MA Thesis, University of Arizona. -
An Adm I N I Strati Ve History of Grand Ca Nyon Nati Onal Pa R K Becomingchapter a Natio Onenal Park -
Figure 1.Map ofGrand Canyon National Monument/Grand Canyon Game Preserve, National Game Preserve (created by Roosevelt in 1906),and unassigned public domain. ca.1906-10. President Theodore Roosevelt liberally interpreted the 1906 Antiquities Act The U.S.Forest Service managed the monument from 1908 until it became a national when he established by proclamation the 1,279-square-milerand G Canyon National park in 1919, relying entirely on the Santa Fe Railroad to invest in roads,trails,and Monument in 1908.The monument was carved from Grand Canyon National Forest amenities to accommodate a budding tourism industry. (created by President Benjamin Harrison as a forest reserve in 1893), Grand Canyon an adm i n i strati ve history of grand ca nyon nati onal pa r k BecomingChapter a Natio Onenal Park - In the decades after the Mexican-American War, federal explorers and military in the Southwest located transportation routes, identified natural resources, and brushed aside resistant Indian peo p l e s . It was during this time that Europ ean America n s , fo ll o wing new east-west wagon roads, approached the rim of the Grand Canyon.1 The Atlantic & Pacific Railroad’s arrival in the Southwest accelerated this settlement, opening the region to entrepreneurs who initially invested in traditional economic ventures.Capitalists would have a difficult time figuring out how to profitably exploit the canyon,how- ever, biding their time until pioneers had pointed the way to a promising export economy: tourism. Beginning in the late 1890s, conflicts erupted between individualists who had launched this nascent industry and corporations who glimpsed its potential. -
GRAND CANYON GUIDE No. 6
GRAND CANYON GUIDE no. 6 ... excerpted from Grand Canyon Explorer … Bob Ribokas AN AMATEUR'S REVIEW OF BACKPACKING TOPICS FOR THE T254 - EXPEDITION TO THE GRAND CANYON - MARCH 2007 Descriptions of Grand Canyon Layers Grand Canyon attracts the attention of the world for many reasons, but perhaps its greatest significance lies in the geologic record that is so beautifully preserved and exposed here. The rocks at Grand Canyon are not inherently unique; similar rocks are found throughout the world. What is unique about the geologic record at Grand Canyon is the great variety of rocks present, the clarity with which they're exposed, and the complex geologic story they tell. Paleozoic Strata: Kaibab depositional environment: Kaibab Limestone - This layer forms the surface of the Kaibab and Coconino Plateaus. It is composed primarily of a sandy limestone with a layer of sandstone below it. In some places sandstone and shale also exists as its upper layer. The color ranges from cream to a greyish-white. When viewed from the rim this layer resembles a bathtub ring and is commonly referred to as the Canyon's bathtub ring. Fossils that can be found in this layer are brachiopods, coral, mollusks, sea lilies, worms and fish teeth. Toroweap depositional environment Toroweap Formation - This layer is composed of pretty much the same material as the Kaibab Limestone above. It is darker in color, ranging from yellow to grey, and contains a similar fossil history. Coconino depositional environment: Coconino Sandstone - This layer is composed of pure quartz sand, which are basically petrified sand dunes. Wedge-shaped cross bedding can be seen where traverse-type dunes have been petrified. -
Historical Development of Water Resources at the Grand Canyon
Guide Feb 7-8, 2015 Training Pioneer Trails Seminar “to” Grand Canyon by Dick Brown Grand Canyon Historical Society Pioneers of the Grand Canyon Seth B. Tanner* Niles J. Cameron* Louis D. Boucher* William F. Hull* Peter D. Berry* Babbitt Brothers John Hance* John A. Marshall Ellsworth Kolb William W. Bass* William O. O’Neill Emery Kolb William H. Ashurst Daniel L. Hogan* Charles J. Jones* Ralph H. Cameron* Sanford H. Rowe James T. Owens* * Canyon Guides By one means or another, and by a myriad of overland pathways, these pioneers eventually found their way to this magnificent canyon. Seth Benjamin Tanner Trailblazer & Prospector . Born in 1828, Bolton Landing, on Lake George in Adirondack Mountains, NY . Family joined Mormon westward migration . Kirtland, OH in 1834; Far West, MO in 1838; IL in 1839; IA in 1840 . Family settled in "the promised land" near Great Salt Lake in 1847 . Goldfields near Sacramento, CA in 1850 . Ranching in San Bernardino, CA (1851-1858) . Married Charlotte Levi, 1858, Pine Valley, UT, seven children, Charlotte died in 1872 . Led Mormon scouting party in 1875, Kanab to Little Colorado River . Married Anna Jensen, 1876, Salt Lake City, settled near today’s Cameron Trading Post . In 1880, organized Little Colorado Mining District and built Tanner Trail . Later years, Seth (then blind) & Annie lived in Taylor, 30 miles south of Holbrook, AZ Photo Courtesy of John Tanner Family Association . Seth died in 1918 William Francis Hull Sheep Rancher & Road Builder . Four brothers: William (born in 1865), Phillip, Joseph & Frank . Hull family came from CA & homesteaded Hull Cabin near Challender, southeast of Williams . -
Grand Canyon
U.S. Department of the Interior Geologic Investigations Series I–2688 14 Version 1.0 4 U.S. Geological Survey 167.5 1 BIG SPRINGS CORRELATION OF MAP UNITS LIST OF MAP UNITS 4 Pt Ph Pamphlet accompanies map .5 Ph SURFICIAL DEPOSITS Pk SURFICIAL DEPOSITS SUPAI MONOCLINE Pk Qr Holocene Qr Colorado River gravel deposits (Holocene) Qsb FAULT CRAZY JUG Pt Qtg Qa Qt Ql Pk Pt Ph MONOCLINE MONOCLINE 18 QUATERNARY Geologic Map of the Pleistocene Qtg Terrace gravel deposits (Holocene and Pleistocene) Pc Pk Pe 103.5 14 Qa Alluvial deposits (Holocene and Pleistocene) Pt Pc VOLCANIC ROCKS 45.5 SINYALA Qti Qi TAPEATS FAULT 7 Qhp Qsp Qt Travertine deposits (Holocene and Pleistocene) Grand Canyon ၧ DE MOTTE FAULT Pc Qtp M u Pt Pleistocene QUATERNARY Pc Qp Pe Qtb Qhb Qsb Ql Landslide deposits (Holocene and Pleistocene) Qsb 1 Qhp Ph 7 BIG SPRINGS FAULT ′ × ′ 2 VOLCANIC DEPOSITS Dtb Pk PALEOZOIC SEDIMENTARY ROCKS 30 60 Quadrangle, Mr Pc 61 Quaternary basalts (Pleistocene) Unconformity Qsp 49 Pk 6 MUAV FAULT Qhb Pt Lower Tuckup Canyon Basalt (Pleistocene) ၣm TRIASSIC 12 Triassic Qsb Ph Pk Mr Qti Intrusive dikes Coconino and Mohave Counties, Pe 4.5 7 Unconformity 2 3 Pc Qtp Pyroclastic deposits Mr 0.5 1.5 Mၧu EAST KAIBAB MONOCLINE Pk 24.5 Ph 1 222 Qtb Basalt flow Northwestern Arizona FISHTAIL FAULT 1.5 Pt Unconformity Dtb Pc Basalt of Hancock Knolls (Pleistocene) Pe Pe Mၧu Mr Pc Pk Pk Pk NOBLE Pt Qhp Qhb 1 Mၧu Pyroclastic deposits Qhp 5 Pe Pt FAULT Pc Ms 12 Pc 12 10.5 Lower Qhb Basalt flows 1 9 1 0.5 PERMIAN By George H. -
Chapter Three
CIrhapteronic Golden T Yhreeears - The s at Grand Canyon National Park witnessed a seamless progression of building pro- grams begun in the mid-s.The two decades were linked as well by persistence with earlier efforts to enhance visitors’experiences and protect the landscape through educational programs,bound- ary extensions, and the elimination of private and state inholdings. The continuity seems odd at first glance, as it accompanied the deepest economic depression the nation has yet endured. This cyclical malady of world capitalism might have resulted in reduced federal spending, a return to traditional extraction of resources, or a nonstructural approach to park management. Instead, it triggered federal subsidies in the form of emergency building funds and a ready supply of desperate low-wage laborers.Under Miner Tillotson,one of the better park superintendents by NPS standards,a mature administration took full and efficient advantage of national economic woes to complete structural improvements that,given World War and subsequent financial scrimping, might never have been built. In contrast to the misery of national unemployment,homelessness,dust bowls,and bread lines,financial circumstances com- bined with a visitational respite to produce a few golden years at many of the West’s national parks,including Grand Canyon. From an administrative perspective, staffing and base fund- $, annually. Normal road and trail funds diminished, ing remained at late-s levels through , as if there causing several new projects to be delayed, but deficits were had been no stock market crash and deepening financial offset by modest emergency funds of the Hoover collapse. Permanent employees in consisted of the Administration that allowed those projects already in superintendent, an assistant superintendent, chief ranger, progress to continue unabated. -
Wes Hildreth
Transcription: Grand Canyon Historical Society Interviewee: Wes Hildreth (WH), Jack Fulton (JF), Nancy Brown (NB), Diane Fulton (DF), Judy Fierstein (JYF), Gail Mahood (GM), Roger Brown (NB), Unknown (U?) Interviewer: Tom Martin (TM) Subject: With Nancy providing logistical support, Wes and Jack recount their thru-hike from Supai to the Hopi Salt Trail in 1968. Date of Interview: July 30, 2016 Method of Interview: At the home of Nancy and Roger Brown Transcriber: Anonymous Date of Transcription: March 9, 2020 Transcription Reviewers: Sue Priest, Tom Martin Keys: Grand Canyon thru-hike, Park Service, Edward Abbey, Apache Point route, Colin Fletcher, Harvey Butchart, Royal Arch, Jim Bailey TM: Today is July 30th, 2016. We're at the home of Nancy and Roger Brown in Livermore, California. This is an oral history interview, part of the Grand Canyon Historical Society Oral History Program. My name is Tom Martin. In the living room here, in this wonderful house on a hill that Roger and Nancy have, are Wes Hildreth and Gail Mahood, Jack and Diane Fulton, Judy Fierstein. I think what we'll do is we'll start with Nancy, we'll go around the room. If you can state your name, spell it out for me, and we'll just run around the room. NB: I'm Nancy Brown. RB: Yeah. Roger Brown. JF: Jack Fulton. WH: Wes Hildreth. GM: Gail Mahood. DF: Diane Fulton. JYF: Judy Fierstein. TM: Thank you. This interview is fascinating for a couple different things for the people in this room in that Nancy assisted Wes and Jack on a hike in Grand Canyon in 1968 from Supai to the Little Colorado River. -
Boatman's Quarterly Review
boatman’s quarterly review Henry Falany the journal of the Grand Canyon River Guide’s, Inc. • voulme 29 number 2 summer 2016 the journal of Grand Canyon River Guide’s, Dear Eddy • Prez Blurb • Farewell • Ed Fund • To DC • Back of the Boat • Letter to a Young Swamper • Supt Retires • GTS 2016! • Lava Falls • Wait, is There More? Call Me No Name • GCRG Endowment • Youth • Cap’n Hance boatman’s quarterly review Dear Eddy …is published more or less quarterly by and for GRAND CANYON RIVER GUIDES. IN REFERENCE TO THE ARTICLE, Analysis of the Cooling GRAND CANYON RIVER GUIDES Rate of Fermented Beverages in the Grand Canyon BY is a nonprofit organization dedicated to REBECCA AND VIRGINIA ZAUNBRECHER, IN BQR VOLUME 29 NUMBER 1, SPRING 2016. Protecting Grand Canyon Setting the highest standards for the river profession HE DETAILED STUDY by the Zaunbrechers is a Celebrating the unique spirit of the river community welcome empirical demonstration of the Providing the best possible river experience TSeven-minute Immersion Conjecture, which the authors state, “asses [sic] the time period necessary General Meetings are held each Spring and Fall. Our to cool beer to river temperature” specifically, with Board of Directors Meetings are generally held the first respect to the cooling effect of “captive” hatch water Wednesday of each month. All innocent bystanders are versus “live” river water on zymurgic beverages. urged to attend. Call for details. The authors, however, have not fully addressed the STAFF peculiar observation that while the “Immersion -
Lockwood, Francis C Collection
MS 441 LOCKWOOD, FRANCIS C., 1864-1948 PAPERS, 1913-1946 DESCRIPTION This is a collection of 10 boxes of correspondence and manuscripts by Francis C. Lockwood who was a member of the University of Arizona faculty for 31 years. The collection consists of correspondence by and to Dr. Lockwood between 1913 and 1948. Of special note is correspondence to various Arizona residents and historical figures on information about Arizona history. In addition, correspondence also covers the work of Dr. Lockwood as chairman of the Kino Memorial Committee. Manuscript entail many of the lectures and programs present by Dr. Lockwood in Arizona and around the nation. 10 Boxes, 5 linear feet BIOGRAPHICAL NOTE Francis C. Lockwood was born in Mount Erie, Illinois in 1864. He came to the University of Arizona as Professor of English in 1916. He served as Dean of College of Letters, Arts and Sciences from 1920 to 1930. Dr. Lockwood served as the acting president of the University of Arizona from 1922-1923. After 1930 he resigned as Dean and devoted his time to research, lecturing, and teaching. Dr. Lockwood remained with the University for 31 years with a brief departure in 1918 to serve overseas in the Army Educational Commission with the Y.M.C.A. As Dean for the College of Liberal Arts Dr. Lockwood was deeply interested in student welfare and education. In 1925 he co-authored with Dean Kate W. Jameson “The Freshmen Girl! A Campus Guide.” Dr. Lockwood was a well known lecturer with a strong interest in Arizona history and published numerous books and articles, including: If Kino Rode Today; Life In Old Tucson; The Old English Coffee House; Arizona Characters; Life of Edward E. -
A Guide to Grand Canyon Village Historic District
COVER PHOTO: BRIGHT ANGEL CAMP, 1898. J. Wilbur Thurber operated the first stage from Flagstaff to the rim of the Grand Canyon. After the three-hour ride from Williams, Arizona, the first passengers to arrive at the Grand Canyon by train posed forthis photograph. attracting people for many years. They gathered wild plant foods and hunted here almost 4,000 years before the train arrived. Eight centuries ago, people lived and farmed both in the canyon and on September 18, 1901. its rims. In 1540, Spaniards from Coronado's expe Santa Fe engineer Harry Schlee eases dition were the first Europeans to view the Grand locomotive 282 along the last mile of Canyon. Modern settlement, however, did not track. Though his passengers are anxious begin until 1883 when John Hance built a cabin to arrive, he pulls the heavy load of tank 12 miles (19.2 km) east of the present Grand cars cautiously over the new rails. The few Canyon Village. It was prospecting that first drew passengers talk excitedly about the event soon Hance and other pioneers, but they soon realized to occur. In minutes, they will be the first visitors that tourism was a more lucrative business than to reach the Grand Canyon by train. mining. Most of them have been here before, taking When the train came, most people viewed the the expensive, 11-hour stage trip from Flagstaff. Grand Canyon from around the head of the At $3.95 the 3-hour trip from Williams is a Bright Angel Trail. With time, the Village grew bargain. -
A Hiker's Companion to GRAND CANYON GEOLOGY
A Hiker’s Companion to GRAND CANYON GEOLOGY With special attention given to The Corridor: North & South Kaibab Trails Bright Angel Trail The geologic history of the Grand Canyon can be approached by breaking it up into three puzzles: 1. How did all those sweet layers get there? 2. How did the area become uplifted over a mile above sea level? 3. How and when was the canyon carved out? That’s how this short guide is organized, into three sections: 1. Laying down the Strata, 2. Uplift, and 3. Carving the Canyon, Followed by a walking geological guide to the 3 most popular hikes in the National Park. I. LAYING DOWN THE STRATA PRE-CAMBRIAN 2000 mya (million years ago), much of the planet’s uppermost layer was thin oceanic crust, and plate tectonics was functioning more or less as it does now. It begins with a Subduction Zone... Vishnu Schist: 1840 mya, the GC region was the site of an active subduction zone, crowned by a long volcanic chain known as the Yavapai Arc (similar to today’s Aleutian Islands). The oceanic crust on the leading edge of Wyomingland, a huge plate driving in from the NW, was subducting under another plate at the zone, a terrane known as the Yavapai Province. Subduction brought Wyomingland closer and closer to the arc for 150 million years, during which genera- tions of volcanoes were born and laid dormant along the arc. Lava and ash of new volcanoes mixed with the eroded sands and mud from older cones, creating a pile of inter-bedded lava, ash, sand, and mud that was 40,000 feet deep! Vishnu Schist Zoroaster Granite Wyomingland reached the subduction zone 1700 mya. -
Isochron Discordances and the Role of Inheritance and Mixing of Radioisotopes in the Mantle and Crust
Chapter 6 Isochron Discordances and the Role of Inheritance and Mixing of Radioisotopes in the Mantle and Crust Andrew A. Snelling, Ph.D.* Abstract. New radioisotope data were obtained for ten rock units spanning the geologic record from the recent to the early Precambrian, five of these rock units being in the Grand Canyon area. All but one of these rock units were derived from basaltic magmas generated in the mantle. The objective was to test the reliability of the model and isochron “age” dating methods using the K-Ar, Rb-Sr, Sm-Nd, and Pb-Pb radioisotope systems. The isochron “ages” for these rock units consistently indicated that the α-decaying radioisotopes (238U, 235U, and 147Sm) yield older “ages” than the β-decaying radioisotopes (40K, 87Rb). Marked discordances were found among the isochron “ages” yielded by these radioisotope systems, particularly for the seven Precambrian rock units studied. Also, the longer the half-life of the α- or β-decaying radioisotope, and/or the heavier the atomic weight of the parent radioisotope, the greater was the isochron “age” it yielded relative to the other α- or β-decaying radioisotopes respectively. It was concluded that because each of these radioisotope systems was dating the same geologic event for each rock unit, the only way this systematic isochron discordance could be reconciled would be if the decay of the parent radioisotopes had been accelerated at different rates at some time or times in the past, the α-decayers having been accelerated more than the β-decayers. However, a further complication to this pattern is that the radioisotope endowments of the mantle sources of basaltic magmas can sometimes be inherited by the magmas without resetting of the radioisotope * Geology Department, Institute for Creation Research, Santee, California 394 A.