Origin of Place Names-Nevada
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The Hills Are Alive
18 ★ FTWeekend 2 May/3 May 2015 House Home perfect, natural columns of Ginkgo biloba“Menhir”. Pergolasandterraces,whichdripwith trumpet vine in summer, look down on standing stones and a massive “stone Returning to Innisfree after 15 years, Jane Owen henge”framingthelake. A grass dome, “possibly a chunk of mountain top or some such cast finds out whether this living work of art in down by the glacier that created the lake”, says Oliver, is echoed by clipped New York State retains its magic domes of Pyrus calleryana, the pear nativetoChina. Beyond the white pine woods, the path becomes boggy and narrow, criss- crossed with tree roots, moss and fungi. A covered wooden bridge reminds visi- torsthisisanall-Americanlandscape. Buteventheall-American,maplesyr- The hills up-supplying sugar maples here come with a twist. They are Acer saccharum “Monumentale” and, like the ginkgos, are naturally column-shaped. Innis- free’s American elms went years ago, are alive . victims of Dutch elm disease, but the Hemlocks are hanging on, with the help ofinsecticidetofightthewoollyadelgid. Larger garden pests include beavers, which have built a lodge 100m from the bout 90 miles west of the Iwillariseandgonow,andgoto bubble fountain, and deer. At least the thrumming heart of New Innisfree, . latter has a use, as part of a programme York City is a landscape Ihearlakewaterlappingwithlow of hunters donating food for those in that stirs my soul. I rate soundsbytheshore; need. So the dispossessed eat venison, it along with Villa Lante, WhileIstandontheroadway,oron albeitthetough,end-of-seasonsort. AThe Garden of Cosmic Speculation, thepavementsgrey, All is beautiful, but there’s one Liss Ard in Ireland, Little Sparta, Nin- Ihearitinthedeepheart’score. -
PARK 0 1 5 Kilometers S Ri South Entrance Road Closed from Early November to Mid-May 0 1 5 Miles G Ra River S Access Sy
To West Thumb North Fa r ll ve YELLOWSTONE NATIONAL PARK 0 1 5 Kilometers s Ri South Entrance Road closed from early November to mid-May 0 1 5 Miles G ra River s access sy ad Grassy Lake L nch Ro a g Ra Reservoir k lag e F - Lake of Flagg Ranch Information Station R n the Woods to o Road not recommended 1 h a Headwaters Lodge & Cabins at Flagg Ranch s d for trailers or RVs. Trailhead A Closed in winter River G r lade C e access re e v k i R SS ERNE CARIBOU-TARGHEE ILD Glade Creek e r W Trailhead k Rive ITH a Falls n 8mi SM S NATIONAL FOREST 13km H Indian Lake IA JOHN D. ROCKEF ELLER, JR. D E D E J To South Bo C Pinyon Peak Ashton one C o reek MEMORIAL PARKWAY u 9705ft lt er Creek Steamboat eek Cr Mountain 7872ft Survey Peak 9277ft 89 C a n erry re B ek o z 191 i 287 r A C o y B o a t il e eek ey r C C r l e w e O Lizard C k r k Creek e e e re k C k e e r m C ri g il ly P z z ri G Jackson Lake North Bitch Overlook Cre ek GRAND BRIDGER-TETON NATIONAL FOREST N O ANY k B C ee EB Cr TETON WILDERNESS W Moose Arizona Island Arizona 16mi Lake k e 26km e r C S ON TETON NY o A u C t TER h OL C im IDAHO r B ilg it P ch Moose Mountain rk Pacic Creek k WYOMING Fo e Pilgrim e C 10054ft Cr re e Mountain t k s 8274ft Ea c Leeks Marina ci a P MOOSE BASIN NATIONAL Park Boundary Ranger Peak 11355ft Colter Bay Village W A k T e E N e TW RF YO r O ALLS CAN C O Colter Bay CE m A ri N g Grand View Visitor Center il L PARK P A Point KE 4 7586ft Talus Lake Cygnet Two Ocean 2 Pond Eagles Rest Peak ay Lake Trailhead B Swan 11258ft er lt Lake o Rolling Thunder -
Chapter 2 Management Plan
Chapter 2 Management Plan Mahogany Canyon in the High Rock Canyon Wilderness 2.1 INTRODUCTION This chapter contains objectives and decisions for managing the natural, physical and cultural resources described in the Act and those located in parts of the planning area not included in the National Conservation Area or designated Wilderness Areas. Background information is provided for each of these resources to establish points of reference for the decisions that follow. 2.2 PROGRAM-SPECIFIC OBJECTIVES AND DECISIONS 2.2.1 LAND HEALTH STANDARDS Land Health Standards are expressions of physical and biological condition or degree of function required for sustainable environmental health. These standards engender measurements that describe on- the-ground conditions in relation to the four fundamentals of healthy, properly functioning ecosystems that are identified at 43 CFR § 4180. These fundamentals are: • Watersheds in properly functioning physical condition; soil and plant conditions support infiltration, soil moisture storage, and the release of water that is in balance with climate and landform and maintain or improve water quality, water quantity, and timing and duration of flow. Ecological processes, including the hydrologic cycle, nutrient cycle, and energy flow, are maintained in order to support healthy biotic populations and communities. • Water quality complies with State water quality standards and achieves BLM management objectives. • Habitats are restored or maintained for listed, proposed, candidate and other special status species. BLACK ROCK-HIGH ROCK RMP 2-1 JULY 2004 Chapter 2 –Management Plan Standards are achieved through the use of guidelines developed for specific programs and uses. Because the Standards were originally applied to livestock grazing, guidelines for livestock grazing (Appendix B) will continue to apply to that use. -
Scout Songs It Goes on and on My Friends
TAPS Day is done, Fading light, Thanks and Praise Opening Songs Gone the sun, dims the sight, For our days; From the lake, And a star ‘Neath the sun, From the hills, gems the sky ‘neath the stars, From the sky, gleaming bright. ‘neath the sky; All is well, safely rest, From afar, As we go, God is nigh. drawing nigh, This we know, fall the night. God is nigh. DAY CAMP CLOSING SONG (Tune: “Yankee Doodle”) And now it’s time to say goodbye, But we won’t feel so blue; ‘Cause soon the time will come again when we’ll be back to see you. Cub Scout day camp’s lots of fun—Games and crafts and singing, So get your pals and join the fun for a week filled to the brimming! SCOUT VESPERS WE’RE ALL TOGETHER AGAIN (Tune: O Tannenbaum) We’re all together again Softly falls the light of day, We’re here, we’re here As our campfire fades away; We’re all together again Silently each Scout should ask, We’re here, we’re here “Have I done my daily task? And who knows when Have I kept my honor bright? We’ll be all together again Can I guiltless sleep tonight? Signing all together again Have I done and have I dared, We’re here, we’re here Everything to be prepared?” 32 1 TAPS Day is done, Fading light, Thanks and Praise Opening Songs Gone the sun, dims the sight, For our days; From the lake, And a star ‘Neath the sun, From the hills, gems the sky ‘neath the stars, From the sky, gleaming bright. -
Jackson Hole Vacation Planner Vacation Hole Jackson Guide’S Guide Guide’S Globe Addition Guide Guide’S Guide’S Guide Guide’S
TTypefypefaceace “Skirt” “Skirt” lightlight w weighteight GlobeGlobe Addition Addition Book Spine Book Spine Guide’s Guide’s Guide’s Guide Guide’s Guide Guide Guide Guide’sGuide’s GuideGuide™™ Jackson Hole Vacation Planner Jackson Hole Vacation2016 Planner EDITION 2016 EDITION Typeface “Skirt” light weight Globe Addition Book Spine Guide’s Guide’s Guide Guide Guide’s Guide™ Jackson Hole Vacation Planner 2016 EDITION Welcome! Jackson Hole was recognized as an outdoor paradise by the native Americans that first explored the area thousands of years before the first white mountain men stumbled upon the valley. These lucky first inhabitants were here to hunt, fish, trap and explore the rugged terrain and enjoy the abundance of natural resources. As the early white explorers trapped, hunted and mapped the region, it didn’t take long before word got out and tourism in Jackson Hole was born. Urbanites from the eastern cities made their way to this remote corner of northwest Wyoming to enjoy the impressive vistas and bounty of fish and game in the name of sport. These travelers needed guides to the area and the first trappers stepped in to fill the niche. Over time dude ranches were built to house and feed the guests in addition to roads, trails and passes through the mountains. With time newer outdoor pursuits were being realized including rafting, climbing and skiing. Today Jackson Hole is home to two of the world’s most famous national parks, world class skiing, hiking, fishing, climbing, horseback riding, snowmobiling and wildlife viewing all in a place that has been carefully protected allowing guests today to enjoy the abundance experienced by the earliest explorers. -
Josie Pearl, Prospector on Nevada's Black Rock Desert
JUNE, 1962 40c • • • • . Author's car crossing the playa of Black Rock Desert in northwestern Nevada. On Black Rock Desert Trails When Dora Tucker and Nell Murbarger first began exploring the Black Rock country in northwestern Nevada they did not realize what a high, wide and wild country it was. On the Black Rock a hundred miles doesn't mean a thing. In the 10,000 square miles of this desert wasteland there isn't a foot of pavement nor a mile of railroad— neither gasoline station nor postoffice. Antelopes out-number human beings fifty to one. There's plenty of room here for exploring. By NELL MURBARGER Photographs by the author Map by Norton Allen S AN illustration of what the want to! Ain't nothin' there!" is known as "the Black Rock country," Black Rock country affords Thanking him, we accepted his re- the desert from which it derives its in the way of variety and con- port as a favorable omen and headed name actually is a stark white alkali trast, we made a J 50-mile loop trip out into the desert. Almost invariably playa, averaging a dozen miles in out of Gerlach last June. Our previous we find our best prowling in places width and stretching for 100 miles exploring of the region had been mostly where folks have told us there "ain't from Gerlach to Kings River. Merging in the northern and eastern sections, nothin'." imperceptibly with the Black Rock on so we hadn't the slightest idea of what Rising precipitously from the dead the southwest is the section known as we might find in the southern part. -
Path to Rome Walk May 8 to 20, 2018
Path to Rome Walk May 8 to 20, 2018 “A delight—great food and wine, beautiful countryside, lovely hotels and congenial fellow travelers with whom to enjoy it all.” —Alison Anderson, Italian Lakes Walk, 2016 RAVEL a portion of the Via Francigena, the pilgrimage route that linked T Canterbury to Rome in the Middle Ages, following its route north of Rome through olive groves, vineyards and ancient cypress trees. Discover the pleasures of Central Italy’s lesser-known cities, such as Buonconvento, Bolsena, Caprarola and Calcata. With professor of humanities Elaine Treharne as our faculty leader and Peter Watson as our guide, we refresh our minds, bodies and souls on our walks, during which we stop to picnic on hearty agrarian cuisine and enjoy the peace and quiet that are hallmarks of these beautiful rural settings. At the end of our meanderings, descend from the hills of Rome via Viale Angelico to arrive at St. Peter’s Basilica, the seat of Catholicism and home to a vast store of art treasures, including the Sistine Chapel. Join us! Faculty Leader Professor Elaine Treharne joined the Stanford faculty in 2012 in the School of Humanities and Sciences as a Professor of English. She is also the director of the Center for Spatial and Textual Analysis. Her main research focuses on early medieval manuscripts, Old and Middle English religious poetry and prose, and the history of handwriting. Included in that research is her current project, which looks at the materiality of textual objects, together with the patterns that emerge in the long history of text technologies, from the earliest times (circa 70,000 B.C.E.) to the present day. -
The Forests of Tuscany (Italy) in the Last Century
Article Forest Surface Changes and Cultural Values: The Forests of Tuscany (Italy) in the Last Century Francesco Piras, Martina Venturi *, Federica Corrieri, Antonio Santoro and Mauro Agnoletti Department of Agriculture, Food, Environment and Forestry (DAGRI), University of Florence, Via San Bonaventura 13, 50145 Florence, Italy; francesco.piras@unifi.it (F.P.); federica.corrieri@unifi.it (F.C.); antonio.santoro@unifi.it (A.S.); mauro.agnoletti@unifi.it (M.A.) * Correspondence: martina.venturi@unifi.it Abstract: Despite the definition of social and cultural values as the third pillar of Sustainable Forest Management (SFM) in 2003 and the guidelines for their implementation in SFM in 2007 issued by the Ministerial Conference on the Protection of Forest in Europe (MCPFE), the importance of cultural values is not sufficiently transferred into forest planning and conservation. Tuscany is widely known for the quality of its cultural landscape, however, the abandonment of agro-pastoral surfaces as a consequence of rural areas depopulation, has led to widespread reforestation and to the abandonment of forest management. In addition, due to the interruption of a regular forest management and to the fact that most of the population lives in cities, forests are no more perceived as part of the cultural heritage, but mainly as a natural landscape. Due to this trend traditional forest management techniques, such as coppicing, have also been considered as a factor of degradation Citation: Piras, F.; Venturi, M.; and not even a historical management form. The aim of the study is therefore to analyze forest Corrieri, F.; Santoro, A.; Agnoletti, M. surface changes in Tuscany in the last century to assess the importance of cultural values. -
Chapter 17. Quartzite Gravel Northwest Wyoming
Chapter 17 Quartzite Gravel of Northwest Wyoming The quartzites of southwest Montana and adjacent Idaho extend eastward into Wyoming1 in a semi-continuous belt, as shown on Figure 16.1 of the previous chapter. This chapter will describe those deposits. Quartzite Gravel Lag John Hergenrather and I have found scattered surficial quartzites from near Interstate 15 in northeastern Idaho, just south of Lima, Montana, eastward to the northern Teton Mountains and over a four-wheel drive pass between Yellowstone and Grand Teton National Parks. These quartzites seem to have mostly formed a thin layer or lag deposit on the surface or were reworked by local mountain glaciation. This lag rep- resents the red hashed area in Figure 16.1. Quartzites on Top of the Northern Teton Mountains Probably the most fascinating quartz- ite location is on top of the northern Teton Mountains! Brent Carter and I took a Figure 17.1. Slightly dipping limestone at the top three day round trip hike to the top of Red of Red Mountain. Mountain in the northern Teton Moun- tains, 10,177 feet (3,102 m) msl!2,3 Red Mountain and Mount Moran (12,605 feet, 3,842 m msl) represent remnants of a flat-topped planation surface.2 Red Mountain is composed of slightly tilted limestones (Figure 17.1), while Mount Moran is composed of granite or gneiss with a 50-foot (15 m) thick cap of Flathead Sandstone on top (see Figure 33.7). The quartzites on top of Red Mountain are mainly a thin lag mixed with angular lime- stone cobbles and boulders (Figure 17.2). -
Hydrographic Basins Information
A p p e n d i x A - B a s i n 54 Crescent Valley Page 1 of 6 Basin 54 - Crescent Valley Crescent Valley is a semi-closed basin that is bounded on the west by the Shoshone Range, on the east by the Cortez Mountains, on the south by the Toiyabe Range, and on the north by the Dry Hills. The drainage basin is about 45 miles long, 20 miles wide, and includes an area of approximately 750 square miles. Water enters the basin primarily as precipitation and is discharged primarily through evaporation and transpiration. Relatively small quantities of water enter the basin as surface flow and ground water underflow from the adjacent Carico Lake Valley at Rocky Pass, where Cooks Creek enters the southwestern end of Crescent Valley. Ground water generally flows northeasterly along the axis of the basin. The natural flow of ground water from Crescent Valley discharges into the Humboldt River between Rose Ranch and Beowawe. It is estimated that the average annual net discharge rate is approximately 700 to 750 acre-feet annually. Many of the streams which drain snowmelt of rainfall from the mountains surrounding Crescent Valley do not reach the dry lake beds on the Valley floor: instead, they branch into smaller channels that eventually run dry. Runoff from Crescent Valley does not reach Humboldt River with the exception of Coyote Creek, an intermittent stream that flows north from the Malpais to the Humboldt River and several small ephemeral streams that flow north from the Dry Hills. Surface flow in the Carico Lake Valley coalesces into Cooks Creek, which enters Crescent Valley through Rocky Pass. -
DOE/ET /27010-2 MC Coy AREA, NEVADA Geothermal Reservoir
t -- DOE/ET /27010-2 MC COy AREA, NEVADA Geothermal Reservo ir Assessment Case History Northern Basin and Range ANNUAL REPORT January 1980 - 31 December 1980 H. D. PILKINGTON August 1981 WORK PERFORMED UNDER CONTRACT DE AC 08-79 ET 27010 At-1AX EXPLORATION, INC. 7100 West 44th Ave. Wheat Rid~~t CO 80033 r TABLE OF CONTENTS Page ABSTRACT INTRODUCTION 2 EXPLORATION HISTORY 4 Geological Studies 4 Geochemical Studies . 6 Geophys i ca 1 Studies. 10 Exploration Drilling 13 \. TAB LE OF ILLUSTRATIONS Page Figure 1. Location map for the McCoy geothermal prospect 3 Figure 2. Geologic map of the McCoy geothermal prospect, Nevada (after Adams, Moore and Struhsacker, 1980) 5 Figure 3 Geologic cross-sections through well 14-7 (top) and well 66-8 (bottom) after Pilkington, 1980. 7 Figure 4 Location map of drill holes used on geochemical study of drill cuttings. 9 Figure 5 Contour map of mercury in drill cuttings from 120-160 foot interval at McCoy (Pilkington, 1980) . 11 Figure 6 Gravity profile with automatic interpretation for density (top) compared wi th geologic cross-section (bottom) 12 Figure 7 Resistivity at 5km depth from 10 magnetotelluric inve·rsion (Te mode) and location of survey lines 14 and stations Figure 8 MT section (Te mode, 10 inversion) along line C-C' compared with geologic section (after Lange, 1980) . 15 Figure 9 Survey location map of the McCoy prospect, after Wilt etal, 1980 . 16 Figure 10 MT section (Te mode 10 inversion) along line A-A" compared with EM data, after Lange, 1980 17 Page Table I Chemical analyses of McCoy Mine well and Well 66-8 waters 8 ABSTRACT The McCoy geothermal prospect is located at the junction of the Augusta Mountains, Clan Alpine Mountains and the New Pass Range. -
THE STRATIGRAPHY and STRUCTURE of the Mccoy GEOTHERMAL PROSPECT, CHURCHILL and LANDER COUNTIES, NEVADA
DOE/ID/12079--95 DE84 012192 THE STRATIGRAPHY AND STRUCTURE OF THE McCOY GEOTHERMAL PROSPECT, CHURCHILL AND LANDER COUNTIES, NEVADA by Michael Curtis Adams June 1982 Work performed under Contract Number: DE-AC07-80ID12079 EARTH SCIENCE LABORATORY University of Utah Research Institute Salt Lake City, Utah Prepared for U.S. Department of Energy Division of Geothermal Energy TABLE OF CONTENTS ABSTRACT. 1 ACKNOWLEDGEMENT. .3 INTRODUCTION. • 4 PREVIOUS INVESTIGATIONS. .9 GEOLOGIC SETTING 10 ASH-FLOW TUF FS. 12 PRE-TERTIARY STRATIGRAPHY. 18 TERTIARY STRATIGRAPHY. 20 Extrusive Rocks. 20 Tertiary Fanglomerate. 21 Tertiary Ash-Flow Tuffs at McCoy •• 21 Older Tuffs. 22 Twt 1 • 22 Twt 2 and 3 • • 27 Twt 4 • 28 Northern Ash-Flow Tuffs (Twt 5). • 29 Edwards Creek Tuff (and Interfingering Tuff) 29 Twt 6A. • 30 Twt 6B. 34 Ts2 • • 34 Twt 6C. 35 Twt 60. • 35 Interfingering Ash-Flow Tuff. 36 Twt 6E. • 36 Twt 6F. 37 Twt 6G. • 37 Tuff of McCoy Mine. 37 Twt 7A. • • 38 Twt 7B. 3B Twt 7C. • 38 Bates Mountain Tuff. 39 Twt BA. • 39 Twt BB. • 40 Twt BC. • 40 QUATERNARY ALLUVIUM. 41 COMPOSITION AND CLASSIFICATION OF ASH-FLOW TUFFS. • 42 STRUCTURE. 46 Paleozoic Structure. • 46 Page Mesozoic Structure. .46 Tertiary Structure. .47 GEOLOGIC HISTORY. • .51 SOURCES FOR THE ASH-FLOW TUFFS AT McCOY • .55 ALTERATION AND MINERALIZATION. .59 HEAT FLOW AND SURFACE HOT WATER DEPOSITS. .60 DISCUSSION. • .62 Trend 1 • • .62 Trend 2 • • . .62 Trends 3 and 4. • • .64 Trend 5 • '. • • .65 CONCLUSIONS • • • .67 APPEND I X. • • • .69 REFERENCES. • • • .81 LIST OF ILLUSTRATIONS Figure 1. Index map of central Nevada.