2020 Annual Statistics and Inventory for Sunriver
Total Page：16
File Type：pdf, Size：1020Kb
Load more
Recommended publications
-
Summits on the Air – ARM for the USA (W7A
Summits on the Air – ARM for the U.S.A (W7A - Arizona) Summits on the Air U.S.A. (W7A - Arizona) Association Reference Manual Document Reference S53.1 Issue number 5.0 Date of issue 31-October 2020 Participation start date 01-Aug 2010 Authorized Date: 31-October 2020 Association Manager Pete Scola, WA7JTM Summits-on-the-Air an original concept by G3WGV and developed with G3CWI Notice “Summits on the Air” SOTA and the SOTA logo are trademarks of the Programme. This document is copyright of the Programme. All other trademarks and copyrights referenced herein are acknowledged. Document S53.1 Page 1 of 15 Summits on the Air – ARM for the U.S.A (W7A - Arizona) TABLE OF CONTENTS CHANGE CONTROL....................................................................................................................................... 3 DISCLAIMER................................................................................................................................................. 4 1 ASSOCIATION REFERENCE DATA ........................................................................................................... 5 1.1 Program Derivation ...................................................................................................................................................................................... 6 1.2 General Information ..................................................................................................................................................................................... 6 1.3 Final Ascent -
VACATION LAND the National Forests in Oregon
VACATION LAND The National Forests in Oregon High up in the mountains, where the timber is scarce and stunted and the only means of transportation is by horseback United States Department of Agriculture::Forest Service 1919 WELCOME TO THE ATIONAL PORESTS U.S.DEPARTVENT OFAGRICULTURE FOREST SIEIRVICE UNITED STATES DEPARTMENT OF AGRICULTURE DEPARTMENT CIRCULAR 4 Contribution from the Forest Service HENRY S. GRAVES. Forester DIRECTORY OF NATIONAL FORESTS IN OREGON. George H. Cecil, District Forester. District Office, Post Office Building, Portland, Oreg. NATIONAL FOREST. FOREST SUPERVISOR. HEADQUARTERS. Cascade C. R. Seitz Eugene, Oreg. 2- Crater H B Rankin Medford, Oreg. Deschutes N. G. Jacobson Bend, Oreg. H Fremont...... Gilbert D. Brown Lakeview, Oreg. -Maiheur Cy J. Bingham John Day, Oreg. L-Milaam R. M. Evans.... Baker, Oreg. - Ochoco.. V. V. Harpham Prineville, Oreg. Oregon H. Sherrard...... Portland, Oreg. Santiam C. C. Hall.. Albany, Oreg. -Siskiyou.... N. F. Macduff Grants Pass, Oreg. Siuslaw R. S. Shelley Eugene, Oreg. \-Umati1la W. W. Cryder Pendleton, Oreg. 13 .Umpqua C. Bartrum Roseburg, Oreg. j Wallowa H. W. Harris Wallowa, Oreg. S'Wenaha J. C. Kulins Walla Walla, Wash. l,Whitman R. M. Evans.... Baker, Oreg. The view on page s of the cover is a reprodtction from a photograph of Mount Jefferson, Sautiam National Forest, showing forest and snow peak. THE NATIONAL VACATION 1 ANDESTS IN OREGON AN IDEAL VACATION LAND HEN, tired of the daily grind, you say to yourself, "I need a vacation," your first thought is to get away from civili- zation and its trammels.Your next is to find interest- ing and health-giving recreation.In the National For- ests in Oregon you may find both, and much besides. -
The Land Volcanoes Made: the Buttes of the Snake River Plain from Idaho
West The Four Lost Rivers and Creeks of Eastern Idaho, and Their Surrounding Mountain Ranges East Idaho's highest peaks are all in the Lost River, Lemhi, and Pioneer Mountains. A panoramic view looking north from the “Geological Site” pull-off on U.S. 20 at Mile 273 in northern Bingham County Borah Peak (12,668 feet) is the highest in the Lost Rivers, Diamond Peak (12,197 feet) The western three of these four valleys were first known to Europeans by the names of fur trappers of the early 1800s. is the highest in the Lemhis, and Hyndman Peak (12,009 feet) is the highest in the Pioneers. The Big Lost, Little Lost, and Birch Creek valleys were named respectively after Thierry Goddin, an Iroquois trapper, Scott Peak (11,393 feet) is the highest peak in the Beaverheads. The double peak of Saddle Mountain provides an John Day, an American trapper, and Joseph Cotes, a Canadian trapper. Trappers eradicated beaver from the region in The only town of any size at the southern end of these valleys is Arco, Lemhi Mountains easily-recognized signpost of the southern Lemhis. less than a decade, and soon the trappers and the names that they had given the rivers and valleys were forgotten. which offers food, lodging, and supplies to travelers on U.S. Highways 20, Lost River Mountains 26, and 93, the last of which goes up the Big Lost River Valley. King Mountain Little Lost River Valley Saddle Mountain Smiley Mountain Shelly Peak, Howe Peak Big Lost River Valley in the White Knob Mtns Hawley Mountain Birch Creek Valley Beaverhead Mountains Timbered Dome -
GEOTHERMAL and STRUCTURAL IMPLICATIONS of MAGNETIC Anomalies OBSERVED OVER the SOUTHERN OREGON CASCADE MOUNTAINS and ADJOINING BASIN and RANGE PROVINCE
AN ABSTRACT OF THE THESIS OF WILLIAM HENRY MCLAIN for the degree of MASTER OF SCIENCE in GEOPHYSICS presented on JULY 21, 1981 Title: GEOTHERMAL AND STRUCTURAL IMPLICATIONS OF MAGNETIC ANOMALIES OBSERVED OVER THE SOUTHERN OREGON CASCADE MOUNTAINS AND ADJOINING BASIN AND RANGE PROVINCE Redacted for privacy Abstract approved: Richard W. Couch To assist in the assessment of the geothermal potential ofsouth- central Oregon and to aid in the understanding of the tectonicmode of transition between the Basin and Range province and theCascade Mountains province, personnel from the Geophysics Group in theSchool of Oceanography at Oregon State University conducted adetailed aero- magnetic survey extending from 42°OO' to 43°OO'N latitudeand 121000T to 122°45'W longitude. Spectral analysis of the aeromagnetic anomalies provided source- depth and depth-to-bottom calculations for south-centralOregon. The magnetic source-bottom depths were interpreted asCurie-point isotherm depths. Several regions with elevated Curie-point isothermdepths were mapped: (1) the Crater Lske area, (2) the Mount McLaughlin - Kiamath Lake area, and (3) the Sprague River Valley.The elevated Curie-point isotherm depths within these areas, asshallow as 4 to 6 km below sea level in the Mount McLoughlin - Klamath Lake areaand 5 to 7 kmbelow sea level in the Crater Lake area and theSprague River Valley, imply vertical temperature gradients in excess of70 °C/km and heat-flow values greater than 120mW/rn2 assuming a Curie-point temperature of 580 °C. A N40°W anomaly trend, observed on the totalfield magnetic intensity map and low-pass filtered anomaly maps, suggeststhe emplacement of volcanic intrusions occurred along apreviously umnapped fracture zone associated with Mount Mazama. -
Reconstruction of Late Pleistocene Paleoclimatic Characteristics in the Great Basin and Adjacent Areas
AN ABSTRACT OF THE THESIS OF Kenneth A. Bevis for the degree of Doctor of Philosophy in Geology presented on March 3. 1995. Title: Reconstruction of Late Pleistocene Paleoclimatic Characteristics in the Great Basin and Adjacent Areas Signature redacted for privacy. Abstract approved:. Peter U. Clark A sequence of glaciation based on relative dating parameters was established in each of nine mountain ranges located along a northwest to southeast transect through the northern Great Basin. Each sequence consists of two or three drift units. Degree of weathering suggests that the younger drift unit in a two-fold sequence and the intermediate drift unit in a three-fold sequence represents deposition during the late Pleistocene. The late Pleistocene equilibrium-line altitude (ELA) in each range was determined by reconstructing the maximum ice extent associated with these drift units and using the accumulation area ratio technique. Paleo-ELAs increase from about 2100 m in northeastern Oregon to approximately 3200 m in central Utah. Paleoclimatic conditions along the study transect were estimated by comparing modern climatic conditions at the reconstructed late Pleistocene ELAs with climatic conditions occurring at the ELAs of modem mid-latitude glaciers. Assuming no change in winter accumulation or in the seasonal distribution of precipitation from the present, a mean summer temperature depression ranging from about 9.0 °C at the northern end of the transect to about 4.0 °C at the southern end would have been necessary to sustain glaciers in these ranges during the late Pleistocene. To simulate possible changes in late Pleistocene precipitation patterns, a change in winter accumulation between 0.5 and 2.0 times the modem value resulted in a respective increase or decrease in temperature depression by approximately 2.0 °C. -
Text-Only PDF File
Geological Field Trips in Southern Idaho, Eastern Oregon, and Northern Nevada Edited by Kathleen M. Haller, and Spencer H. Wood Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government Open-File Report 2004-1222 U.S. Department of the Interior U.S. Geological Survey Geological Field Trips in Southern Idaho, Eastern Oregon, and Northern Nevada Edited by Kathleen M. Haller, and Spencer H. Wood Contents Introduction ...................................................................................................................................................... 2 The Rattlesnake Tuff and Other Miocene Silicic Volcanism in Eastern Oregon By Martin Streck and Mark Ferns ....................................................................................................... 4 The Western Margin of North America After the Antler Orogeny: Mississippian Through Late Permian History in the Basin and Range, Nevada By James H. Trexler, Jr., Patricia H. Cashman, Walter S. Snyder, and Vladimir I. Davydov......... 20 Fire and Ice in Central Idaho: Modern and Holocene Fires, Debris Flows, and Climate in the Payette River Basin, and Quaternary and Glacial Geology in the Sawtooth Mountains By Jennifer L. Pierce, Grant A. Meyer, Glenn D. Thackray, Spencer H. Wood, Kari Lundeen, Jennifer A. Borgert, and Eric Rothwell............................................................................... 38 Late-Pleistocene Equilibrium-Line Altitudes, Atmospheric Circulation, and Timing of Mountain -
Gladney and Adams Claim Report
GEOLOGY OF flm GLA.pllllY up ADAMS SA.i.'ID AND GM,VJIL fltA.N!. 8 U·t!W'I l♦ It!t p • Klamath County Lpcajion: !. J6 s., R. ?tE., sea. J2 on the 1outhwe1t aide of Ho"WRrd. :Bay, upper llama.th Lake. fwenty-one mile• north and weat of Xlamath 1alle on the Lake-o-the Wood& Forest Service road. ~e aource of the material of thia deposit is the mountains to the General: • southwest. The peaks of Mt. Harriman, Kt. Carmine, Aspen Butte, and Greylock Mountain at one time were moat likely parts of a single volcanic cone of the shield or Icelandic type. At the time of its maximum aize this cone must have been approximately 11 mile• long by 7 milea wide and risen above the plateau at least 2500 feet. Little Aspen Butte, High Knob, and Crater Mountain are probably paraaitic cones of thi1 shield which apparently, by the degree of disaection on their flank:1, were not active until the parent cone had. undergone cODSiderable eroaion. !he depoeit waa formed by streams depoaiUng their lead along the outer :margin of thia mountain. !he diatance which the streua could carry their load wa.a restricted by the ahore of Howard Bay. Consequently all the material derived from the mountain by eroaion (except the moat minute particle• and that which went into 10lution) was concentrated between the lake ehore and the steeper alopea - a distance of three to four miles. That the amount depoaited is con siderable is shown by the test pita of the gravel plant, a well, and the gravel mantle around the baae of the preaent mountains. -
Matsutake Collection Authorization Deschutes, Fremont-Winema
Matsutake Collection Authorization Deschutes, Fremont-Winema, Umpqua, and Willamette National Forests Under the authority of the Forest Supervisor, this document grants the collection, transport and sale of matsutake mushrooms from Oregon Forests including the Deschutes, Fremont-Winema, Umpqua and, and Willamette. This interim change to the matsutake permitting process is a result of the COVID-19 pandemic and an effort to maximize social distancing measures to the extent possible. The Deschutes, Fremont-Winema, Umpqua, and Willamette Forests reserve the right to revoke this authorization for noncompliance with its terms and conditions or when revocation is in the public’s interest. Any violations of these conditions may invalidate the authorization and may result in legal action including criminal violations (36 CFR 261.10(L)) and civil damage. Valid from September 8, 2020 to November 8, 2020 AUTHORIZED USER (Individual Name) (Address) (State) (Zip Code) (Signature) (Date) The authorized user agrees to hold the Government harmless from any claim for damage or loss of property, personal injury or death. The U.S. Department of Agriculture (USDA) prohibits discrimination in all its programs and activities on the basis of race, color, national origin, gender, religion, age, disability, political belief, sexual orientation, and martial or family status. (Not all prohibited bases apply to all program) Persons with disability who require alternative means of communication of the program information (Braille, large print, audiotape, etc.) should contact USDA’s TARGET Center at 202-720-2600 (Voice and TDD). To file a complaint of discrimination, write USDA, Director, Office of Civil Rights, 1400 Independence Avenue, SW Washington DC 20250-9410 or call (800) 795-3272 (voice) or (202) 720-6382 (TDD) USDA is an equal opportunity provider. -
Wildlife Specialist Report Lake of the Woods Late-Successional Reserve Project
APPENDIX A Wildlife Specialist Report Lake of the Woods Late-Successional Reserve Project USDA-Forest Service Winema National Forest Klamath Ranger District Submitted by: __Betsy Hamann________________________________ Betsy Hamann, Wildlife Biologist, FS TEAMS Date: ___4/29/04________________________ Edited on 5/27/04 to incorporate comments and new information from FWS Edited on 6/29/04 to incorporate additional information Duty Station: Lewis and Clark National Forest White Sulphur Springs Ranger District Box A, 204 W. Folsom White Sulphur Springs, Mt 59645 406-547-6011 Wildlife Specialist Report- Lake of the Woods LSR Project Wildlife Resource Area Introduction Numerous species of wildlife potentially use the project areas, including threatened, endangered, sensitive (TES), and management indicator species (MIS). See Attachment A for a list of species, habitat associations, and potential for use of the areas. The project vicinity is on the Klamath Ranger District, on the east side of the Cascade Range, west of Klamath Lake. Recreation use began at Lake of the Woods in the early 1900’s when the Forest Service took over management of the area. As access improved, recreation use increased. Today, recreational facilities at the Lake of the Woods includes two Forest Service campgrounds, five Day Use areas, three organizational camps, Lake of the Woods Resort and 218 recreation residences. As part of the NWFP (USFS 1994), the Lake of the Woods area was included as part of Late Successional Reserve (LSR) R0227 to provide late successional habitats for spotted owls and other associated species. This LSR is about 101,506 acres, with 48% on the Winema and 52% on the Rogue National Forest. -
Day 6 Ashland to Klamath Falls.Ai
Olson Mtn Seven Lakes 6884 5053 Medco Venus Pond Basin Weed Rd 7315 Agency Hill KLAMATH T JACKSON h r 4502 ee mile C 5038 Devils Peak r Camel Jupiter 7582 ROGUE RIVER 33-1E-25 7422 Hump eek e Lucifer r l 37 C o 6210 34 3105 ep Rustler 7481 Puck 3449 S a g i NATIONAL J a d o Lakes C Peak n o B Meva o c L u i Klamath r rk k 6208 g B o t a b t en Cr o l a f d h fo C l i R e s W l Lather Mtn w s l Braymill i o FOREST Agency a Cave r g a e C Luther Mtn r C 6945 r h 3484 s Mtn WNF t – C o 7153 el 4179 s s F h 5251 3450 K C 3260 i i e B M 949 Rd o ag d l i r ure o l g Santiam tt H l WINEMA d e M r L e q B a w l k a k e u Pine Ridge Tr u 200 c Peak a y p D O p i e N t r L n a Sky ke 4597 t 34-2E-29 34-3E-21 r Steiger el 4208 e C e Ch e err i y 3450 l Butte h W F i T 858 zzar 4785 d Lake r t RRNF Ish Cherry Peak e Fredenberg c erw e R oo d Butte p d L 6623 e s o ak 62 5815 n 4320 o g e r k La M b P r reek 32 u ke N C e o C ot Crater Lake Hwy – e a o Chiloquin Cre r s e r s F 35-3E-3 h Heavenly Twin el 4179 g a 3419 e B l d e C u l R k k o t a Lakes t r i e F y c WINEMA a v e Upper F i 3770 Lakes C s a e h r e Rock r l t 34 t P l t k s t r e a eek r o H u o h r l i C Butte c C a w B 32 n N Imagination y n 97 Smith NATIONAL t a n Round Top L 5810 #25#25 - 20122012 Falls i R ia H r Peak u Rock 3240 3690 e R 6495 E q h 6640 Klamath o c Red Lake el 4139 d l I Rancheria Rd y i Sout n h i ROGUE RIVER h L WNF ButteBut w c C te F T RRNF o S r n k O 3220 B FallsFalls e IVER 5805 W ilderness 980 R E C g Q E r el 22536536 W ODSODS RestRest K StopStop y e -
Or Wild and Scenic Rivers System
Cascades Ecoregion ◆ Introduction 115 Young Volcanoes and Old Forests Cascades Ecoregion he Oregon portion of the Cascades Ecoregion encompasses 7.2 million growth forests. These include Roosevelt elk, black-tailed deer, beaver, black bear, coyote, acres and contains the highest mountains in the state. The Cascades marten, fisher, cougar, raccoon, rabbits, squirrels and (probably) lynx. Bird species Ecoregion is the backbone of Oregon, stretching lengthwise from the include the northern spotted owl and other owls, blue and ruffed grouse, band-tailed T Columbia River Gorge almost to the California border. Its width is pigeon, mountain quail, hawks, numerous songbirds, pileated woodpecker and other defined by the Willamette Valley and Klamath Mountains Ecoregions woodpeckers, bald eagle, golden eagle, osprey and peregrine falcon. Fish species include on the west and the Eastern Cascade Slope and Foothills Ecoregion on the east. The Pacific salmon stocks, bull trout and rainbow trout. Five of the eleven species endemic to highest peak is Mount Hood (11,239’). This ecoregion also extends northward into the ecoregion are amphibians: Pacific giant salamander, Cascade seep salamander, Washington and has three unusual outlier terrestrial “islands:” Paulina Mountains Oregon slender salamander, Larch Mountain salamander and the Cascades frog. southeast of Bend, Black Butte near Sisters and Mount Shasta in California. The effects of latitude on forest type are obvious in the Cascades as they range from Geologically, the ecoregion consists of two mountain ranges: the High Cascades the Columbia River to the California border. The effects of elevation are dramatic as well. and the Western (sometimes called “Old”) Cascades. Both are parallel north-south Beginning at the Willamette Valley margin and heading both eastward and ranges, but they are geologically distinct, as one is much older than the other. -
Geologic Processes in the RWMC
INEL-95/0519 Geologic Processes in the RWMC Area, Idaho National Engineering Laboratory: Implications for Long Term Stability and Soil Erosion at the Radioactive Waste Management Complex W. R. Hackett J. A. Tullis R. P. Smith S. J. Miller T. V. Dechert* P. A. McDaniel* A. L Falen* September 1995 Idaho National Engineering Laboratory Lockheed Martin Idaho Technologies Idaho Falls, Idaho 83415 and WW a Ol University of Idaho College of Agriculture Soil Science Division Moscow, Idaho 83844-2339 Prepared for the U.S. Department of Energy Assistant Secretary for Environmental Management Under DOE Idaho Operations Office Contract DE-AC07-94ID13223 DISTRIBUTION OF THIS DOCUMENT IS UMumrrm DISCLAIMER This report was prepared as an account of work sponsored by an agency of the United States Government. Neither the United States Government nor any agency thereof, nor any of their employees, make any warranty, express or implied, or assumes any legal liability or responsibility for the accuracy, completeness, or usefulness of any information, apparatus, product, or process disclosed, or represents that its use would not infringe privately owned rights. Reference herein to any specific commercial product, process, or service by trade name, trademark, manufacturer, or otherwise does not necessarily constitute or imply its endorsement, recommendation, or favoring by the United States Government or any agency thereof. The views and opinions of authors expressed herein do not necessarily state or reflect those of the United States Government or any agency thereof. DISCLAIMER Portions of this document may be illegible in electronic image products. Images are produced from the best available original document.