BRIGHAM YOUNG UNIVERSITY GEOLOGY STUDIES Volume 42, Part I, 1997
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LZ Streets County Boundary Printed 4/23/2018 ®
H R A I L R FR526 D A R G R HORSE SAD I DLE M SO E A A AP 9 STO RIN M N NE G 8 R TAIL RAN P I CH R E O O HORN L BUFFALO C C E O C TW K W A V O T O F N E B H R R C R W E RAWA S DIAMOND PEAK LZ AR E 2 A L E S A D 0 A V S 2 M O K L E A WALNO C R O B F B E O C M R N # K R * N E L I D W R A A E C G L K O D N T A A O D BIG HOLE A E S C N R R E A R R P H N E I E F D R B 8 E R Y R 9 V O P R L F SOAPSTONE PRAIRIE NA NORTH LOT LZ P O F S T R E C C A Y D U U H IX D Y W T M K A C D B L K W E S N F # N * M N T F E A S U L O Y Y IT A O L T M S B N O E Y Y V E M C O B R S D N R K O W A R I I A E N E O A R L R N E H I C IG L C L R W R AN I G 4 W E T D S E C S P F A B 3 R R N 7 A I E U T 8 NG I P F P N S G E R A Q O R F S L R L T H C T I S Y P R V 6 I E F C 4 0 I S N 5 A 2 O N E C D A D S R R C L G R 3 F N R G D 1 W T E N 2 U R N S 0 AIL L E I E O C R RED MOUNTAIN OPEN SPACE LZ K 3 RE K K O A O EK R L E M C Z R M N TIM P L N E BER # S E *N O C G T W H I O K R L N N Y E E N L O K H E C I C N C R L A Y C O I I C L H A O V T L P CR80C & FR87C LZ T E VIRGINIA DALE LZ I N A R G C N R RA ED O N J E E A A L P A R I S SH W E L 2 B R C F Y E R A T *# *# P F 8 1 S H C R C A D 8 O E 1 T A 7 E T A HOHNHOLZ LAKES LZ K R AT R E SOAPSTONE PRAIRIE NA SOUTH LOT LZ R V R N I C O R M M P E T R F F E I T 200 B U E W FR L E P # B S L E # * Y * R E K IN E T S C T I H L O 5 C N G K 4 E LS CREEK R I C DEVI D O F A 5 C N S D N E E W R EATON RESERVOIR LZ A I T F I N P U R E BE R A P E R K Q A D 5 R L 9 P *# N O V N K E I A T S T D L I M U D I CR80C MM 22 LZ L D M H E R E Y *# E C B V U R S L CR80C & CR89 LZ T L T DE D E M R S # W PA N E * A R T U L K HOMESTEAD LZ JOY A R N C 0 O J K CANYON O 4 E W A P HA F W 5 R R # L IV ROUND BUTTE LZ * X E R I ATE D F D M R CR92 W IV # B E * CH E E N L F A AN D R R H E R C 5 T J 2 O 3 R P R 1 . -
Deschutes National Forest
Deschutes National Forest Summer Trail Access and Conditions Update KNOW BEFORE YOU GO! Updated July 13, 2013 Summer Trail Highlights Summer weather, high summer/holiday use at many recreation sites and trails. Remaining snow limited to South Sister, Broken Top, Road 370 and a few patches on trails and the volcanoes above 6,000’ along the Crest. Reports of heavy blowdown (50+ trees/mile) on some trails. Wilderness Permits required. Broken Top TH and 370 Road from Todd Lake to Road 4601 are blocked by snow and closed until determined safe. June 29 photo from Broken Top. Nearly all Wilderness Tumalo Falls road open to vehicle trails are snow free with a few patches likely remaining traffic. North Fork Trail is cleared of along the PCT and on climber trails and routes up the blow down; open to bikers uphill only. volcano peaks. 16 Road and Three Creek Lakes are open and snow free. Tumalo Mt. Trail may yet have a patch or two of snow but very passible. Green Lks/Moraine Lks Trails are snow free with light blowdown. PCT has patchy snow above 6,000’ with some trail clearing in progress. Mosquito populations are highly variable with some backcountry lakes and riparian areas at high levels. Go prepared with your Ten Essential Systems: Navigation (map and compass) Sun protection (sunglasses/sunscreen) Ongoing Suttle Lake trail project with Deschutes NF Trail Insulation (extra clothing) Crew constructing one of many rock retaining walls. For Illumination (headlamp/flashlight) Your safety, please use caution and leash dogs when First-aid supplies approaching trail crews working the various trails on the Fire(waterproofmatches/lighter/candles) Deschutes. -
Central Cascades Wilderness Strategies Project Deschutes and Willamette National Forests Existing Conditions and Trends by Wilderness Area
May 31, 2017 Central Cascades Wilderness Strategies Project Deschutes and Willamette National Forests Existing Conditions and Trends by Wilderness Area Summary of Central Cascades Wilderness Areas ......................................................................................... 1 Mount Jefferson Wilderness ....................................................................................................................... 10 Mount Washington Wilderness .................................................................................................................. 22 Three Sisters Wilderness ............................................................................................................................. 28 Waldo Lake Wilderness ............................................................................................................................... 41 Diamond Peak Wilderness .......................................................................................................................... 43 Appendix A – Wilderness Solitude Monitoring ........................................................................................... 52 Appendix B – Standard Wilderness Regulations Concerning Visitor Use ................................................... 57 Summary of Central Cascades Wilderness Areas Introduction This document presents the current conditions for visitor management-related parameters in three themes: social, biophysical, and managerial settings. Conditions are described separately for each of -
Quaternary Fault and Fold Database of the United States
Jump to Navigation Quaternary Fault and Fold Database of the United States As of January 12, 2017, the USGS maintains a limited number of metadata fields that characterize the Quaternary faults and folds of the United States. For the most up-to-date information, please refer to the interactive fault map. Diamond Valley fault (Class A) No. 1161 Last Review Date: 2000-06-06 citation for this record: Anderson, R.E., compiler, 2000, Fault number 1161, Diamond Valley fault, in Quaternary fault and fold database of the United States: U.S. Geological Survey website, https://earthquakes.usgs.gov/hazards/qfaults, accessed 12/14/2020 02:17 PM. Synopsis The Diamond Valley fault is along the precipitous east-facing bedrock escarpment of the Sulphur Spring Range adjacent to Diamond Valley near the southeastern corner of the Winnemucca 1:250,000 map. It includes a subparallel 6-km-long fault along the east margin of Union Mountain in Elko County. The Sulphur Spring Range is an east-tilted structural block similar to many ranges in the region. The range is also a north-trending horst, and the Diamond Valley fault is the east-bounding structure of the horst. The precipitous, convex-eastward bedrock escarpment along the fault is little incised by transverse drainages, and generally lacks the faceted spurs and wineglass valleys that tend to characterize the geomorphology of major active range blocks. The fault probably juxtaposes Quaternary alluvium against bedrock, but fault scarps and (or) lineaments on Quaternary surficial deposits or erosion surfaces are apparently lacking. Name Modified from dePolo (1998 #2845), who applied the name comments Diamond Valley fault zone to a single-trace north-striking fault mapped by Dohrenwend and Moring (1991 #282) at the base of the precipitous east-facing bedrock escarpment of the Sulphur Spring Range adjacent to Diamond Valley. -
Volcanic Vistas Discover National Forests in Central Oregon Summer 2009 Celebrating the Re-Opening of Lava Lands Visitor Center Inside
Volcanic Vistas Discover National Forests in Central Oregon Summer 2009 Celebrating the re-opening of Lava Lands Visitor Center Inside.... Be Safe! 2 LAWRENCE A. CHITWOOD Go To Special Places 3 EXHIBIT HALL Lava Lands Visitor Center 4-5 DEDICATED MAY 30, 2009 Experience Today 6 For a Better Tomorrow 7 The Exhibit Hall at Lava Lands Visitor Center is dedicated in memory of Explore Newberry Volcano 8-9 Larry Chitwood with deep gratitude for his significant contributions enlightening many students of the landscape now and in the future. Forest Restoration 10 Discover the Natural World 11-13 Lawrence A. Chitwood Discovery in the Kids Corner 14 (August 4, 1942 - January 4, 2008) Take the Road Less Traveled 15 Larry was a geologist for the Deschutes National Forest from 1972 until his Get High on Nature 16 retirement in June 2007. Larry was deeply involved in the creation of Newberry National Volcanic Monument and with the exhibits dedicated in 2009 at Lava Lands What's Your Interest? Visitor Center. He was well known throughout the The Deschutes and Ochoco National Forests are a recre- geologic and scientific communities for his enthusiastic support for those wishing ation haven. There are 2.5 million acres of forest including to learn more about Central Oregon. seven wilderness areas comprising 200,000 acres, six rivers, Larry was a gifted storyteller and an ever- 157 lakes and reservoirs, approximately 1,600 miles of trails, flowing source of knowledge. Lava Lands Visitor Center and the unique landscape of Newberry National Volcanic Monument. Explore snow- capped mountains or splash through whitewater rapids; there is something for everyone. -
Paleozoic Geology of the Dobbin Summit-Clear Creek Area, Monitor
AN ABSTRACT OF THE THESIS OF DIANE CAROL WISE for the degree of MASTER OF SCIENCE in Geology presented on August 13, 1976 Title: PALEOZOIC GEOLOGY OF THE DOBBIN SUMMIT- CLEAR CREEK AREA, MONITOR RANGE, NYiE COUNTY, NEVADA Abstract approved: Redacted for Privacy son Paleozoic limestones, dolomites, quartz arenites, and other clastic rocks were mapped in the vicinity of Dobbin Summit and Clear Creek in the central Monitor Range. Sedimentary rock units present in this area represent the shallow-shelf eastern assemblage and basin and also the basin-slope facies of the traditional limestone- clastic assemblage. The four oldest, Ordovician, units were deposited in shallow shelf environments. The Lower Ordovician Goodwin Formation is composed of about 1200 feet of calcareous shales and thin-bedded limestones. The overlying Antelope Valley Limestone is about 500 feet thick and consists of wackestones, packstones, and rare algal grainstones.The Copenhagen Formation (135 feet thick) is the highest regressive deposit of sandstone, siltstone, and limestone below the transgressive Eureka Quartzite.The Eureka is a quartz arenite 181 feet thick, with an intercalated shallow marine dolomite member. The transition from shallow to deep water conditions can be seen in the change from algal boundstones to laminated lime mud- stones in the Hanson Creek Formation (190 feet thick).The super- jacent Roberts Mountains Formation (285 feet thick) is composed of lime mudstones and allodapic beds deposited in basinal, deep water conditions.During earliest Devonian -
Lassen Volcanic National Park
LASSEN VOLCANIC NATIONAL PARK • CALIFORNIA • UNITED STATES DEPARTMENT OF THE INTERIOR RATIONAL PARK SERVICE UNITED STATES DEPARTMENT OF THE INTERIOR HAROLD L. ICKES, Secretary NATIONAL PARK SERVICE ARNO B. CAMMERER, Director LASSEN VOLCANIC NATIONAL PARK CALIFORNIA SEASON FROM JUNE 1 TO SEPTEMBER IS UNITED STATES GOVERNMENT PRINTING OFFICE WASHINGTON : 1934 RULES AND REGULATIONS The park regulations are designed for the protection of the natural beauties as well as for the comfort and convenience of visitors. The com plete regulations may be seen at the office of the superintendent of the park. The following synopsis is for the general guidance of visitors, who are requested to assist in the administration of the park by observing CONTENTS the rules. PAGE Automobiles.—Many sharp unexpected curves exist on the Lassen Peak Loop Highway, and fast driving—over 25 miles per hour in most places—is GEOLOGIC HISTORY 2 dangerous. Drive slowly, keeping always well to the right, and enjoy the THE ANCIENT BROKEOFF CRATER 5 scenery. Specimens and souvenirs.—In order that future visitors may enjoy the SOLFATARAS 6 park unimpaired and unmolested, it is strictly prohibited to break any THE CINDER CONE 8 formation; to take any minerals, lava, pumace, sulphur, or other rock MOUNTAINS 9 specimens; to injure or molest or disturb any animal, bird, tree, flower, or shrub in the park. Driving nails in trees or cutting the bark of trees in OTHER INTERESTING FEATURES I0 camp grounds is likewise prohibited and strictly enforced. Dead wood WILD ANIMALS :: may be gathered for camp fires. Trash.—Scraps of paper, lunch refuse, orange peelings, kodak cartons, FISHING :4 chewing-gum wrappers, and similar trash scattered along the roads and CAMPING r5 trails and camp grounds and parking areas are most objectionable and unsightly. -
Summits on the Air – ARM for USA - Colorado (WØC)
Summits on the Air – ARM for USA - Colorado (WØC) Summits on the Air USA - Colorado (WØC) Association Reference Manual Document Reference S46.1 Issue number 3.2 Date of issue 15-June-2021 Participation start date 01-May-2010 Authorised Date: 15-June-2021 obo SOTA Management Team Association Manager Matt Schnizer KØMOS 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. Page 1 of 11 Document S46.1 V3.2 Summits on the Air – ARM for USA - Colorado (WØC) Change Control Date Version Details 01-May-10 1.0 First formal issue of this document 01-Aug-11 2.0 Updated Version including all qualified CO Peaks, North Dakota, and South Dakota Peaks 01-Dec-11 2.1 Corrections to document for consistency between sections. 31-Mar-14 2.2 Convert WØ to WØC for Colorado only Association. Remove South Dakota and North Dakota Regions. Minor grammatical changes. Clarification of SOTA Rule 3.7.3 “Final Access”. Matt Schnizer K0MOS becomes the new W0C Association Manager. 04/30/16 2.3 Updated Disclaimer Updated 2.0 Program Derivation: Changed prominence from 500 ft to 150m (492 ft) Updated 3.0 General information: Added valid FCC license Corrected conversion factor (ft to m) and recalculated all summits 1-Apr-2017 3.0 Acquired new Summit List from ListsofJohn.com: 64 new summits (37 for P500 ft to P150 m change and 27 new) and 3 deletes due to prom corrections. -
The Regular Meeting of the Incline Village General Improvement District Will Be Held Starting at 6:00 P.M
The regular meeting of the Incline Village General Improvement District will be held starting at 6:00 p.m. on Wednesday, December 10, 2014 in the Boardroom, 893 Southwood Boulevard, Incline Village, Nevada. A. PLEDGE OF ALLEGIANCE* B. ROLL CALL OF THE IVGID BOARD OF TRUSTEES* C. ROLL CALL OF THE IVGID BOARD OF TRUSTEES-ELECTS* Tim Callicrate Kendra Wong D. PUBLIC COMMENTS* (During the Public Comment section of the agenda, the public may comment on any subject pertaining to Incline Village General Improvement District, that is in Reports and/or on the Consent Calendar and/or is not on the agenda for action. Comments from the public, relating to a General Business agenda item, will be taken during the Board's consideration of that item. When recognized by the Chair, speakers are requested to come to the podium at the front of the room, state their name and address, and direct their comments to the Chair. All speakers are made aware that their comments will be included in the minutes of the meeting. Speaking time is limited to three minutes and yielding of time is prohibited. Persons are invited to submit comments in writing on the agenda items and/or attend and make comment. The Chair may or may not provide a response or may take the comment under advisement. The Board of Trustees conducts the business of Incline Village and Crystal Bay and its citizens during its meetings. The Chair may order the removal of any person whose conduct disrupts the orderly, efficient or safe conduct of the meeting. -
STRATIGRAPHY and STRUCTURE of the SOUTHERN SULPHUR SPRING RANGE, EUREKA COUNTY, NEVADA Redacted for Privacy Abstract Approved: U G
AN ABSTRACT OF THE THESES OF Joseph T. Lipka IC for the degree ofMaster of Sciencein Geology presented on April 17, 1987 Title:STRATIGRAPHY AND STRUCTURE OF THE SOUTHERN SULPHUR SPRING RANGE, EUREKA COUNTY, NEVADA Redacted for Privacy Abstract approved: U G. Johnson Early Paleozoic limestones and dolomites of the shallow shelf transitional facies belt were mapped in the southern Sulphur Spring Range, Eureka County, Nevada.The four youngest units in the map area are in fault contact with the Lower Devonian rocks and wereprobably transported westward, along a low-angle normal fault. The minoirlal dolomites of the Hanson Creek Formation, dated as latest Ordovician in the map area, were deposited in a low-energy lagoon.Overlying the Hanson Creek Formation, with a gradational contact, is the lower member ofthe Lone Mountain Dolomite, a probable reef complex.The exposed thickness of the lower Lone Mountain Dolomite is estimated to be 250 feet.The Lower Devonian Old Whalen Member of the Lone Mountain Dolomite is composed of well-bedded, alternating brown and gray dolomites.The repetition of rock types in the Old Whalen Member indicates recurring shallow marine environments on a broad carbonate platform.The Old Whalen is estimated to be 1400 feet thick.Directly overlying the Old Whalen Member, is the Kobeh Member of the Mc Colley Canyon Formation.Rocks of the Mc Colley Canyon Formation were deposited on a shallow shelf under normal marine conditions.The mid-Lower Devonian Kobeh Member is sparsely to abundantly fosciliferous and varies from a peloidal wackestone to a peloidal sandy wackestone to a sandy peloidal packstone.The thickness is 276 feet.Overlying the Kobeh Member are the abundantly fossiliferous beds of the lower part of the Bartine. -
High Elevation Surveys, Willamette NF
High Elevation Bryophyte Surveys Willamette National Forest Final Report March 2013 Project Objectives Our objective was to survey high priority, high elevation habitat for rocky outcrop and lakeside sensitive and strategic non vascular species on the Willamette National Forest during 2012. Few of these species are documented and most are suspected on the forest. Surveys in this habitat provide information on the range and rarity of these species. All surveys and special status species that were found in surveys (highlighted in red) have been entered into the NRIS TESP Database. Species codes from the USDA PLANTS database are used below for common tree species. Sweet Home District Surveys Surveys were conducted at upper Gordon Lake, Riggs Lake, Don Lake, Silver Lake, Crescent Lake, North Peak Lake, Heart Lake and Gordon Meadows. Cliffs adjacent to lakes were also surveyed. Surveys occurred in August and September, 2012. Surveyors were Ryan Murdoff, Alice Smith, Kate Richards and Anna Bonnette. Collections ranged from 0-10 bryophytes per site. Gordon Meadows 8/20/2012 T14S, R4E, Section 11 - UTM 0555208 4913002 Sphagnum sp., Potentilla palustris, Caltha biflora, Drosera rotundifolia, Hypericum anagalloides, Apargidium boreale, Kalmia occidentalis Collected 9 liverworts ; Alice Smith Upper Gordon Lake and meadow and cliff southwest of Upper Gordon Lake 9/17/2012 T14S, R5E, Section 18 - UTM 0558382 4911742 Gordon Lake: Sphagnum sp., Potentilla palustris, Menyanthes trifoliata, Carex lenticularis, Calamagrostis canadensis, Cicuta douglasii, -
DIAMOND PEAKS Information Guide
DIAMOND PEAKS Information Guide COMMUNITY: Pristine one plus acre dream sites located in Southern Central Oregon near the Diamond Peak Wilderness Area and only minutes from Crescent Lake, Odell Lake, Waldo Lake, Davis Lake and the Willamette Pass Ski Resort. LOCATION: We are located off Highway 58 (Willamette Pass) near Crescent Lake Junction, approximately 75 miles east of Eugene, 65 miles south of Bend, and 3 ½ hours south of Portland. We are situated in the Oregon Cascade Range adjacent to the Diamond Peak Wilderness Area and the Deschutes National Forest in one of Oregon's most beautiful areas. ELEVATION: Approximately 4600 feet, dry and healthy. TREES: Douglas Fir, Noble Fir, Cedar, Lodge pole and Ponderosa Pine. Ground cover is native bunch grass and deer forage, manzanita, wild strawberries and serviceberry. TOPOGRAPHY: Sloped to gently rolling with a spectacular view of surrounding peaks and wilderness area. SOIL: Sandy volcanic soil – there is no fill on any home site. RAIN & SNOW: Total approximately 160 inches per year, approximately 25" rain. Snow on ground November to March. Young and old enjoy the winter season with snowmobiles and cross-country skiing. RECREATIONAL Unlimited!! - Only minutes away, including: OPPORTUNITIES: Downhill skiing, cross-country skiing, snowmobiling, sledding, mountain biking, water-skiing, boating, fly fishing, lake fishing, bird watching, hiking, sailing, wind surfing, swimming & sunbathing on Crescent Lake Beaches, Horseback riding. LAKES & RIVERS: More than 80 lakes, rivers, streams and reservoirs within one hour. Odell Lake and Crescent Lake only 5 minutes away. FISHING: Brook Trout, Rainbow Trout, Dolly Varden, German Brown Trout, Mackinaws, Kokanee, Bass and Atlantic Landlocked Salmon are from 3 minutes to 1 hour.