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Foundation Document Crater Lake National Park Oregon August 2015
NATIONAL PARK SERVICE • U.S. DEPARTMENT OF THE INTERIOR Foundation Document Crater Lake National Park Oregon August 2015 Signatur es 8-7-2015 Foundation Document To Diamond Lake, Roseburg, and 5 Pacifc Crest National Visitor center Gasoline 0 1 2 3 4 5 Kilometers Scenic Trail (PCT) 0 1 2 3 4 5 Miles Other hiking trail Lodging Picnic area North Food service Campground UMPQUA NATIONAL Pets are prohibited Beaver on all hiking trails. Meadows Store Backcountry campsite FOREST Offroad driving is (permit required) prohibited. Cree Showers k 230 k or ) ( F ver st Rogue Ri Cascade Mountain Pass 138 Ea Lake West North Entrance Station To Bend, Eugene, and 97 To Medford and 5 Boundary Springs l i a r T c i North Entrance Road n e ROGUE RIVER c S l NATIONAL a n o i FOREST t a PUMICE DESERT N t s e r C c WINEMA if c Pa NATIONAL Oasis Butte FOREST CRATER LAKE NATIONAL PARK Red Cone Sphagnum Bog Red Cone Spring ic Trail en Cleetwood Cove Trail c S l a n o i t a Steel East N R Bay t i m s North Junction e r D C r c f i Grotto c a Cove P Watchman Overlook Crater Lake WIZARD ISLAND Cloudcap Overlook Cloudcap Lightning Bay Spring W Rim Village e s Rim Village Café & Gift Shop MOUNT SCOTT t Phantom Ship Sinnott Memorial Overlook (highest point in park) R Overlook im Rim Village Visitor Center 8929ft Kerr Notch 2721m D Crater Lake Lodge Plaikni Falls To Medford r. -
Crater Lake Reflections Summer-Fall 2018
Crater Lake National Park National Park Service Crater Lake U.S. Department of the Interior Refections Visitor Guide Summer/Fall 2018 Park News 2 ... Camping, Lodging, Food Discovering Crater Lake 3 ... Ranger Programs f Water Restrictions in Effect Please help us conserve water during 12 Great Ways to Enjoy Your Stay 4 ... Hiking Trails your visit. In March, the state of 5 ... Driving Map Oregon declared a drought emergency The frst European-American to see Crater Lake was lucky to ... In the News: Bull Trout for our county. In 8 of the past 10 survive the experience. On June 12, 1853, gold prospector John 6 years, the park has received less snow Wesley Hillman was riding his mule up a long, sloping mountain. 7 ... Feature Article: Lake Level than normal. Last winter’s snow total He was lost, tired, and not paying attention to the terrain ahead. was 15 feet below average. While 8 ... Climate Chart Suddenly, his mule stopped. Hillman sat up and found himself you’re here, please take short showers, on the edge of a clif, gazing in astonishment at “the bluest and don’t run the tap, and reuse towels most beautiful body of water I had ever seen.” He added: “If and sheets if staying overnight in park Look Inside! I had been riding a blind mule, I frmly believe I would have lodging. Thanks for your help! ridden over the edge to death and destruction.” f Leave Your Drone at Home While mules—no matter how sharp their eyesight—are no longer Operating remote-controlled aircraft permitted to approach the rim of Crater Lake, there are many in the park is prohibited. -
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 -
Crater Rim Historic District Hawaii Volcanoes National Park
National Park Service Cultural Landscape Inventory 2006 Crater Rim Historic District Hawaii Volcanoes National Park Table of Contents Executive Summary...................................................................................................................................... 1 Park Information ........................................................................................................................................... 3 Property Level and CLI Number .................................................................................................................. 3 Completion Status......................................................................................................................................... 3 Landscape Description.................................................................................................................................. 4 CLI Hierarchy Description ........................................................................................................................... 5 Location Map................................................................................................................................................ 5 Boundary Description ................................................................................................................................... 6 Regional Context .......................................................................................................................................... 6 Site Plans...................................................................................................................................................... -
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. -
West Hawai'i Covers
National Park Service U. S. Department of the Interior Crater Lake National Park Museum Management Plan Cultural Resources Pacific West Region August 2007 Crater Lake National Park Museum Management Planning Team Mary Benterou, Park Curator Crater Lake National Park Crater Lake, Oregon Kent Bush, Regional Curator, Retd. Pacific West Region Seattle, Washington (Team Leader) Kelly Cahill, Park Curator North Cascades National Park Marblemount, Washington Rick Cronenberger, Historical Architect, RA Cultural Collections Consultant Intermountain Region Denver, Colorado Scott E. Foss, Ph.D., Park Curator John Day Fossil Beds National Monument John Day, Oregon Department of the Interior National Park Service Pacific West Region 2007 Crater Lake National Park Museum Management Plan August 2007 Executive Summary The Crater Lake National Park Museum Management Plan outlines a series of issues concerning the development, management, and use of the park archives, library, and museum collections (hereafter referred to as “the collections”), and it recommends corresponding actions to address these issues. A Collections Management Plan (CMP) (precursor to the current Museum Management Plan format) was completed in 1995, and the park has had the services of a journeyman-level curator for 12 years. Despite the age and maturity of the park, these park-specific resources remain in a developmental stage. They lack status, definition, and support, and thus are not able to efficiently contribute to park operations. Few of the recommendations in the 1995 CMP have been implemented. With the continued influx of collections, the documentation program and physical facilities are in worse condition now than in 1995. These deficiencies could be corrected by the following actions: • Developing internal protocols to govern collections growth, processing, and access. -
Diamond Craters Oregon's Geologic
Text by Ellen M. Benedict, 1985 Features at stops correspond to points on a clock ago, a huge mass of hot gases, volcanic ashes, bits face. Imagine that you are standing in the middle of a of pumice and other pyroclastics (fire-broken rock) Travel And Hiking Hints clock face. Twelve o’clock is the road in front of you violently erupted. The blast – greater than the May and 6 o’clock the road behind. If you always align the 18, 1980, eruption of Mt. St. Helens – deposited a Diamond Craters is located in the high desert country clock face with the road, you should be able to locate layer of pyroclastics 30 to 130 feet thick over an area about 55 miles southeast of Burns, Oregon. It’s an the features. almost 7,000 square miles! isolated place and some precautions should be taken . when traveling in the area. Start Tour. Mileage begins halfway Pyroclastics are between milepost 40 and 41 on State normal behavior Diamond Craters has no tourist facilities. The nearest Highway 205 at the junction to Diamond. for magmas place where gasoline is sold is at Frenchglen. Turn left. (subsurface That’s the opinion held by scores of molten rocks) Keep your scientists and educators who have visited Diamond, Oregon, a small ranching community, was of rhyolitic (a vehicle on named in 1874 for Mace McCoy’s Diamond brand. volcanic material and studied the area. It has the “best and hard-packed The nearby craters soon became known as Diamond related to granite) most diverse basaltic volcanic features in the road surfaces Craters. -
Overview for Geologic Field-Trip Guides to Mount Mazama, Crater Lake Caldera, and Newberry Volcano, Oregon
Overview for Geologic Field-Trip Guides to Mount Mazama, Crater Lake Caldera, and Newberry Volcano, Oregon Scientific Investigations Report 2017–5022–J U.S. Department of the Interior U.S. Geological Survey Cover (top photo): View east-northeast from Garfield Peak on the south rim of Crater Lake caldera. Peak on skyline is 8,929 feet (2,722 meters) Mount Scott, an ~420 thousand years before present (ka) dacite stratovolcano considered to be part of Mount Mazama, the volcano that collapsed during the caldera-forming eruption ~7,700 years ago. The caldera walls in this view expose Mazama lava flows and fragmental deposits from as old as ~400 ka at Phantom Cone, adjacent to tiny Phantom Ship island, to as young as ~27 ka at Redcloud Cliff, the V-shaped face at the top of the wall left of center. The beheaded glacial valley of Kerr Notch, the low point on the caldera rim, is seen between Phantom Ship and Mount Scott. Photograph by Carly McLanahan. Cover (bottom photo): Newberry Volcano, Oregon, is the largest volcano in the Cascades volcanic arc. This north-facing view taken from the volcano’s peak, Paulina Peak (elevation 7,984 feet), encompasses much of the volcano’s 4-by-5-milewide central caldera, a volcanic depression formed in a powerful explosive eruption about 75,000 years ago. The caldera’s two lakes, Paulina Lake (left) and the slightly higher East Lake (right), are fed in part by active hot springs heated by molten rock (magma) deep beneath the caldera. The Central Pumice Cone sits between the lakes. -
Geology of the Northern Part of the Southeast Three Sisters
AN ABSTRACT OF THE THESIS OF Karl C. Wozniak for the degree of Master of Science the Department cf Geology presented on February 8, 1982 Title: Geology of the Northern Part of the Southeast Three Sisters Quadrangle, Oregon Redacted for Privacy Abstract approved: E. M. Taylorc--_, The northern part of the Southeast Three Sisters quadrangle strad- dles the crest of the central High Cascades of Oregon. The area is covered by Pleistocene and Holocene volcanic and volcaniclastic rocks that were extruded from a number of composite cones, shield volcanoes, and cinder cones. The principal eruptive centers include Sphinx Butte, The Wife, The Husband, and South Sister volcanoes. Sphinx Butte, The Wife, and The Husband are typical High Cascade shield and composite vol- canoes whose compositions are limited to basalt and basaltic andesite. South Sister is a complex composite volcano composed of a diverse assem- blage of rocks. In contrast with earlier studies, the present investi- gation finds that South Sister is not a simple accumulation of andesite and dacite lavas; nor does the eruptive sequence display obvious evolu- tionary trends or late stage divergence to basalt and rhyolite. Rather, the field relations indicate that magmas of diverse composition have been extruded from South Sister vents throughout the lifespan of this volcano. The compositional variation at South Sister is. atypical of the Oregon High Cascade platform. This variation, however, represents part of a continued pattern of late Pliocene and Pleistocene magmatic diver- sity in a local region that includes Middle Sister, South Sister, and Broken Top volcanoes. Regional and local geologic constraints combined with chemical and petrographic criteria indicate that a local subcrustal process probably produced the magmas extruded fromSouth Sister, whereas a regional subcrustal process probably producedthe magmas extruded from Sphinx Butte, The Wife, and The Husband. -
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. -
Hydrogeology of the Mckinney Butte Area: Sisters, Oregon
Portland State University PDXScholar Dissertations and Theses Dissertations and Theses 1-1-2011 Hydrogeology of the McKinney Butte Area: Sisters, Oregon Joshua Andrew Hackett Portland State University Follow this and additional works at: https://pdxscholar.library.pdx.edu/open_access_etds Let us know how access to this document benefits ou.y Recommended Citation Hackett, Joshua Andrew, "Hydrogeology of the McKinney Butte Area: Sisters, Oregon" (2011). Dissertations and Theses. Paper 371. https://doi.org/10.15760/etd.371 This Thesis is brought to you for free and open access. It has been accepted for inclusion in Dissertations and Theses by an authorized administrator of PDXScholar. Please contact us if we can make this document more accessible: [email protected]. Hydrogeology of the McKinney Butte Area: Sisters, Oregon by Joshua Andrew Hackett A thesis submitted in partial fulfillment of the requirements for the degree of Master of Science in Geology: Geohydrology Thesis Committee: Robert B. Perkins, Chair Michael Cummings Kenneth Lite, Jr. Portland State University ©2011 Abstract McKinney Butte, a late Tertiary andesite vent and flow complex, is located near the town of Sisters, Oregon, in the upper Deschutes Basin, and is situated along the structural trend that forms the eastern margin of the High Cascades graben (Sisters fault zone and Green Ridge). Rapid development and over appropriated surface water resources in this area have led to an increased dependence upon groundwater resources. A primary concern of resource managers is the potential impact of expanding groundwater use on stream flows and spring discharge. Two sets of springs (McKinney Butte Springs and Camp Polk Springs) discharge to Whychus Creek along the east flank of McKinney Butte, and during low-flow conditions supply a substantial component of the total flow in the creek.