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Parrott's Metal 18 SUMMER ADVENTURES, DAILY COURIER, Grants Pass, Oregon • SUNDAY, JUNE 27, 2021 CCommittedommitted ttoo TTopop QQualityuality RRoofingoofing & SSidingiding Custom Metal Fabrication Available Southern Oregon’s Premier Metal Roofing • Custom Forming - Flashing • Metal Building Components • On-Site Forming Available Whether you have a home, farm, ranch, mini storage unit, strip mall, or a large commerical building, Parrott’s Metal, Inc. will give you roofing manufactured to the specs you need. Our roofs are constructed to last and made of materials that will enhance the appearance of your facility for years to come. We can help you with colors, matching your materials, and getting the feel you SCOTT STODDARD/Daily Courier might be looking for. Hikers descend to the shore of Crater Lake via the 1.1-mile Cleetwood Cove Trail in 2020. The historic Crater Lake Lodge over- METAL ROOFS . Crater From 15 looks the lake and has 71 rooms for guests. Rooms are available for reservation from THAT ARE MADE TO LAST now until Oct. 10. Room rates start at $197, The season. The park is open year- but are subject to change. round, though the Watchman Peak and top Located seven miles from the lake rim, half of Garfield Peak trails as well as East The Cabins at Mazama Village are open Rim Drive and Pinnacles Road are closed from now until Sept. 26. The 40 cabins in winter. The Cleetwood Cove Trail also start at $165 a night. The Mazama Village remains closed due to rockfall, treefall Campground is open from now until Sept. and erosion. All other park roads and all 27. Tent sites are $21 a night and RV sites three entrances, North, South and West, range from $31 to $42 a night depending on are open now. hook-ups. All of the 214 sites are first- Still closed. At the time of publication come, first-serve during June but will in mid-June, both park visitor centers, require reservations July to September by Lost Creek Campground, all boat tours, either calling 888-774-2728 or visiting trav- and the Crater Lake trolley remained PARROTT’S METAL elcraterlake.com. The Lost Creek Camp- closed due to the pandemic. ground will remain closed for the 2021 sea- 992 Ort Lane, Merlin • 541-955-8077 Reserve early. For those looking to son due to COVID-19 restrictions. spend multiple days in the park, reserving Backpackers can obtain a free back- a room, cabin or campsite can make the country permit day-of at the Crater Lake trip go smoothly. Reserve online at travel- www.parrottsmetal.com craterlake.com or call 866-292-6720. Turn to LAKE, Page 19.
Recommended publications
  • 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.
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  • 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.
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  • USGS Scientific Investigations Map 2832, Pamphlet
    Geologic Map of Mount Mazama and Crater Lake Caldera, Oregon By Charles R. Bacon Pamphlet to accompany Scientific Investigations Map 2832 View from the south-southwest rim of Crater Lake caldera showing the caldera wall from Hillman Peak on the west to Cleetwood Cove on the north. Crater Lake fills half of the 8- by 10-km-diameter caldera formed during the climactic eruption of Mount Mazama volcano approximately 7,700 years ago. Volcanic rocks exposed in the caldera walls and on the flanks record over 400,000 years of eruptive history. The exposed cinder cone and andesite lava flows on Wizard Island represent only 2 percent of the total volume of postcaldera volcanic rock that is largely covered by Crater Lake. Beyond Wizard Island, the great cliff of Llao Rock, rhyodacite lava emplaced 100–200 years before the caldera-forming eruption, dominates the northwest caldera wall where andesite lava flows at the lakeshore are approximately 150,000 years old. 2008 U.S. Department of the Interior U.S. Geological Survey This page intentionally left blank. CONTENTS Introduction . 1 Physiography and access . 1 Methods . 1 Geologic setting . 4 Eruptive history . 5 Regional volcanism . 6 Pre-Mazama silicic rocks . 6 Mount Mazama . 7 Preclimactic rhyodacites . 9 The climactic eruption . 10 Postcaldera volcanism . .11 Submerged caldera walls and floor . .11 Glaciation . .11 Geothermal phenomena . 12 Hazards . 13 Volcanic hazards . 13 Earthquake hazards . 14 Acknowledgments . 14 Description of map units . 14 Sedimentary deposits . 15 Volcanic rocks . 15 Regional volcanism, northwest . 15 Regional volcanism, southwest . 17 Mount Mazama . 20 Regional volcanism, east . 38 References cited .
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  • Rogue Gorge (Mt
    Rogue Gorge (Mt. Stella) Roadless Area-- T30S R3E (primarily in portions of Sections 23, 26, 33, 34 & 35) Rogue River-Siskiyou National Forest--High Cascades Ranger District Upper, higher elevation trail provides two expansive summit top views of the Crater Lake Rim and crest of the southern Cascades. Additionally, two, lower, old growth-lined trails closely parallel the upper Rogue River within this same roadless area. A longer 7 mile, (north-south) river trail, follows just above the Rogue River’s westside. While a shorter 3.5 mile trail provides easy access opportunities on the opposite shore to outstanding riverside views of the geologically remarkable “Rogue Gorge” and “Natural Bridge”— the latter being the southern access to the riverside portion of this remarkable roadless area. All 4 recommended hikes (described below) in this most varied roadless area are easily accessible from the main Crater Lake Hwy. 62 (& Hwy. 230). Also, nearby and outside this proposed Wilderness area are 3 local area campgrounds, a restaurant, rustic cabins, and a small store. Upper Rogue River along trail #1034A at the confluence with Union Creek. Rogue Gorge Roadless Area—Page 2 The 2,300 acres Rogue Gorge proposed Wilderness area, bordered along its east side by the upper Rogue River, provides unspoiled vistas along the river and the Crater Lake/Rogue-Umpqua Scenic Highway. The lower elevations of this old growth dominated, riverside roadless area provide a scenic backdrop for the Forest Service’s Farewell Bend and Union Creek Campgrounds, as well as the geologically remarkable “Rogue (River) Gorge”. All described trailheads below are located just off the Crater Lake Highway 62-230, immediately north and south of the 56 mile post at Union Creek (private restaurant and resort).
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  • Best of the West : USA 2019
    FMC Travel Club A subsidiary of Federated Mountain Clubs of New Zealand (Inc.) www.fmc.org.nz Club Convenor : John Dobbs Travel Smart Napier Civic Court, Dickens Street, Napier 4110 P : 06 8352222 E : [email protected] Best of the West : USA 2019 26th May to 27th June 2019 – 32 days $8795 from San Diego to Seattle Trip leader : Phillip Donnell (based on a minimum of 8 participants and subject to currency fluctuations) This an estimated price as at September 2018 Any payment by visa or mastercard adds $275 to the final price PRICE INCLUDES : • All accommodations inclusive of taxes, mostly twin share rooms in hotels, motels etc • Transport – hired minivan for the trip duration • The services of an experienced and knowledgeable Kiwi leader throughout • All breakfasts and 2 special dinners (welcome and farewell) • National park fees, historic site entry fees, and payment to FMC PRICE DOES NOT INCLUDE : • Flights to San Diego and from Seattle • Lunches, dinners not otherwise included • Any optional activities or choices, personal expenses outside of the inclusions • Travel insurance (mandatory) Trip Leader Phillip Donnell lives in sunny Tauranga with his wife Katrina. He has three married children and nine grandchildren. He has been involved in outdoor activities for more than 40 years, leading hundreds of tramping expeditions in New Zealand and overseas, as well as extensive involvement in kayaking and mountain-biking. He has also run more than 100 marathons and 110 half-marathons. He has an M.A. in Geography, which has given him a deep enthusiasm for travel and for exploring places.
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  • Mount Mazama and Crater Lake: a Study of the Botanical and Human Responses to a Geologic Event
    AN ABSTRACT OF THE THESIS OF Robyn A. Green for the degree of Master of Arts in Interdisciplinary Studies in Geology. Botany and Plant Pathology. and Anthropology presented on June 3. 1998. Title: Mount Mazama and Crater Lake: A Study of the Botanical and Human Responses to a Geologic Event Abstract approved: / Robert J. Lillie Crater Lake, located in the southern Cascade mountains of Oregon, is the seventh deepest lake in the world. Unlike a majority of the deepest lakes in the world, found in continental rift valleys, Crater Lake is in the caldera of a volcano. For the young at heart and mind, those willing to descend (and ascend) about 700 feet to Cleetwood Cove can undertake a boat tour of Crater Lake. From the boat, Crater Lake is more than just a beautiful blue lake; it becomes the inside of a volcano, where the response of people and plants to a geologic event can be investigated. The catastrophic eruption of Mount Mazama 7,700 years ago affected both plant and human populations. Before pumice and ash from the volcano blanketed the landscape like freshly fallen snow, the forests to the east of Mount Mazama were dominated by ponderosa and lodgepole pine. Within the immediate vicinity of the volcano all life was obliterated; the force of the eruptive material toppled vegetation and buried it with ash and pumice. Through the recovery process of succession, life has slowly returned to Crater Lake. Forests surrounding the lake are now dominated by mountain hemlock, whitebark pine, and lodgepole pine. These plants not only depict the process of succession, but also of adaptation to a volcanic environment.
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  • Crater Lake U.S
    National Park Service Crater Lake U.S. Department of the Interior Refections Visitor Guide Summer/Fall 2017 Park News 2 ... Camping, Lodging, Food Visit the Sinnott Overlook 3 ... Ranger Programs f Water Restrictions in Effect Please help us conserve water during Plus 10 Other Ways to Enjoy Your Park 4 ... Hiking Trails your visit. The park’s ability to provide 5 ... Driving Map water is currently restricted as we The Sinnott Memorial Overlook ofers one of the ... In the News: Bull Trout transition from a surface water source fnest views of Crater Lake. You can peer down a 6 to a groundwater well. If you’re sheer drop of nearly 900 feet (274 meters) to the 7 ... Feature Article: Lake Level reading this before arriving, please shore! It also features the park’s best exhibits. A small stock up on water outside the park. 8 ... Climate Chart museum describes the lake’s geology, formation, and While you’re here, please take short exploration. (Of special interest is the original device showers, don’t run the tap, and reuse used by scientists to measure the lake’s depth in 1886.) towels and sheets if staying overnight Look Inside! in park lodging. Thanks for your help! Finding this special viewpoint can be a challenge. f Leave Your Drone at Home It’s hidden behind the Rim Visitor Center, perched on a promontory 50 feet (15 meters) below the rim. Operating remote-controlled aircraft Landscape architect Merel Sager, who oversaw in the park is prohibited. Please report Park Profle violators to the nearest employee.
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  • Day Hikes Crater Lake National Park the Following Is a Partial List of Day Hikes at Crater Lake National Park
    Day Hikes Crater Lake National Park The following is a partial list of day hikes at Crater Lake National Park. The list is organized according to estimated time length for completing the hike. Please note that the steep terrain of Crater Lake National Park means time, length and difficulty are not directly related. Times given are estimates of how long it will take to complete the trail and return to the trailhead. Trails listed as strenuous should be taken only by people in good physical condition. SHORT HIKES (15 to 45 minutes) MEDIUM HIKES (cont.) Sun Notch Viewpoint Annie Creek Canyon Time:20min. Time: 1 hour and 15 nun. Length: 0.25 mileoneway. Length: 1.7mileloop. Elevation: 7000 to 7115 ft. Elevation: 5800 to 6000 ft. Difficulty: moderate. Difficulty: moderate. Trailhead: 4 miles east ofParkHQ on East Rim Trailhead: AmpMtheafreatMazama Campground. Drive, marked by a sign. Features: Deep stream cut canyon, creek habitats, Features: Overlook of Crater Lakeand Phantom Ship, scattered wildflowers and occasional animals. wildflowers, dry meadow. Use caution near steep edges. Cleetwood Cove (lake shore trail) Godfrey Glen Time: 1 hour. Time:30min. Length: 1.1 miles, one way. Length: 1 mile. Elevation: 6850 to 6176 ft. Elevation: 6000to 6050ft. Difficulty: strenuous, 11% grade. Difficulty: easy. Trailhead: Parking area4.5 mi. east ofNorth Junction Trailhead: 2.4 miles south ofParkHQ. Features: Access to lake shore and boat landing. Features: Old growthforests and viewsof Annie Creek Canyon. LONGER HLKES (2 hours or more) Castle Crest Wildflower Garden Garfield Peak Time:30to45min. Time: 2 to 3 hours. Length: 0.4mfteloopfromRimDrive.
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  • Crater Lake National Park Oregon
    DEPARTMENT OF THE INTERIOR ALBERT B. FALL. SECRETARY NATIONAL PARK SERVICE STEPHEN T. MATHER, DIRECTOR RULES AND REGULATIONS CRATER LAKE NATIONAL PARK OREGON Photograph by Senic America Co. APPLEGATE PEAK FROM DUTTON CLIFF SEASON FROM JULY 1 TO SEPTEMBER 20 THE NATIONAL PARKS AT A GLANCE. [Number, 19; total area, 11,304 square miles.] National parks in , .. Area in order of creation Location. square Distinctive characteristics. miles. Hot Springs Middle Arkansas 1], 46 hot springs possessing curative properties— 1332 Many hotels and boarding houses—17 bath­ houses under public control. Yellowstone Northwestern Wye- 3,348 More geysers than in all rest of world together— 1872 ming. Boiling springs—Mud volcanoes—Petrified for­ ests—Grand Canyon of the Yellowstone, remark­ able for gorgeous coloring—Large lakes—Many large streams and waterfalls—Vast wilderness, reatest wild bird and animal preserve in world— fexceptional trout fishing. Sequoia Middle eastern Cali- 252 The Big Tree National Park—several hundred 1890 forma. sequoia trees over 10 feet in diameter, some 25 to 36 feet in diameter—Towering mountain ranges— Startling precipices—Mile long cave of delicate beauty. Yosemite Middle eastern Cali- 1,125 Valley of world-famed beauty—Lofty cliffs—Ro- 1890 fornia. man (ic vistas—Many waterfalls of extraordinary height—3 groves of big trees—High Sierra— Waterwheel falls—Good trout fishing. General Grant Middle eastern Cali- 4 Created to preserve the celebrated General Grant 1890 fornia. Tree, 35 feet in diameter—6 miles from Sequoia THE 1'IIANTOM SHIP. National Park. Mount Rainier ... West central Wash- 324 Largest accessible single peak glacier system—28 1899 ington.
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  • Crater Lake National Park
    CRATER LAKE National Pa^rR O T*~ E O O W UNITED STATES RAILROAD ADMINISTRATION N AT IONAU PARK SERIES Reflections stand out distinctly in water that gleams as though glazed by the sun Looking "Over the Top" Page two An Appreciation of (rater Lake National Park By WINSTON CHURCHILL, Author of "The Crisis," "Richard Carvel," "The Crossing," etc. Written Especially for the United States Railroad Administration i|T IS not so man) years ago that I left San Francisco with a case of rods, bound for Crater Lake in Oregon. What I had heard about the place had filled me with awe and expectation, tempered by a little skepticism. I was personally conducted by patriotic and hos­ pitable Oregonians who met me in sight of the fountains of Klamath, put me in a motor car and sped me northward through great forests and across wide prairies which once, not long since, had been an almost inaccessible wilderness. The immensity of the extinct volcano whither we were bound, that in prehistoric times had strewn the entire countryside with powdered stone, was hard to grasp. It was July. We climbed the wooded slopes to the snows, forged through the melting drifts to the very lip of the crater and suddenly looked down upon a scene celebrated in Indian myth, and unique in all America. Some thousand feet below us lay a bottomless crystal lake, six miles across dotted with black volcanic islands. My delight in the grandeur of this view, it must be confessed, was heightened by the knowledge that the lake was in­ habited by large rainbow trout which would rise to the fly.
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  • Analyses of Rocks and Minerals
    DEPARTMENT OF THE INTERIOR UNITED STATES GEOLOGICAL SURVEY GEORGE OTIS SMITH, DIRECTOR BULLETIN 419 ANALYSES OF ROCKS AND MINERALS FEOM THE LABORATORY OF THE UNITED STATES GEOLOGICAL SURVEY \ 1880 TO 1908 TABULATED BY F. W. CLARKE, CHIEF CHEMIST WASHINGTON GOVERNMENT PRINTING OFFICE 1910 CONTENTS. Page. Introduction.............................................................. 1 The average composition of rocks. ..'.....< .................................. 4 Analyses of igneous and crystalline rocks................................... 13 Maine. .................................................................... 13 1. Rocks from Aroostook County..... ^..................'........... 13 2. Miscellaneous rocks............................................. 14 New Hampshire....................................................... 15 Vermont............................................................... 15 1. Rocks of Mount Ascutney........................................ 15 2. Miscellaneous rocks.................:........................... 17 Massachusetts....:..............................................:..... .18 1. Magnesian rocks.............. ; .................................. 18 2. Amphibolite................................................... 19 3. Miscellaneous rocks............................................. 21 Connecticut............................................................ 24 New York............................................................. 26 1. Rocks of the Adirondack region................................... 26 2.
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  • Crater-Lake-Reflections-Summer-Fall
    National Park Service Crater Lake U.S. Department of the Interior Reflections Summer/Fall 2012 Visitor Guide 2 ... Camping, Lodging, Food Find the Phantom Ship 3 ... Ranger Programs Plus 10 Other Ways to Enjoy Your Park 4 ... Hiking Trails 5 ... Driving Map Of the two islands in Crater Lake, Wizard Island is ... Park News by far the more renowned (see photo, top of page 2). A 6 cinder cone that erupted out of the lake about 7,300 7 ... Park News years ago, it dominates our attention when we first 8 ... Climate Chart arrive at the rim. Hidden near the lake’s south shore, however, is an equally interesting rock that goes undetected by many park visitors. As its name suggests, Look Inside! the Phantom Ship is elusive. This isn’t because it travels around the lake—while resembling a sailboat, it’s firmly anchored to the underlying bedrock. It’s because, depending on your location, the angle of the sun, the Hike to a Hidden presence or absence of clouds, and whether or not the Park Profile lake is calm and mirrored, you may or may not be able Waterfall to see it. When you circle the lake on the Rim Drive, the Crater Lake National Park protects the island might seem to come and go like a “phantom.” deepest lake in the United States. Fed by A new hiking trail opened up last summer rain and snow (but no rivers or streams), at Crater Lake National Park. It’s called Despite its ghostly appearance, the Phantom Ship is solid lava, 400,000 years old—a resistant the lake is considered to be the cleanest the Plaikni Falls Trail, and it leads to a lush remnant of rock along a partially submerged ridge between two scalloped bays, as the view large body of water in the world.
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