What You Need to Know Before Climbing Mt. Hood Oregon's
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Protecting Freshwater Resources on Mount Hood National Forest Recommendations for Policy Changes
PROTECTING FRESHWATER RESOURCES ON MOUNT HOOD NATIONAL FOREST RECOMMENDATIONS FOR POLICY CHANGES Produced by PACIFIC RIVERS COUNCIL Protecting Freshwater Resources on Mount Hood National Forest Pacific Rivers Council January 2013 Fisherman on the Salmon River Acknowledgements This report was produced by John Persell, in partnership with Bark and made possible by funding from The Bullitt Foundation and The Wilburforce Foundation. Pacific Rivers Council thanks the following for providing relevant data and literature, reviewing drafts of this paper, offering important discussions of issues, and otherwise supporting this project. Alex P. Brown, Bark Dale A. McCullough, Ph.D. Susan Jane Brown Columbia River Inter-Tribal Fisheries Commission Western Environmental Law Center G. Wayne Minshall, Ph.D. Lori Ann Burd, J.D. Professor Emeritus, Idaho State University Dennis Chaney, Friends of Mount Hood Lisa Moscinski, Gifford Pinchot Task Force Matthew Clark Thatch Moyle Patrick Davis Jonathan J. Rhodes, Planeto Azul Hydrology Rock Creek District Improvement Company Amelia Schlusser Richard Fitzgerald Pacific Rivers Council 2011 Legal Intern Pacific Rivers Council 2012 Legal Intern Olivia Schmidt, Bark Chris A. Frissell, Ph.D. Mary Scurlock, J.D. Doug Heiken, Oregon Wild Kimberly Swan Courtney Johnson, Crag Law Center Clackamas River Water Providers Clair Klock Steve Whitney, The Bullitt Foundation Klock Farm, Corbett, Oregon Thomas Wolf, Oregon Council Trout Unlimited Bronwen Wright, J.D. Pacific Rivers Council 317 SW Alder Street, Suite 900 Portland, OR 97204 503.228.3555 | 503.228.3556 fax [email protected] pacificrivers.org Protecting Freshwater Resources on Mt. Hood National Forest: 2 Recommendations for Policy Change Table of Contents Executive Summary iii Part One: Introduction—An Urban Forest 1 Part Two: Watersheds of Mt. -
Ramona Falls Hike, Mount Hood Wilderness, Oregon, OR
www.outdoorproject.com MADE BY: Anzelina Coodey CONTRIBUTOR: Tyson Gillard LAST UPDATED: 08.10.16 © The Outdoor Project LLC NOTE: Content specified is from time of PDF creation. Please check website for up-to-date information or for changes. Maps are illustrative in nature and should be used for reference only. Ramona Falls Hike, Mount Hood Wilderness, Oregon, OR Adventure Description by Tyson Gillard | 06.12.12 The 120-foot Ramona Falls is tucked away on the western flanks of Mount Hood, and while the cascade is a remarkable destination by itself, the trail leading to the falls is equally delightful. You'll begin hiking along the open and sandy bed that flanks the Sandy River. The granular nature of the soil means that the river bed is home to a distinct blend of flora not typically found in the Mount Hood area, such as the many lodgepole pines, Oregon beaked moss, juniper haircap moss and broom moss. Once you've reached Ramona Falls, loop back on the trail’s northern section, where you'll gain a great appreciation for Ramona Creek. The trail follows the creek and adjacent cliffs downstream as it weaves through a forest of western hemlock, noble fir and western red cedar. If you are in the mood for something a little more challenging or you are looking for some good backpacking, continue on the Ramona Falls trail to Bald Mountain/McNeil Point, the scenic and secluded Yocum Ridge, or to the incredible wildflower haven of Paradise Park. Tyson Gillard | 06.12.12 Getting there (from Portland): From Portland, take I-84 E Take exit 16 for 238th Dr toward Wood Village Turn right onto NE 238th Dr Highlights Continue on NE 238th Dr, which turns into SE 242nd Dr/NE Hogan Dr DIFFICULTY: Moderate After roughly 3 miles turn left onto NE Burnside Rd/US-26 E TRAILHEAD ELEV.: 2,460 ft (750 m) After roughly 27 miles, just past Welches, turn left onto E NET ELEV. -
The Timberline Express Proposal
THE TIMBERLINE EXPRESS PROPOSAL United States Final Environmental Impact Statement Department of Agriculture Forest Service Summary of DEIS, Errata Sheet, Pacific Response to Comments Northwest Region November 2005 Mt. Hood National Forest View offrom Mt. Mt. Hood Snoqualmie from Trilium looking Lake. West at Alpental. The U.S. Department of Agriculture (USDA) prohibits discrimination in all its programs and activities on the basis of race, color, national origin, age, disability, and where applicable, sex, marital status, familial status, parental status, religion, sexual orientation, genetic information, political beliefs, reprisal, or because all or part of an individual’s income is derived from any public assistance program. (Not all prohibited bases apply to all programs.) Persons with disabilities who require alternative means for communication of 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 to USDA, Director, Office of Civil Rights, 1400 Independence Avenue, S.W., Washington D.C. 20250-9410, or call (800) 795-3271 (voice) or (202) 720-6382 (TDD). USDA is an equal opportunity provider and employer. ACRONYM LIST ACS Aquatic Conservation Strategy NMFS National Marine Fisheries Service ACSOs Aquatic Conservation Strategy Objectives NPDES National Pollutant Discharge Elimination System ADA Americans w/ Disabilities Act of 1990 NOAA National Oceanic and Atmospheric Administration ADT Average Daily Traffic -
Glisan, Rodney L. Collection
Glisan, Rodney L. Collection Object ID VM1993.001.003 Scope & Content Series 3: The Outing Committee of the Multnomah Athletic Club sponsored hiking and climbing trips for its members. Rodney Glisan participated as a leader on some of these events. As many as 30 people participated on these hikes. They usually travelled by train to the vicinity of the trailhead, and then took motor coaches or private cars for the remainder of the way. Of the four hikes that are recorded Mount Saint Helens was the first climb undertaken by the Club. On the Beacon Rock hike Lower Hardy Falls on the nearby Hamilton Mountain trail were rechristened Rodney Falls in honor of the "mountaineer" Rodney Glisan. Trips included Mount Saint Helens Climb, July 4 and 5, 1915; Table Mountain Hike, November 14, 1915; Mount Adams Climb, July 1, 1916; and Beacon Rock Hike, November 4, 1917. Date 1915; 1916; 1917 People Allen, Art Blakney, Clem E. English, Nelson Evans, Bill Glisan, Rodney L. Griffin, Margaret Grilley, A.M. Jones, Frank I. Jones, Tom Klepper, Milton Reed Lee, John A. McNeil, Fred Hutchison Newell, Ben W. Ormandy, Jim Sammons, Edward C. Smedley, Georgian E. Stadter, Fred W. Thatcher, Guy Treichel, Chester Wolbers, Harry L. Subjects Adams, Mount (Wash.) Bird Creek Meadows Castle Rock (Wash.) Climbs--Mazamas--Saint Helens, Mount Eyrie Hell Roaring Canyon Mount Saint Helens--Photographs Multnomah Amatuer Athletic Association Spirit Lake (Wash.) Table Mountain--Columbia River Gorge (Wash.) Trout Lake (Wash.) Creator Glisan, Rodney L. Container List 07 05 Mt. St. Helens Climb, July 4-5,1915 News clipping. -
Mt. Hood National Scenic Byway Interpretive Plan and Design Guidelines USDA Mt
Mt. Hood National Scenic Byway Interpretive Plan and Design Guidelines USDA Mt. Hood United States National Scenic Byway Department of Agriculture Interpretive Plan Forest Service & Design Guidelines Region 6 Mt. Hood National Forest April 2009 1 OCTOBER 2008 Draft Mt. Hood National Scenic Byway Interpretive Plan & Design Guidelines Prepared by: • U.S. Forest Service, Rocky Mountain Region Center for Design and Interpretation • Shapins Belt Collins (Planning, Civil Engineering, and Landscape Architecture) Prepared For: Mt. Hood National Scenic Byway Committee The U.S. Department of Agriculture (USDA) prohibits discrimination in all its programs and activities on the basis of race, color, national origin, age, disability, and where applicable, sex, marital status, familial status, parental status, religion, sexual orientation, genetic information, political beliefs, reprisal, or because all or part of an individual’s income is derived from any public assistance program. (Not all prohibited bases apply to all programs.) Persons with disabilities who require alternative means for communication of 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 to USDA, Director, Office of Civil Rights, 1400 Independence Avenue, S.W., Washington, DC 20250-9410, or call (800) 795-3272 (voice) or (202) 720-6382 (TDD). USDA is an equal opportunity provider and employer. 2 Mt. Hood National Scenic Byway Interpretive Plan & Design Guidelines -
Post-Glacial Lahars of the Sandy River Basin, Mount Hood, Oregon
Kenneth A. Cameron and Patrick Pringle, USGSCascades Volcano Observatory VancouverWashinoton 98661 Post-GlacialLahars of the SandyRiver Basin, MountHood, Oregon Abstract Vithin the last I0,000 years,three significant lahar'producingperiods have occurr€dar Mount Hood, Oregon.The Timberline eruptire period occurred belween 1400and 1800years BP. It wasby far the nosr voluminousof lhe three periods,producing enoughclastic debris to bury the glacialtopography ofthe southwestface of the mountain beneatha snootb debris fan. Snaller debris fans were forned in the upper reachesof the Sandy and Salmon Rivers. Timberline-agelahars trareled the length of the Zigzag and SandyRivers, a disrancein ercesso{90 krn. Thesejahars and associatedfluvial depositshelped forrn flat-floored valleys near the confluenceof these rivers and cr€ated a deha at the mouth of the Sandy at the Colunbia River. The flons probably atlained depthsofg to 12 m above modern river level for nost of their passage.Pyroclastic flows of this age traveled at least 13 km frorn the rent a.€a at Crat€r Rock along the Zigzag or Litle Zigzag Rirers. Between400 and 600 yearsBP, ihe Zigzag erupriveperiod produceddeposirs along the middle reachesof the Zigzag River and the upper Sandy River. Bouldert labars and flurial depositscreated a terrace B to I0 n above present river lerel along the Zigzag and veneereda Timberlin€-aget€rrace on the Sandy River. The Old Maid eruptive period occured b€tw€€n lB0 and 2?0 years BP. A single lahar flowed down the Sandy River at least as {ar as Brightwood,30 }n from Crarer Rock. Sand d€posilsthat may b€ related to this erent are found down to the nouth of the SandyRiver. -
Downstream Effects of Glaciers on Stream Water Quality, Mt. Hood, Oregon and Mt
Downstream Effects of Glaciers on Stream Water Quality, Mt. Hood, Oregon and Mt. Rainier, Washington JANICE A. DOUGALL, DR. ANDREW G. FOUNTAIN Department of Geography, PortlaPortlandnd State University,University, Portland, OrOregon,egon, 97207 ………… Introduction Methods Electrical Conductivity Previous studies have shown that basins with partial glacier cover have less summer discharge variability Field data Measure temperature, turbidity, electrical conductivity, and collect suspended sediment, and Electrical conductivity (specific conductance) is low in both glacial and non-glacial headwaters, and than non glacial basins due to increased melt during otherwise warm, dry periods ( e.g. Fountain and ion samples during late-summer on cloud-free days. increases with distance, but varies by stream. The lowest measures of specific conductance were found Walder 1998). Other studies addressed glacier effects on water quality in the proglacial plain (e.g. • Data loggers recorded temperature every 15 minutes over a period of days. among glacial streams. Runoff from the two smallest glaciers studied, Palmer and White rivers, had the Gurnell 1982, Uehlinger et al. 2003). However, few studies consider distant downstream effects of • Teams of 3 or 4 people measured conductivity and turbidity and sampled for suspended sediments lowest conductivities observed (<10μS cm-1). Runoff from larger glaciers, Emmons and Eliot, had glaciers on water quality. Glacial meltwater is characterized by low temperatures, low concentrations of hourly for between 6 and 24 hours specific conductance values >20μS cm-1 close to the glaciers. soluble ions, high suspended sediment concentrations, and high turbidity (Milner and Petts 1994).These • Samples were collected along streams in a Lagrangian fashion and included suspended sediment and qualities differ significantly between glacial and non-glacial streams. -
31 FRI 12.8. After Having Breakfast at a Lovely Spot, We Drove Back Onto
FRI 12.8. After having breakfast at a lovely spot, we drove back onto the highway. A bit of info for us the students of English: In North American and Australian English, major roads such as controlled-access highways or arterial roads are often state highways (Canada: provincial highways). Other roads may be designated "county highways" in the US and Ontario. These classifications refer to the level of government (state, provincial, county) that maintains the roadway. In British English, "highway" is primarily a legal term. Everyday use normally implies roads, while the legal use covers any route or path with a public right of access, including footpaths etc. The term has led to several related derived terms, including highway system, highway code, highway patrol and highwayman. The first photo was taken on the way to our third volcano in Cascade Range - Mt. Hood Mount Hood (3429m) is the tallest point in the U.S. state of Oregon. We can see its reflection in Mirror Lake. The Multnomah tribe name for Mount Hood was Wy'east. 31 Mt. Hood, once again, as seen from Timothy Lake The peak is home to 12 named glaciers and snowfields. It is the highest point in Oregon and the fourth highest in the Cascade Range. Mount Hood is considered the Oregon volcano most likely to erupt, though based on its history, an explosive eruption is unlikely. Still, the odds of an eruption in the next 30 years are estimated at between 3 and 7 percent, so the U.S. Geological Survey (USGS) characterizes it as "potentially active", but the mountain is informally considered dormant. -
Mount Hood by Jon Bell Mount Hood Is a Stratovolcano in Northwest Oregon Located About Fifty Miles East of Portland and Thirty-Five Miles South of the Columbia River
Mount Hood By Jon Bell Mount Hood is a stratovolcano in northwest Oregon located about fifty miles east of Portland and thirty-five miles south of the Columbia River. At 11,244 feet, it is the highest point in Oregon and the fourth highest peak in the Cascade Range. Mount Hood has played a central role in the geology, history, natural environment, and culture that have helped shape northwest Oregon and the entire Pacific Northwest. Eruptions and Glaciers Composed primarily of andesite and dacite, Mount Hood began to form during volcanic eruptions between 500,000 and 700,000 years ago. Over the ensuing millennia, further eruptions continued to shape and give rise to the mountain. At its highest, Mount Hood topped 12,000 feet, with ice and erosion reducing the peak to its current height. Notable natural features include Cooper Spur, Illumination Rock, Barrett Spur, Mississippi Head, McNeil Point, Yocum Ridge, and Cathedral Ridge. Eruptions on Mount Hood have been characterized less by powerful explosions than by the gradual building and collapse of lava domes, pyroclastic flows, and volcanic mudflows known as lahars. In the past 2,000 years, Mount Hood has experienced three eruptive periods: the Timberline period, just over 1,500 years ago; the Zigzag period, about 600 years ago; and the Old Maid period, between the 1760s and the early 1800s. The most recent major eruption, estimated to have occurred in the 1780s, sent a massive lahar down the Sandy River and left behind Crater Rock, a 550-foot-high lava dome on the mountain’s south side. -
Mount Hood and Timberline Lodge
MAG/NÂ STARTING your &Cent at the 3426 metre Mount Hoodsummit. Due For skiers, snow- nearly 2000 metres. The sky is to the low wind and high visibiiiiy, the deep blue, three metres of snow is Magic Mile Chair is operating today, and we grstefulty ride it to over 2100 metres, boarders, climbers, firm underneath ten centimetres of saving hour of fell night, about an ciimfnng effort. fresh powder that in the As vse /cave the shelter of t& few hikers, and even and the shining peak the Natrue remaining trees, a lidt breeze picks up. AmericansI called Wy 'Eastseems nearly close enough to touch; yet it will take sail boarders, the several hours mere4 to crest its shoulder. majestic hunt The early morning light casts a pink glow, - raising distinctive shadows near each ridge and valley, all clearly visible here peted by a wonderfu? spectacle, as most above the timberfifte, where only a fm of the Oregon Cascades spread out before twisted, flagged sub-alpine fir dare to But we North Oregon, is a exist. A gray jay swoops nearby, perhaps us in early morning relief. are hoping it wiij be sharing our breakfast headed up, andthe view will inerease soon. We stick climbing skins onto our with each stn'de. Now the real work true year-round telemark skis, rub on some leueZ 21 sun- begins.. block, and prepare to head off for destination Illumination Saddle, a high pass betsseen Huffiag and puffing, we trudge up the the 2909 metre I//umination Rock and last 700 metres toward the saddle, Outdoor* (lhstmld June /July 19'" skimming the edgy of Palmer Glacier, A skier walks dwsn off the mountain (left) home of the only a//-summerlift-serviced having made the climb (using sktas) in the skiing in the United States, The Palmer early morning. -
The Stratigraphy, Depositional Processes, and Environment of the Late Pleistocene Polallie-Period Deposits at Mount Hood Volcano, Oregon, USA
Geomorphology 70 (2005) 12–32 www.elsevier.com/locate/geomorph The stratigraphy, depositional processes, and environment of the late Pleistocene Polallie-period deposits at Mount Hood Volcano, Oregon, USA Jean-Claude ThouretT Laboratoire Magmas et Volcans UMR 6524 CNRS, Universite´ Blaise Pascal, OPGC, France IRD 5 rue Kessler, 63038 Clermont-Ferrand cedex, France Received 9 March 2004; received in revised form 23 March 2005; accepted 25 March 2005 Available online 23 May 2005 Abstract The Polallie eruptive period of Mt. Hood, Oregon, is the last major episode of eruption and dome growth, before the late Holocene activity which was centered at Crater Rock. A volume of 4–8 km3 of Polallie deposits forms an apron of ca. 60 km2 on the east, northeast and southeast flanks. The Polallie deposits can be divided, stratigraphically, into four groups: Group I rockslide avalanche and pyroclastic-flow deposits; Group II debris-flow and pyroclastic-flow deposits that suggest some explosive activity and remobilization of pyroclastic debris in a glacial environment; Group III block-and-ash flow deposits that attest to summit dome growth; Group IV alternating debris-flow deposits, glacial sediments, and reworked pyroclastic-flow deposits that indicate a decrease in dome activity and an increase in erosion and transport. Group III clearly indicates frequent episodes of dome growth and collapse, whereas Groups II and IV imply increasing erosion and, conversely, decreasing volcanic activity. The Polallie period occurred in the late Pleistocene during and just after the last Alpine glaciation, which is named Evans Creek in the Cascade Range. According to four K–Ar age dates on lava flows interbedded with Polallie deposits and to published minimum 14C ages on tephra and soils overlying these deposits, the Polallie period had lasted 15,000–22,000 years between 28–34 ka and 12–13 ka. -
DECISION NOTICE and FINDING of NO SIGNIFICANT IMPACT USDA
TIMBERLINE SKI AREA MOUNTAIN BIKE TRAILS AND SKILLS PARK DECISION NOTICE and FINDING OF NO SIGNIFICANT IMPACT USDA FOREST SERVICE MT. HOOD NATIONAL FOREST ZIGZAG RANGER DISTRICT CLACKAMAS COUNTY, OREGON T3S, R9E, Sections 7, 12, & 13, Willamette Meridian The Mt. Hood National Forest has completed the Environmental Assessment (EA) for the Timberline Ski Area Mountain Bike Trails and Skills Park project in compliance with the National Environmental Policy Act (NEPA) and other relevant Federal and State laws and regulations. BACKGROUND RLK & Company (RLK), the operators of the Timberline Lodge and Ski Area Complex, submitted a proposal for a lift-assisted downhill mountain biking trail system and skills park to the Forest Service in 2010. Lift-assisted mountain biking involves riders using a modified chairlift to bring themselves and their mountain bikes to the top of a mountain bike trail system. Rather than using ski runs as trails, downhill, lift-assisted mountain biking uses trails between 16 and 66 inches in width to descend from the top of the ski lift to the bottom, using turns and following natural contours as they cross though ski runs and the areas between them at a much less steep grade than the ski runs themselves. Grade-reversals, dips, and other techniques are used to control speed, keep riders on the trail, and maintain the trails and the natural resources they pass through. RLK’s goal was to develop a managed, high-quality mountain bike park that would appeal to families and feature predominantly beginner and intermediate level trails, as well as for learning biking skills and riding etiquette.