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2019 Oregon Administrative Rules Compilation
2019 OREGON ADMINISTRATIVE RULES COMPILATION CHAPTER 736 Parks and Recreation Department Published By DENNIS RICHARDSON Secretary of State Copyright 2019 Office of the Secretary of State Rules effective as of January 01, 2019 DIVISION 1 PROCEDURAL RULES 736-001-0000 Notice of Proposed Rules 736-001-0005 Model Rules of Procedure 736-001-0030 Fees for Public Records DIVISION 2 ADMINISTRATIVE ACTIVITIES 736-002-0010 State Park Cooperating Associations 736-002-0015 Working with Donor Organizations 736-002-0020 Criminal Records Checks 736-002-0030 Definitions 736-002-0038 Designated Positions: Authorized Designee and Contact Person 736-002-0042 Criminal Records Check Process 736-002-0050 Preliminary Fitness Determination. 736-002-0052 Hiring or Appointing on a Preliminary Basis 736-002-0058 Final Fitness Determination 736-002-0070 Crimes Considered 736-002-0102 Appealing a Fitness Determination 736-002-0150 Recordkeeping, Confidentiality, and Retention 736-002-0160 Fees DIVISION 3 WILLAMETTE RIVER GREENWAY PLAN 736-003-0005 Willamette River Greenway Plan DIVISION 4 DISTRIBUTION OF ALL-TERRAIN VEHICLE FUNDSTO PUBLIC AND PRIVATELY OWNED LANDMANAGERS, ATV CLUBS AND ORGANIZATIONS 736-004-0005 Purpose of Rule 736-004-0010 Statutory Authority 736-004-0015 Definitions 736-004-0020 ATV Grant Program: Apportionment of Monies 736-004-0025 Grant Application Eligibility and Requirements 736-004-0030 Project Administration 736-004-0035 Establishment of the ATV Advisory Committee 736-004-0045 ATV Operating Permit Agent Application and Privileges 736-004-0060 -
Uplift, Rupture, and Rollback of the Farallon Slab Reflected in Volcanic
PUBLICATIONS Journal of Geophysical Research: Solid Earth RESEARCH ARTICLE Uplift, rupture, and rollback of the Farallon slab reflected 10.1002/2017JB014517 in volcanic perturbations along the Yellowstone Key Points: adakite hot spot track • Volcanic perturbations in the Cascadia back-arc region are derived from uplift Victor E. Camp1 , Martin E. Ross2, Robert A. Duncan3, and David L. Kimbrough1 and dismemberment of the Farallon slab from ~30 to 20 Ma 1Department of Geological Sciences, San Diego State University, San Diego, California, USA, 2Department of Earth and • Slab uplift and concurrent melting 3 above the Yellowstone plume Environmental Sciences, Northeastern University, Boston, Massachusetts, USA, College of Earth, Ocean, and Atmospheric promoted high-K calc-alkaline Sciences, Oregon State University, Corvallis, Oregon, USA volcanism and adakite generation • Creation of a seismic hole beneath eastern Oregon resulted from thermal Abstract Field, geochemical, and geochronological data show that the southern segment of the ancestral erosion and slab rupture, followed by Cascades arc advanced into the Oregon back-arc region from 30 to 20 Ma. We attribute this event to thermal a period of slab rollback uplift of the Farallon slab by the Yellowstone mantle plume, with heat diffusion, decompression, and the release of volatiles promoting high-K calc-alkaline volcanism throughout the back-arc region. The greatest Supporting Information: • Supporting Information S1 degree of heating is expressed at the surface by a broad ENE-trending zone of adakites and related rocks • Data Set S1 generated by melting of oceanic crust from the Farallon slab. A hiatus in eruptive activity began at ca. • Data Set S2 22–20 Ma but ended abruptly at 16.7 Ma with renewed volcanism from slab rupture occurring in two separate • Data Set S3 regions. -
Oregon Historic Trails Report Book (1998)
i ,' o () (\ ô OnBcox HrsroRrc Tnans Rpponr ô o o o. o o o o (--) -,J arJ-- ö o {" , ã. |¡ t I o t o I I r- L L L L L (- Presented by the Oregon Trails Coordinating Council L , May,I998 U (- Compiled by Karen Bassett, Jim Renner, and Joyce White. Copyright @ 1998 Oregon Trails Coordinating Council Salem, Oregon All rights reserved. No part of this document may be reproduced or transmitted in any form or by any means, electronic or mechanical, including photocopying, recording, or any information storage or retrieval system, without permission in writing from the publisher. Printed in the United States of America. Oregon Historic Trails Report Table of Contents Executive summary 1 Project history 3 Introduction to Oregon's Historic Trails 7 Oregon's National Historic Trails 11 Lewis and Clark National Historic Trail I3 Oregon National Historic Trail. 27 Applegate National Historic Trail .41 Nez Perce National Historic Trail .63 Oregon's Historic Trails 75 Klamath Trail, 19th Century 17 Jedediah Smith Route, 1828 81 Nathaniel Wyeth Route, t83211834 99 Benjamin Bonneville Route, 1 833/1 834 .. 115 Ewing Young Route, 1834/1837 .. t29 V/hitman Mission Route, 184l-1847 . .. t4t Upper Columbia River Route, 1841-1851 .. 167 John Fremont Route, 1843 .. 183 Meek Cutoff, 1845 .. 199 Cutoff to the Barlow Road, 1848-1884 217 Free Emigrant Road, 1853 225 Santiam Wagon Road, 1865-1939 233 General recommendations . 241 Product development guidelines 243 Acknowledgements 241 Lewis & Clark OREGON National Historic Trail, 1804-1806 I I t . .....¡.. ,r la RivaÌ ï L (t ¡ ...--."f Pðiräldton r,i " 'f Route description I (_-- tt |". -
Washington Division of Geology and Earth Resources Open File Report
RECONNAISSANCE SURFICIAL GEOLOGIC MAPPING OF THE LATE CENOZOIC SEDIMENTS OF THE COLUMBIA BASIN, WASHINGTON by James G. Rigby and Kurt Othberg with contributions from Newell Campbell Larry Hanson Eugene Kiver Dale Stradling Gary Webster Open File Report 79-3 September 1979 State of Washington Department of Natural Resources Division of Geology and Earth Resources Olympia, Washington CONTENTS Introduction Objectives Study Area Regional Setting 1 Mapping Procedure 4 Sample Collection 8 Description of Map Units 8 Pre-Miocene Rocks 8 Columbia River Basalt, Yakima Basalt Subgroup 9 Ellensburg Formation 9 Gravels of the Ancestral Columbia River 13 Ringold Formation 15 Thorp Gravel 17 Gravel of Terrace Remnants 19 Tieton Andesite 23 Palouse Formation and Other Loess Deposits 23 Glacial Deposits 25 Catastrophic Flood Deposits 28 Background and previous work 30 Description and interpretation of flood deposits 35 Distinctive geomorphic features 38 Terraces and other features of undetermined origin 40 Post-Pleistocene Deposits 43 Landslide Deposits 44 Alluvium 45 Alluvial Fan Deposits 45 Older Alluvial Fan Deposits 45 Colluvium 46 Sand Dunes 46 Mirna Mounds and Other Periglacial(?) Patterned Ground 47 Structural Geology 48 Southwest Quadrant 48 Toppenish Ridge 49 Ah tanum Ridge 52 Horse Heaven Hills 52 East Selah Fault 53 Northern Saddle Mountains and Smyrna Bench 54 Selah Butte Area 57 Miscellaneous Areas 58 Northwest Quadrant 58 Kittitas Valley 58 Beebe Terrace Disturbance 59 Winesap Lineament 60 Northeast Quadrant 60 Southeast Quadrant 61 Recommendations 62 Stratigraphy 62 Structure 63 Summary 64 References Cited 66 Appendix A - Tephrochronology and identification of collected datable materials 82 Appendix B - Description of field mapping units 88 Northeast Quadrant 89 Northwest Quadrant 90 Southwest Quadrant 91 Southeast Quadrant 92 ii ILLUSTRATIONS Figure 1. -
Timing of In-Water Work to Protect Fish and Wildlife Resources
OREGON GUIDELINES FOR TIMING OF IN-WATER WORK TO PROTECT FISH AND WILDLIFE RESOURCES June, 2008 Purpose of Guidelines - The Oregon Department of Fish and Wildlife, (ODFW), “The guidelines are to assist under its authority to manage Oregon’s fish and wildlife resources has updated the following guidelines for timing of in-water work. The guidelines are to assist the the public in minimizing public in minimizing potential impacts to important fish, wildlife and habitat potential impacts...”. resources. Developing the Guidelines - The guidelines are based on ODFW district fish “The guidelines are based biologists’ recommendations. Primary considerations were given to important fish species including anadromous and other game fish and threatened, endangered, or on ODFW district fish sensitive species (coded list of species included in the guidelines). Time periods were biologists’ established to avoid the vulnerable life stages of these fish including migration, recommendations”. spawning and rearing. The preferred work period applies to the listed streams, unlisted upstream tributaries, and associated reservoirs and lakes. Using the Guidelines - These guidelines provide the public a way of planning in-water “These guidelines provide work during periods of time that would have the least impact on important fish, wildlife, and habitat resources. ODFW will use the guidelines as a basis for the public a way of planning commenting on planning and regulatory processes. There are some circumstances where in-water work during it may be appropriate to perform in-water work outside of the preferred work period periods of time that would indicated in the guidelines. ODFW, on a project by project basis, may consider variations in climate, location, and category of work that would allow more specific have the least impact on in-water work timing recommendations. -
On Foot Scampering Over Tree Roots
5. Netarts/Happy Camp Beaches Safety & Etiquette Netarts has two good beach access points, 7-9 Cape Lookout • Pack it in, pack it out. Cape to Cape with restrooms at both. Just north of the These hikes are longer and more • Keep dogs on leash. village of Netarts, take Happy Camp Road ! strenuous than the other hikes in this • Watch children closely. west down the hill. At the end of the road you guide. Be prepared for muddy sections and • Do not climb cliffs or walk out will find a gravel parking lot near the mouth on Foot scampering over tree roots. Wear good onto rock faces. of Netarts Bay. From the parking lot, you can shoes, carry water, and plan for unpredictable Netarts Area Trails and Beach Walks • Be prepared for sudden walk to the south along the bay or to the changes in weather. Cape Lookout can be weather changes. from Cape Meares to Cape Lookout north with great views of Three Arch Rocks. very windy or become shrouded in fog quickly. This area has strong tidal currents and is • Watch for sneaker waves. unsafe for swimming. Jim Young In Netarts, turn west off the main highway 7. North Trail at Netarts Bay Drive. You will immediately Jim Young see Netarts Bay and the County Boat Ramp North Trail crosses the cape and follows the parking lot. From the lot, walk west about coastline north 2.3 miles (4.6 miles round-trip) 100 yards to the bay beach. A day-use through the shaded forest and down to the parking fee is required. -
O R E G O N North Pacific Ocean
412 ¢ U.S. Coast Pilot 7, Chapter 9 31 MAY 2020 Chart Coverage in Coast Pilot 7—Chapter 9 124° 123° NOAA’s Online Interactive Chart Catalog has complete chart coverage 18520 C O L http://www.charts.noaa.gov/InteractiveCatalog/nrnc.shtml U M B I A 126° 125° 18521 R Astoria I V E R 46° Seaside Tillamook Head NEHALEM RIVER 18556 Vancouver 18558 TILLAMOOK BAY Portland Cape Lookout Cascade Head 45° SILETZ RIVER YAQUINA RIVER ALSEA RIVER 18581 18561 NORTH PA CIFIC OCEAN OREGON Heceta Head 44° 18583 SIUSLAW RIVER 18584 UMPQUA RIVER 18587 Coos Bay Cape Arago 18588 COQUILLE RIVER 43° 18589 Cape Blanco 18600 18580 Port Orford ROUGE RIVER 18601 CHETCO RIVER 42° 18602 CALIFORNIA 31 MAY 2020 U.S. Coast Pilot 7, Chapter 9 ¢ 413 Chetco River to Columbia River, Oregon (1) This chapter describes 200 miles of the Oregon coast rare clear skies; it is more likely in early winter. Winter from the mouth of the Chetco River to the mouth of the and spring winds are moderately strong, particularly south Columbia River. Also described are the Chetco and Rogue of Newport. From North Bend southward, winds reach 17 Rivers, Port Orford, Coquille River, Coos Bay, Umpqua knots or more about 5 to 15 percent of the time and 28 and Siuslaw Rivers, Yaquina Bay and River, Nehalem knots or more about 1 to 3 percent of the time. Extreme River and Tillamook Bay. The cities of Coos Bay and wind speeds usually occur in either winter or early spring North Bend on Coos Bay and Newport on Yaquina Bay and have climbed to around 50 knots. -
3.2 Flood Level of Risk* to Flooding Is a Common Occurrence in Northwest Oregon
PUBLIC COMMENT DRAFT 11/07/2016 3.2 Flood Level of Risk* to Flooding is a common occurrence in Northwest Oregon. All Flood Hazards jurisdictions in the Planning Area have rivers with high flood risk called Special Flood Hazard Areas (SFHA), except Wood High Village. Portions of the unincorporated area are particularly exposed to high flood risk from riverine flooding. •Unicorporated Multnomah County Developed areas in Gresham and Troutdale have moderate levels of risk to riverine flooding. Preliminary Flood Insurance Moderate Rate Maps (FIRMs) for the Sandy River developed by the Federal Emergency Management Agency (FEMA) in 2016 •Gresham •Troutdale show significant additional risk to residents in Troutdale. Channel migration along the Sandy River poses risk to Low-Moderate hundreds of homes in Troutdale and unincorporated areas. •Fairview Some undeveloped areas of unincorporated Multnomah •Wood Village County are subject to urban flooding, but the impacts are low. Developed areas in the cities have a more moderate risk to Low urban flooding. •None Levee systems protect low-lying areas along the Columbia River, including thousands of residents and billions of dollars *Level of risk is based on the local OEM in assessed property. Though the probability of levee failure is Hazard Analysis scores determined by low, the impacts would be high for the Planning Area. each jurisdiction in the Planning Area. See Appendix C for more information Dam failure, though rare, can causing flooding in downstream on the methodology and scoring. communities in the Planning Area. Depending on the size of the dam, flooding can be localized or extreme and far-reaching. -
Mineral Resources of the Abert Rim Wilderness Study Area, Lake County, Oregon
Mineral Resources of the Abert Rim Wilderness Study Area, Lake County, Oregon U.S. GEOLOGICAL SURVEY BULLETIN 1738-C AVAILABILITY OF BOOKS AND MAPS OF THE U.S. GEOLOGICAL SURVEY Instructions on ordering publications of the U.S. Geological Survey, along with prices of the last offerings, are given in the cur rent-year issues of the monthly catalog "New Publications of the U.S. Geological Survey." Prices of available U.S. Geological Sur vey publications released prior to the current year are listed in the most recent annual "Price and Availability List" Publications that are listed in various U.S. Geological Survey catalogs (see back inside cover) but not listed in the most recent annual "Price and Availability List" are no longer available. Prices of reports released to the open files are given in the listing "U.S. Geological Survey Open-File Reports," updated month ly, which is for sale in microfiche from the U.S. Geological Survey, Books and Open-File Reports Section, Federal Center, Box 25425, Denver, CO 80225. Reports released through the NTIS may be obtained by writing to the National Technical Information Service, U.S. Department of Commerce, Springfield, VA 22161; please include NTIS report number with inquiry. Order U.S. Geological Survey publications by mail or over the counter from the offices given below. BY MAIL OVER THE COUNTER Books Books Professional Papers, Bulletins, Water-Supply Papers, Techniques of Water-Resources Investigations, Circulars, publications of general in Books of the U.S. Geological Survey are available over the terest (such as leaflets, pamphlets, booklets), single copies of Earthquakes counter at the following Geological Survey Public Inquiries Offices, all & Volcanoes, Preliminary Determination of Epicenters, and some mis of which are authorized agents of the Superintendent of Documents: cellaneous reports, including some of the foregoing series that have gone out of print at the Superintendent of Documents, are obtainable by mail from WASHINGTON, D.C.-Main Interior Bldg. -
English Information
National Park Service U.S. Department of the Interior Capitol Reef National Park … the light seems to flow or shine out of the rock rather than to be reflected English from it. – Clarence Dutton, geologist and early explorer of Capitol Reef, 1880s A Wrinkle in the Earth A vibrant palette of color spills across the landscape before bridges, and twisting canyons. Over millions of years geologic forces you. The hues are constantly changing, altered by the play shaped, lifted, and folded the earth, creating this rugged, remote area of light against the towering cliffs, massive domes, arches, known as the Waterpocket Fold. Panorama Point at Sunset Erosion creates waterpockets and potholes that collect The Castle is made of fractured Wingate Sandstone perched upon grey Chinle and red Moenkopi Formations. rainwater and snowmelt, enhancing a rich ecosystem. From the east, the Waterpocket Fold appears as a formidable barrier Capitol Dome reminded early travelers of the US Capitol to travel, much like a barrier reef in an ocean. building and later inspired the name of the park. Creating the Waterpocket Fold Capitol Reef’s defining geologic feature is a wrinkle in Uplift: Between 50 and 70 million years ago, an ancient fault was Earth’s crust, extending nearly 100 miles from Thousand reactivated during a time of tectonic activity, lifting the layers to the Lake Mountain to Lake Powell. It was created over time by west of the fault over 7,000 feet higher than those to the east. Rather three gradual, yet powerful processes—deposition, uplift, than cracking, the rock layers folded over the fault line. -
New to Newport Guide
New to Newport Guide Welcome! We’re happy to have you join the Hatfield student community! To help you settle in and answer some burning questions, we’ve prepared a brief explainer on the slightly-quirky town of Newport and the people that live here. By HSO grad students Updated 9/2020 Yaquina Head Lighthouse (Image courtesy of Hillary Thalmann) Table of Contents Getting Settled In at HMSC ................................................................................................................... 3 Grad School in the time of COVID-19 ................................................................................................. 6 Hatfield Student Organization ........................................................................................................... 6 Guin Library Resources ......................................................................................................................... 7 Racial Justice Resources at HMSC ...................................................................................................... 9 HMSC Green Team, Recycling, and Fresh Food Options ............................................................ 10 Commuting from Newport ................................................................................................................. 13 Housing .................................................................................................................................................... 14 Healthcare on the Coast ..................................................................................................................... -
Josephine County, Oregon, Historical Society Document Oregonłs
Finding fossils in Oregon is not so much a question of Places to see fossils: where to look for them as where not to look. Fossils are rare John Day Fossil Beds National Monument in the High Lava Plains and High Cascades, but even there, , _ Contains a 40-million year record of plant and animal life . ·� � .11�'!]�:-.: some of the lakes are famous for their fossils. Many of the ill the John Day Basill ill central Oregon near the towns of .• .� . ' · sedimentary rocks in eastern Oregon contain fossil leaves or · ,,����<:l. · . ' · •· Dayville' Fossil, and Mitchell. The Cant Ranch Visitor ; ' " ' ' j ' .- � bones. Leaffossils are especially abundant in the - Center at Sheep Rock on Highway 19 includes museum : ,· .,, 1 • , .. rocks at the far side of the athletic · exhibits of fossils. Open every day 8:30-5. For general l· · . ., ;: . · : field at Wheeler High School ,...,..;� information, contact John Day Fossil Beds National . -- - ' '· in the town of Fossil. Monument, 420 West Main St., John Day, OR 97845, ' l-, Although it is rare to phone (503) 575-0721. find a complete Oregon Museum of Science and Industry animal fossil, a 1945 SE Water Ave., Portland, OR 97214. Open Thurs. & search of river Fri. 9:30-9; Sat. through Wed. 9:30-7(sumrner hours); beds may turn . l 9:30-5(rest of year), phone (503) 797-4000 up c h1ps or Condon Museum, University of Oregon even teeth. In Pacific Hall, Eugene, OR 97403. Open only by western appointment, phone (503) 346-4577. Oregon, the ' . ; Douglas County Museum of History and sedimentary ' r Natural History rocks that are 1 primarily off1-5 at exit 123 at Roseburg (PO Box 1550, Roseburg, marine in OR 97470).