Drainage Basin Morphology in the Central Coast Range of Oregon
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In Partial Fulfillment Of
WATER UTILI AT'ION AND DEVELOPMENT IN THE 11ILLAMETTE RIVER BASIN by CAST" IR OLISZE "SKI A THESIS submitted to OREGON STATE COLLEGE in partialfulfillment of the requirements for the degree of MASTER OF SCIENCE June 1954 School Graduate Committee Data thesis is presented_____________ Typed by Kate D. Humeston TABLE OF CONTENTS CHAPTER PAGE I. INTRODUCTION Statement and History of the Problem........ 1 Historical Data............................. 3 Procedure Used to Explore the Data.......... 4 Organization of the Data.................... 8 II. THE WILLAMETTE RIVER WATERSHED Orientation................................. 10 Orography................................... 10 Geology................................. 11 Soil Types................................. 19 Climate ..................................... 20 Precipitation..*.,,,,,,,................... 21 Storms............'......................... 26 Physical Characteristics of the River....... 31 Physical Characteristics of the Major Tributaries............................ 32 Surface Water Supply ........................ 33 Run-off Characteristics..................... 38 Discharge Records........ 38 Ground Water Supply......................... 39 CHAPTER PAGE III. ANALYSIS OF POTENTIAL UTILIZATION AND DEVELOPMENT.. .... .................... 44 Flood Characteristics ........................ 44 Flood History......... ....................... 45 Provisional Standard Project: Flood......... 45 Flood Plain......... ........................ 47 Flood Control................................ 48 Drainage............ -
Bioenergy Harvest, Climate Change, and Forest Carbon in the Oregon Coast Range
Portland State University PDXScholar Environmental Science and Management Faculty Publications and Presentations Environmental Science and Management 3-2016 Bioenergy Harvest, Climate Change, and Forest Carbon in the Oregon Coast Range Megan K. Creutzburg Portland State University, [email protected] Robert M. Scheller Portland State University, [email protected] Melissa S. Lucash Portland State University, [email protected] Louisa B. Evers Bureau of Land Management Stephen D. LeDuc United States Environmental Protection Agency See next page for additional authors Follow this and additional works at: https://pdxscholar.library.pdx.edu/esm_fac Part of the Forest Biology Commons Let us know how access to this document benefits ou.y Citation Details Creutzburg, M. K., Scheller, R. M., Lucash, M. S., Evers, L. B., LeDuc, S. D., & Johnson, M. G. (2015). Bioenergy harvest, climate change, and forest carbon in the Oregon Coast Range. GCB Bioenergy. This Article is brought to you for free and open access. It has been accepted for inclusion in Environmental Science and Management Faculty Publications and Presentations by an authorized administrator of PDXScholar. Please contact us if we can make this document more accessible: [email protected]. Authors Megan K. Creutzburg, Robert M. Scheller, Melissa S. Lucash, Louisa B. Evers, Stephen D. LeDuc, and Mark G. Johnson This article is available at PDXScholar: https://pdxscholar.library.pdx.edu/esm_fac/118 GCB Bioenergy (2016) 8, 357–370, doi: 10.1111/gcbb.12255 Bioenergy harvest, climate change, and forest carbon in the Oregon Coast Range MEGAN K. CREUTZBURG1 , ROBERT M. SCHELLER1 , MELISSA S. LUCASH1 , LOUISA B. EVERS2 , STEPHEN D. LEDUC3 and MARK G. -
The Oregon Coast Range- Considerations for Ecological Restoration Joe Means Tom Spies Shu-Huei Chen Jane Kertis Pete Teensma
Forests of the Oregon Coast Range- Considerations for Ecological Restoration Joe Means Tom Spies Shu-huei Chen Jane Kertis Pete Teensma The Oregon Coast Range supports some of the most dense Ocean, so they are warm and often highly productive, com- and productive forests in North America. In the pre-harvest- pared to the Cascade Range and central Oregon forests. ing period these forests arose as a result of large fires-the Isaac's (1949) site index map shows much more site class I largest covering 330,000 ha (Teensma and others 1991). and I1 land in the Coast Range than in the Cascades. In the These fires occurred mostly at intervals of 150 to 300 years. summers, humid maritime air creates a moisture gradient The natural disturbance regime supported a diverse fauna from the coastal western hemlock-Sitka spruce (Tsuga and large populations of anadromous salmonids (salmon heterophylla-Piceasitchensis) zone with periodic fog extend- and related fish). In contrast, the present disturbance re- ing 4 to 10 km inland, through Douglas-fir (Pseudotsuga gime is dominated by patch clearcuts of about 10-30 ha menziesii var. rnenziesii)-western hemlock forests in the superimposed on most of the forest land with agriculture on central zone to the drier interior-valley foothill zone of the flats near rivers. Ages of most managed forests are less Douglas-fir, bigleaf maple (Acer rnacrophyllum)and Oregon than 60 years. This logging has coincided with significant oak (Quercus garryana). declines in suitable habitat and populations of some fish and wildlife species. Some of these species have been nearly extirpated. -
A Multivariate Geomorphometric Approach to Prioritize Erosion-Prone Watersheds
sustainability Article A Multivariate Geomorphometric Approach to Prioritize Erosion-Prone Watersheds Jesús A. Prieto-Amparán 1, Alfredo Pinedo-Alvarez 1 , Griselda Vázquez-Quintero 2, María C. Valles-Aragón 2 , Argelia E. Rascón-Ramos 1, Martin Martinez-Salvador 1 and Federico Villarreal-Guerrero 1,* 1 Facultad de Zootecnia y Ecología, Universidad Autónoma de Chihuahua, Chihuahua 31453, Mexico; [email protected] (J.A.P.-A.); [email protected] (A.P.-A.); [email protected] (A.E.R.-R.); [email protected] (M.M.-S.) 2 Facultad de Ciencias Agrotecnológicas, Universidad Autónoma de Chihuahua, Chihuahua 31350, Mexico; [email protected] (G.V.-Q.); [email protected] (M.C.V.-A.) * Correspondence: [email protected]; Tel.: +52-(614)-434-1448 Received: 15 August 2019; Accepted: 15 September 2019; Published: 19 September 2019 Abstract: Soil erosion is considered one of the main degradation processes in ecosystems located in developing countries. In northern Mexico, one of the most important hydrological regions is the Conchos River Basin (CRB) due to its utilization as a runoff source. However, the CRB is subjected to significant erosion processes due to natural and anthropogenic causes. Thus, classifying the CRB’s watersheds based on their erosion susceptibility is of great importance. This study classified and then prioritized the 31 watersheds composing the CRB. For that, multivariate techniques such as principal component analysis (PCA), group analysis (GA), and the ranking methodology known as compound parameter (Cp) were used. After a correlation analysis, the values of 26 from 33 geomorphometric parameters estimated from each watershed served for the evaluation. The PCA defined linear-type parameters as the main source of variability among the watersheds. -
Bear Creek Coastal Cutthroat Trout Habitat Connectivity And
Bear Creek Coastal Cutthroat Trout Habitat Connectivity and Enhancement State(s): Oregon Managing Agency/Organization: Long Tom Watershed Council and Bureau of Land Management Type of Organization: Nonprofit Organization/Federal Government Project Status: Underway Project type: WNTI Project Project action(s): Riparian or instream habitat restoration, Barrier removal or construction Trout species benefitted: coastal cutthroat trout Population: Long Tom River Watershed, Bear Creek The project will reconnect 5.5 miles of high-quality headwater spawning habitat and cold water refugia and enhance a one mile stretch of in-stream habitat for coastal cutthroat trout in western Oregon. As part of the project, four, human-made fish passage barriers will be remedied on Bear Creek, an Oregon Coast Range tributary to Coyote Creek about nine miles southwest of Eugene that provides spawning habitat and cold water refugia for coastal cutthroat trout. Three of these barriers are culverts and the other is a dam. The project will leverage significant contributions from the Bureau of Land Management (BLM) Eugene District, Oregon Watershed Enhancement Board, as well as the BLM Resource Advisory Committee to remedy fish- passage barriers on private, BLM, and Lane County Public Works property, resulting in the removal of the final four priority barriers in Bear Creek and the connection of mainstem Coyote Creek to high-quality headwater habitat. Additional project objectives are to place 60 conifer logs in a 0.5 mile stretch of Bear Creek to increase pool depth and frequency and improve in-stream habitat complexity. Effects of the project will be assessed on the physical habitat and fish community in Bear Creek by conducting pre- and post-project rapid bio- assessment snorkel surveys and large woody debris surveys. -
Geomorphic Classification of Rivers
9.36 Geomorphic Classification of Rivers JM Buffington, U.S. Forest Service, Boise, ID, USA DR Montgomery, University of Washington, Seattle, WA, USA Published by Elsevier Inc. 9.36.1 Introduction 730 9.36.2 Purpose of Classification 730 9.36.3 Types of Channel Classification 731 9.36.3.1 Stream Order 731 9.36.3.2 Process Domains 732 9.36.3.3 Channel Pattern 732 9.36.3.4 Channel–Floodplain Interactions 735 9.36.3.5 Bed Material and Mobility 737 9.36.3.6 Channel Units 739 9.36.3.7 Hierarchical Classifications 739 9.36.3.8 Statistical Classifications 745 9.36.4 Use and Compatibility of Channel Classifications 745 9.36.5 The Rise and Fall of Classifications: Why Are Some Channel Classifications More Used Than Others? 747 9.36.6 Future Needs and Directions 753 9.36.6.1 Standardization and Sample Size 753 9.36.6.2 Remote Sensing 754 9.36.7 Conclusion 755 Acknowledgements 756 References 756 Appendix 762 9.36.1 Introduction 9.36.2 Purpose of Classification Over the last several decades, environmental legislation and a A basic tenet in geomorphology is that ‘form implies process.’As growing awareness of historical human disturbance to rivers such, numerous geomorphic classifications have been de- worldwide (Schumm, 1977; Collins et al., 2003; Surian and veloped for landscapes (Davis, 1899), hillslopes (Varnes, 1958), Rinaldi, 2003; Nilsson et al., 2005; Chin, 2006; Walter and and rivers (Section 9.36.3). The form–process paradigm is a Merritts, 2008) have fostered unprecedented collaboration potentially powerful tool for conducting quantitative geo- among scientists, land managers, and stakeholders to better morphic investigations. -
The Upper James River
Waterproof The Upper James River The James River originates at the only class I or II rapids making it ideal will need to plan a river trip. This guide A Paddle Guide to the Upper confluence of the Jackson and Cowpasture for canoe or kayak trips at normal water includes locations of boat landings, rivers in Botetourt County and forms levels. The white water section below campsites, major rapids, and unique Virginia’s longest and most famous river. Glasgow includes a class III section for historic points of interests along the way. The upper section of the James River those interested in more technical water. This is a great resource for planning day is very scenic with stunning Blue Ridge trips as well as multi-day canoe camping mountain views. Dam releases on the This paddle guide covers the upper 64 expeditions. Jackson River flow releases ensure the miles section from the start of the James upper James River is typically run able river to the Cushaw Dam, just below all season. The first 60 miles contain Snowden. It includes everything a paddler Using This Map George Washington and Rapids (See River Safety panel for class system) Jefferson National Forrest* 30 Mile markers— numbered from start of the James Park* River counting down stream Landmark These maps have been orientated so that the river always flows from the bottom of the map to the top of the map. This allows paddlers to easily orient themselves in the river in terms of river right and left while paddling downstream. Bridge 1km Distance gauge 0 1mi North indicator Canal Boat launch Small boat launch Commercial campground River flow River Informal camping Appalachian Trail Hiking Trail *All land along river bank is private property unless noted otherwise. -
Mill Creek Watershed Assessment
Yamhill Basin Council Mill Watershed Assessment December 30, 1999 Funding for the Mill Assessment was provided by the Oregon Watershed Enhancement Board and Resource Assistance for Rural Environments. Mill Assessment Project Manager: Robert J. Bower, Principal Author Co-authors: Chris Lupoli, Linfield College intern, for Riparian section and assisted with Wetlands Conditions section. Tamara Quandt, Linfield College intern, for Sensitive Species section. Editors: Melissa Leoni, Yamhill Basin Council, McMinnville, OR Alison Bower, Forest Ecologist, Corvallis, OR Contributors: Bill Ferber, Salem, Water Resources Department (WRD) Chester Novak, Salem, Bureau Land Management (BLM) Dan Upton, Dallas, Willamette Industries David Anderson, Monmouth, Boise Cascade Dean Anderson, Dallas, Polk County Geographical Information Systems (GIS) Dennis Ades, Salem, Department of Environmental Quality (DEQ) Gary Galovich, Corvallis, Oregon Department Fish and Wildlife (ODFW) Mark Koski, Salem, Bureau of Land Management (BLM) Patrick Hawe, Salem, Bureau of Land Management (BLM) Rob Tracey, McMinnville, Natural Resource and Conservation Service (NRCS) Stan Christensen, McMinnville, Yamhill Soil Water Conservation District Susan Maleki, Corvallis, Oregon Watershed Enhancement Board (OWEB) Warren Tausch, Tillamook Bureau of Land Management (BLM) Special Thanks: ! John Cruickshank, Gooseneck Creek resident for his assistance with the Historical, and Channel Modification sections and in the gathering of historical photographs. ! Gooseneck Creek Watershed Group for their support and guidance. ! John Caputo, Yamhill County GIS. ! BLM and Polk County GIS for providing some of the GIS base layers used to create the maps in this assessment. ! USDA Service Center, Natural Resource Conservation Service, McMinnville, for copying and office support. ! Polk and Yamhill Soil and Water Conservation Districts. ! Nick Varnum, PNG Environmental Inc., Tigard, for assisting with the Hydrology and Channel Habitat Typing sections. -
I I 71-15,061 CAMERON, Christopher Paul, 1940- PALEOMAGNETISM of SHEMYA and ADAK ISLANDS, ALEUTIAN ISLANDS, ALASKA. University O
Paleomagnetism Of Shemya And Adak Islands, Aleutian Islands, Alaska Item Type Thesis Authors Cameron, Christopher Paul Download date 23/09/2021 14:56:00 Link to Item http://hdl.handle.net/11122/9194 I I 71-15,061 CAMERON, Christopher Paul, 1940- PALEOMAGNETISM OF SHEMYA AND ADAK ISLANDS, ALEUTIAN ISLANDS, ALASKA. University of Alaska, Ph.D., 1970 Geology University Microfilms, A XEROX Company, Ann Arbor, Michigan tutc nTCCTDTATTOM MAC HTTM MTPROFIT.MFD F.VAPTT.Y AS RF.OF.TVF.D Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. PALE01IAGNETISM OF SHEMYA AMD ADAK ISLAUDS, ALEUTIAN ISLANDS, ALASKA A DISSERTATION Presented to the Faculty of the University of Alaska in Partial Fulfillment of the Requirements for the Degree of DOCTOR OF PHILOSOPHY by Christopher P/" Cameron B. S. College, Alaska May, 1970 Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. PALEOilAGNETISM OF SHEMYA AND ADAK ISLANDS, ALEUTIAN ISLANDS, ALASKA APPROVED: f t l ‘y l .V" ■i. n ■ ■< < ; N w 1 T *W -C ltc-JL It / _ _ ____ /vx... , ~ ~ 7 YdSV Chairman APPPvOVED: dai£ 3 / 3 0 / 7 0 Dean of the College of Earth Sciences and Mineral Industry Vice President for Research and Advanced Study Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. ABSTRACT Paleomagnetic results are presented for Tertiary and Quaternary volcanic rocks from Shemya and Adak Islands, Aleutian Islands, Alaska. The specimens were collected and measured using standard paleomagnetic methods. Alternating field demagnetization techniques were applied to test the stability of the remanence and to remove unwanted secondary components of magnetization. -
Junction City Water Control District Long-Term Irrigation Water Service Contract
Junction City Water Control District Long-Term Irrigation Water Service Contract Finding of No Significant Impact Environmental Assessment Willamette River Basin, Oregon Pacific Northwest Region PN EA 13-02 PN FONSI 13-02 U.S. Department of the Interior Bureau of Reclamation Columbia-Cascades Area Office Yakima, Washington June 2013 MISSION STATEMENTS U.S. Department of the Interior Protecting America’s Great Outdoors and Powering Our Future The Department of the Interior protects America’s natural resources and heritage, honors our cultures and tribal communities, and supplies the energy to power our future. Bureau of Reclamation The mission of the Bureau of Reclamation is to manage, develop, and protect water and related resources in an environmentally and economically sound manner in the interest of the American public. FINDING OF NO SIGNIFICANT IMPACT Long-Term Irrigation Water Service Contract, Junction City Water Control District U.S. Department of the Interior Bureau of Reclamation Columbia-Cascades Area Office PN FONSI13-02 Decision: It is my decision to authorize the Preferred Alternative, Alternative B - Long-term Water Service Contract, identified in EA No. PN-EA-13-02. Finding of No Significant Impact: Based on the analysis ofpotential environmental impacts presented in the attached Environmental Assessment, Reclamation has determined that the Preferred Alternative will have no significant effect on the human environment or natural and cultural resources. Reclamation, therefore, concludes that preparation of an Environmental -
Risk Assessment
SECTION 2: RISK ASSESSMENT This section of the NHMP addresses 44 CFR 201.6(b)(2) - Risk Assessment. The Risk Assessment applies to Polk County and the Cities of Dallas, Falls City, Independence, and Monmouth. City specific information is called out where relevant. In addition, this chapter can assist with addressing Oregon Statewide Planning Goal 7 – Areas Subject to Natural Hazards. The information presented below, along with hazard specific information presented in the Hazard Annexes and community characteristics presented in the Community Profile Appendix, is used to inform the risk reduction actions identified in Section 3 – Mitigation Strategy. The risk assessment process is graphically depicted in Figure 2-1 below. Ultimately, the goal of hazard mitigation is to reduce the area where hazards and vulnerable systems overlap. Figure 2-1 Understanding Risk Source: Oregon Partnership for Disaster Resilience. Polk County NHMP October 2017 Page 2-1 What is a Risk Assessment? A risk assessment consists of three phases: hazard identification, vulnerability assessment, and risk analysis. • Phase 1: Identify hazards that can impact the jurisdiction. This includes an evaluation of potential hazard impacts – type, location, extent, etc. • Phase 2: Identify important community assets and system vulnerabilities. Example vulnerabilities include people, businesses, homes, roads, historic places and drinking water sources. • Phase 3: Evaluate the extent to which the identified hazards overlap with, or have an impact on, the important assets identified by the community. The following figure illustrates the three-phase risk assessment process: Figure 2-2 Three Phases of a Risk Assessment Source: Planning for Natural Hazards: Oregon Technical Resource Guide, 1998 This three-phase approach to developing a risk assessment should be conducted sequentially because each phase builds upon data from prior phases. -
River Dynamics 101 - Fact Sheet River Management Program Vermont Agency of Natural Resources
River Dynamics 101 - Fact Sheet River Management Program Vermont Agency of Natural Resources Overview In the discussion of river, or fluvial systems, and the strategies that may be used in the management of fluvial systems, it is important to have a basic understanding of the fundamental principals of how river systems work. This fact sheet will illustrate how sediment moves in the river, and the general response of the fluvial system when changes are imposed on or occur in the watershed, river channel, and the sediment supply. The Working River The complex river network that is an integral component of Vermont’s landscape is created as water flows from higher to lower elevations. There is an inherent supply of potential energy in the river systems created by the change in elevation between the beginning and ending points of the river or within any discrete stream reach. This potential energy is expressed in a variety of ways as the river moves through and shapes the landscape, developing a complex fluvial network, with a variety of channel and valley forms and associated aquatic and riparian habitats. Excess energy is dissipated in many ways: contact with vegetation along the banks, in turbulence at steps and riffles in the river profiles, in erosion at meander bends, in irregularities, or roughness of the channel bed and banks, and in sediment, ice and debris transport (Kondolf, 2002). Sediment Production, Transport, and Storage in the Working River Sediment production is influenced by many factors, including soil type, vegetation type and coverage, land use, climate, and weathering/erosion rates.