Index Catalog // ScholarsArchive@OSU

The effects of hillslope and fluvial processes on particle size of the stream bed at the watershed, reach and within-reach scales in a fifth-order mountain stream

Creator:: Lambert, Beth C.
Abstract:: This study addressed the effects of hilislope and fiuvial processes on spatial patterns of stream bed particle size at the watershed, reach and within-reach scales. The study was conducted in Lookout Creek watershed, a fifth-order, 64 km2 basin in the Western Cascades mountains of Oregon. Stream bed particle size was...
Resource Type:: Masters Thesis

Evaluation of suspended sediment discharges from the Willow Creek Basin : project completion report

Creator:: Koelliker, James K. and Oregon State University. Water Resources Research Institute
Resource Type:: Technical Report
Full Text:: Land Use Data for Willow Creek Basin, 1970 8 2 Use of Cropland in Morrow County, Oregon

An assessment of a Stream Reach Inventory and Channel Stability Evaluation : predicting and detecting flood-induced change in channel stability

Creator:: Morét, Stephanie L.
Abstract:: Pre-flood (1995), and post-flood (1996) channel stability surveys were conducted on 22 reaches along Oak Creek, Benton County, Oregon in an effort to note if the flood of February 1996 altered the channel and if the channel stability survey that was being used accurately predicted the channels resistance to change...
Resource Type:: Masters Thesis
Full Text:: of Oregon and the Oak Creek Watershed is displayed in Figure 2. 2.1.2 The Five Research Areas and

Particle selection for tube building and the stabilization of sediments by Leptochelia dubia (Crustacea, Tanaidacea): interactions with bacteria and microalgae

Creator:: Krasnow, Lynne D.
Resource Type:: Dissertation

Sediment production from forest roads in the upper Oak Creek Watershed of the Oregon Coast Range

Creator:: Amann, Joseph R.
Abstract:: Unpaved roads are sources of chronic sediment in forested watersheds. Bare soil on roads is exposed to erosion from rainfall and runoff Published research on sediment production from forest roads focuses primarily on road characteristics. Since water drives the mechanics of sediment transport, hydrologic variables should correlate with sediment production....
Resource Type:: Masters Thesis

Along-coast variations of Oregon beach-sand compositions produced by the mixing of sediments from multiple sources under a transgressing sea

Creator:: Clemens, Karen E.
Abstract:: Heavy mineral compositions of sands from Oregon beaches, rivers and sea cliffs have been determined in order to examine the causes of marked along-coast variations in the beach-sand mineralogy. The study area extends southward from the Columbia River to the Coquille River in southern Oregon. The heavy-mineral compositions were determined...
Resource Type:: Masters Thesis
Full Text:: Heavy mineral compositions of sands from Oregon beaches, rivers and sea cliffs have been determined in

Sediment characteristics and the trophic status of four Oregon lakes : project completion report

Creator:: Davis, Gerald E. and Larson, Gary L.
Abstract:: This study was undertaken to evaluate the usefulness of sediment records for correlating changes in the sediment characteristics of four Oregon lakes with past cultural developments of the lakes and their watersheds. The lakes chosen for this study were Waldo, Odell, and Diamond lakes located in the Cascade mountains and...
Resource Type:: Technical Report
Full Text:: Sediment Characteristics and the Trophic Status of Four Oregon Lakes

Influence of hillslope and instream processes on channel morphology of Esmond Creek in the Oregon Coast Range

Creator:: Dent, Elizabeth F.
Abstract:: Esmond Creek is a tributary to the Siuslaw River located in the Oregon Coast Range. It is 18 km in length and drains a watershed area is 48.9 km². Average channel gradient of the study reach is 0.9%. In 1988 a landslide occurred in the Esmond Creek watershed involving approximately...
Resource Type:: Masters Thesis
Full Text:: MORPHOLOGY OF ESMOND CREEK IN THE OREGON COAST RMGE INTRODUCTION Channel morphology is a function of the

Patterns of hillslope and channel recovery following disturbances in steep, forested basins

Creator:: Madej, Mary Ann
Abstract:: Geomorphic response to watershed disturbances commonly results in alterations of landforms. Subsequent geomorphic recovery is dependent on the ability of flows to entrain, transport, and organize inorganic and organic material on hillslopes and in channels. This research analyzed changes in sediment production, channel structure, and channel organization following disturbances in...
Resource Type:: Dissertation
Full Text:: network in the Redwood Creek basin. I thank anonymous reviewers for their insight and helpful comments

Valley fill and channel incision in Meyer's Canyon, northcentral Oregon

Creator:: Peacock, Kathi A.
Abstract:: Meyer's Canyon, a tributary of Bridge Creek in the John Day Basin, is a deeply incised valley fill in northcentral Oregon. The current channel is incised to the Cretaceous and Tertiary bedrock. To determine the precedence of the current incision and the variation and timing of depositional sequences, the sediments...
Resource Type:: Masters Thesis

ScholarsArchive@OSU

The effects of hillslope and fluvial processes on particle size of the stream bed at the watershed, reach and within-reach scales in a fifth-order mountain stream

Evaluation of suspended sediment discharges from the Willow Creek Basin : project completion report

An assessment of a Stream Reach Inventory and Channel Stability Evaluation : predicting and detecting flood-induced change in channel stability

Particle selection for tube building and the stabilization of sediments by Leptochelia dubia (Crustacea, Tanaidacea): interactions with bacteria and microalgae

Sediment production from forest roads in the upper Oak Creek Watershed of the Oregon Coast Range

Along-coast variations of Oregon beach-sand compositions produced by the mixing of sediments from multiple sources under a transgressing sea

Sediment characteristics and the trophic status of four Oregon lakes : project completion report

Influence of hillslope and instream processes on channel morphology of Esmond Creek in the Oregon Coast Range

Patterns of hillslope and channel recovery following disturbances in steep, forested basins

Valley fill and channel incision in Meyer's Canyon, northcentral Oregon

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