EISI Deschutes River Module - Summer 2009 Start End

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EISI Deschutes River Module - Summer 2009

Steve Taylor, Earth and Physical Sciences, Western Oregon University

Start

End

LEARNING OBJECTIVES

To engage team building in the context of outdoor adventure and experiential education

To acquire knowledge of the regional geologic, hydrologic, and geomorphic setting of western

Oregon

To apply spatial and temporal scaling concepts to watershed systems

To develop skills in field-based observation, data collection, analysis, and hypothesis testing

To gain experience with techniques of landscape analysis and interpretation of the geologic record

To

HJA

EISI Float

Location of dams

Ochoco

Mtns

Ad = 26,860 sq. km

N-S length ~ 300 km

3 hydroelectric dams

John Day Basin to east

Cascades to west

Geology

 John Day and Clarno Forma-

 tions (55-20 m.y. old)

Columbia River Basalts

(17-14 m.y.)

 Deschutes Fm volcanics

(10-2 m.y.)

 Pleistocene and Holocene surficial deposits (< 1 m.y.)

Avg. rainfall < 1000 mm

Semi-Arid

Avg. Runoff = 0.19 m

Q range: 124-213 cms

Pacific Northwest Climate and Tectonics:

Linked System Drivers

“Wet”

Westerly cyclonic storm systems

“Dry”

Deschutes

HJA

Field Trip Content

Regional physiography of Cascades and central Oregon

Geology, geomorphology and hydrology of Deschutes Basin

Introduction to geologic observation and landscape analysis

Fundamental principles of hydrology and geomorphology

Fundamentals of fisheries, riparian habitat, watershed assessment, and river restoration

Participant Deliverables And Assessment

Pre-trip reading questions

Active learning assignments

Post-trip reflection paper

Smiles, laughter, fun, friends, adventurous stories to tell

LOGISTICS

Travel HJA to Trout Creek, Sunday, June 21, PM

3 nights camping; 2.5 days rafting, ~55 river miles

Field support: river guides, paddle boats, bag boats

Food: 3-a-day provided except for Trout Ck. Camp

Camp kitchen and staff cooks provided

Extra group coolers, snacks, specialty items = CYA

Personal gear stowed in dry bags / on bag boats

Tent teams encouraged

Dry and sunny, rain possible, cold water, WIND

Prepare for sunburn, dehydration, prickly vegetation

Other stuff: water shoes / river sandals, sleeping bag, sleeping pad, tent, flashlight, closed shoes for hiking, swimming / fly fishing, towel, soap/shampoo, river baths

INTRODUCTION TO WATERSHEDS AND RIVERS

Energy Sources in the

Fluvial System

Gravitational

Solar (Climate)

Geothermal (Tectonics)

Work of the

Fluvial System

Transfer of Energy

Transfer of Mass

Water

Sediment

Rafting People

WATERSHEDS: Scalable Routing Networks

(Tectonics)

The physical work of rivers: transport sediment and water

Ecological services and riparian habitat

“Hey Taylor – note to self…now’s the time to show the video clip illustrating hillslope-valley bottom process-response mechanisms and the interaction between variables, including human impacts from geomorphic change…”

And now a message from our sponsor: kayakingsucks.com

…increasing the scale of this example…

Columbia River Gorge: Bridge of the Gods Landslide Complex

-Blocked river ca. 300 yrs ago

-Legacy effects on landscape

Landscape Analysis: Landform, Material, Process, Age

The record of past processes and tapestry of time…

Material: Sedimentary

Bedrock (Age = 20 m.y.)

Hillslope

Regime

Process:

Anthropogenic

Process: Alluvial

Transport

Valley-Bottom

Regime

Material: Angular Cobbles

(Age = 10,000 yr)

Process: Colluvial

Transport

Material: Gravel

(Age = 2000 yr)

Material: Igneous

Bedrock (Age = 100 m.y.)

Material: Unconsolidated

Sandy Gravel (Age = last winter)

Stream Processes and

Floodplain Development

Age of landscape features and rates of processes: the most elusive facets of study.

Geologically Relevant Time Scales: 10 -5 to 10 9 Years

(minutes-hours-days-years-thousands-hundreds of thousands-millions-billions of years)

Engineering Time Scales? 10 0 to 10 2 yrs (then build another one…)

Age of Landforms (Surfaces)

River Terrace

Age of Deposits (Terrace Deposits)

How long since these gravels were last transported by channel processes?

Synergistic extension to Eco-Informatics work at HJ Andrews

Experimental Forest, “the home of long-term watershed research in the Pacific Northwest”?… 2009 EISI campers, academic enlightenment is knocking at your door, seize the moment!

WS-10

684

Streamflow gaging stations

Spot elevations meters AMSL

Experimental watershed (WS)

OREGON

Rid ge

Ri ve r

B lu e

Lo ok ou t

549

Creek

WS-7

WS-6

WS-8

991

M cR ae

WS-9

427

WS-1

WS-3

WS-2

Carpenter

Mountain

1630

Cr ee k

1230

Linn County

Lane County

0 1 km

Lookou t

1347

Ridge

M ac k

Creek

1609

Lookout

Mountain

1312

1098

1568

Frissel

Point

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