Sucker Creek Design Draft

Slides:



Advertisements
Similar presentations
River Regulation / Dam Construction – Effects on Rivers and Streams.
Advertisements

Meeting Two More Theory
The Middle and Lower Course of a River
Oxbow Lakes By Cara.
This project and its actions were made possible due to co-financing by the European Fund for the Integration of Third-Country Nationals Rivers River features.
Introduction to Hydrology: Floodplains & Drainage Basins Lessons 21 & 22 Introduction to hydrology  Introduction to hydrology  Stream types, orders,
Assessment of gravel transport characteristics of the upper Santa Ana River Scott Wright and Toby Minear USGS California Water Science Center Sacramento,
Channel Pattern Outline Description of channel pattern Alternate bars Channel pattern continua and evolution Controls of channel pattern.
Fluvial Geomorphology Lab 7. Concepts Basic concepts and definitions Types of work performed by streams Alluvium Base level Watersheds/Drainage Basins.
Background: In the mid 18 th century a dam was built at E N for the E.N. Colton shingle and saw mills along the Mill Brook in the town of.
FLOODS, STREAMS AND MEANDERS. GAUGING STATION On all major streams Measures Stream Height Height vs. Discharge (volume) Flood Stage and height above Flood.
Biological Objectives Tied to Physical Processes Dr. William Trush Scott McBain Arcata, CA.
Lab 8 Stream Processes. Channel Types Braided - steeper, large sediment supply Meandering - less steep, lower sediment supply.
Watershed Assessment and River Restoration Strategies
Unit 4: Gradational Processes Ms. Thind
Channel Modification Washington Dept. Forestry, 2004, Channel Modification Techniques Katie Halvorson.
Stream Processes and Habitat Ryan Johnson. Overview Watershed Processes – Factors and their effects on the watershed as a whole Stream Processes – Factors.
Streams (Rivers). Runoff: H 2 0 that does not sink into ground Most ends up in streams.
13 Surface Water 13.1 Streams and Rivers
RIVERS. A meander is a turning or winding of a stream Incised meanders of Dolores River, Colorado.
Comparison of Geomorphic Change in Two Flood Events on the Umatilla River, Oregon Patricia McDowell, Michael L. Hughes, and W. Andrew Marcus Department.
Rivers: Fluvial Processes
Stream Erosion and Transport
A stream is a body of water that carries rock particles and dissolved ions and flows down slope along a clearly defined path, called a channel. Thus, streams.
Geomorphology.
As you know from Chapter 2, weathering is the breakdown of rocks into smaller pieces. So what is erosion? Erosion is the movement of the broken or weathered.
A river system is made up of a main stream and tributaries – Tributary: a stream that flows into a lake or into a larger stream.
(,rivers, brooks, creeks, etc.)
Stream Channel Geology. Stream Channel Behavior CCCChannel shape and Velocity Less contact with channel = greater velocity Deeper narrow channels.
Water Erosion Chapter 3 Section 2. Standard S 6.2.a – Students know water running downhill is the dominant process in shaping the landscape S 6.2.a.
A meander is a turning or winding of a stream Incised meanders of Dolores River, Colorado.
TRANSPORTATION & DEPOSITION in a Stream System.
Landforms and Oceans 5.E.3A.1 Construct explanations of how different landforms and surface features result from the location and movement of water on.
Snohomish County Surface Water Management R2 Resource Consultants
River Characteristics
Streams Water flowing through a channel ranging from a large river to a narrow creek.
Deposition Notes and Stream Life History Notes
Erosion of rock by moving water
AIM: What is a stream/river?
Image Analysis Task: Describe the features shown in each of the images. How do you think they have been formed? Extension: Come and collect an exam skills.
RIVERS AS AGENTS OF EROSION, TRANSPORTATION AND DEPOSITION
Fish Passage Restoration at Roy’s Pools
Warm-up What are four things that impact INFILTRATION? (the answer is in your notes) After you finish the warm-up put your river basin project in the inbox.
River Processes.
River System Development
Erosional/Depositional Systems
River Erosion River Erosion.
Water Testing Project for the North Fork River
Chapter 13 Notes.
Jeopardy Rocks Weathering Erosion Glaciers Water Q $100 Q $100 Q $100
River Erosion / Deposition
Study Update Tailrace Slough Use by Anadromous Salmonids
Meandering Rivers.
The Work of Streams.
The life cycle of a river
Chapter 18.
Gradient The land surrounding the river channel. Valley The middle section of the river. Upper Course The steepness of the river. Mid Course The part of.
stream, river, lake, wetland, or ocean
Characteristics of a Mature Stream
River Systems Part 2 Features of a Meandering River Levees
Streams Hydrodynamics
Water Cycle, Groundwater, Aquifers, Caves
Streams Hydrodynamics
1ST YEAR OF ESO RIVERS PROFESOR TIERNO GALVÁN SECONDARY SCHOOL.
Streams and Rivers cont’d
River Erosion River Erosion.
Rivers and Streams Chapter 6.1 and 6.2.
Common Stream Habitat Problems
STREAMS AND THE EARTH Water Erosion
Stages in the Development of a River Valley
Presentation transcript:

Sucker Creek Design Draft (Existing Condition) Poor fisheries habitat Incised channel Bridge Settling ponds Tailings pile Disconnected ponds Existing condition Flow Direction

Sucker Creek Conceptual Design-A Draft (channel pattern and layout) Create mid-channel island Connect to existing tribs or cold water seeps Bridge Side-Channel habitat (active during higher water) A A Settling ponds Tailings pile Notes: 1st island after bridge. Split flow around mid channel bar island. Careful not to let it agrade over time. And not too high to prevent wood and sediment from being transported downstream. Bring one side along valley wall and connect to side tribs for cold refuge, over-wintering habitat, spawning habitat, connection with tribs. Create oxbow lakes and meander scars for habitat. Project area is a depositional zone which is causing channel migration towards valley walls as sediment builds up. This is why we see large meander wavelengths and tight radius of curvatures. Baseflows estimated at 30-40 cfs. A design alternative to allow flow year round is to create smaller side channels, more like islands along mainstem. This could provide an alternative if banks are high or channel is incised. Channel Reconstruction Key Perennial Flow FMF Large Wood Complex Grade Control Structures Active During higher flows Island Bar Buddies Constructed Spawning Areas Bridge not to scale

Cut/Fill Estimations Bridge Settling ponds Tailings pile Reach 1 channel reconstruction volume is estimated to be approx 10% greater than that estimated for the side-channel.

Perspective View Flow Direction

1.5yr Flood (HEC-RAS analysis) 820 cfs

10 yr Flood (HEC-RAS analysis)

100 yr Flood (HEC-RAS analysis) 5,271 cfs