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Page 1: Geomorphology of - King County, Washington › dnrp › library › water-and...Geomorphology of Stream Channels in the Lower Snoqualmie River Watershed. Green-shaded areas have bedrock
Page 2: Geomorphology of - King County, Washington › dnrp › library › water-and...Geomorphology of Stream Channels in the Lower Snoqualmie River Watershed. Green-shaded areas have bedrock

Geomorphology ofStream Channels in

the Lower Snoqualmie River Watershed

Page 3: Geomorphology of - King County, Washington › dnrp › library › water-and...Geomorphology of Stream Channels in the Lower Snoqualmie River Watershed. Green-shaded areas have bedrock

Green-shaded areas have bedrock at or near the ground surface

Page 4: Geomorphology of - King County, Washington › dnrp › library › water-and...Geomorphology of Stream Channels in the Lower Snoqualmie River Watershed. Green-shaded areas have bedrock

The Maximum Extent of the Puget Lobe of the Cordilleran ice sheet during the Vashon stade of the Fraser (late Wisconsin) glaciation. Approximately 14,000 years bp. Contour lines show ice thickness in meters.

Easterbrook, 1979

Seattle

Page 5: Geomorphology of - King County, Washington › dnrp › library › water-and...Geomorphology of Stream Channels in the Lower Snoqualmie River Watershed. Green-shaded areas have bedrock

Major Glacial Troughs in

the Eastern Puget

Lowland

Page 6: Geomorphology of - King County, Washington › dnrp › library › water-and...Geomorphology of Stream Channels in the Lower Snoqualmie River Watershed. Green-shaded areas have bedrock

Major Glacial Troughs in

the Eastern Puget

Lowland

Page 7: Geomorphology of - King County, Washington › dnrp › library › water-and...Geomorphology of Stream Channels in the Lower Snoqualmie River Watershed. Green-shaded areas have bedrock
Page 8: Geomorphology of - King County, Washington › dnrp › library › water-and...Geomorphology of Stream Channels in the Lower Snoqualmie River Watershed. Green-shaded areas have bedrock

Lower Snoqualmie Mainstem

Page 9: Geomorphology of - King County, Washington › dnrp › library › water-and...Geomorphology of Stream Channels in the Lower Snoqualmie River Watershed. Green-shaded areas have bedrock

Figure 21 Snoqualmie Streambed Sediment Texture (Booth et. al. 1991)

0

10

20

30

40

50

60

0 5 10 15 20 25 30 35 40 45 50

River Mile

d 50 (

mm

)

Tolt

Rag

ing

Toku

l

Thre

e Fo

rks

The particle size shown is for for the median particle size (d50) for the subsurface sample collected at each sample site. The texture of the subsurface sediment in an alluvial channel bed is similar to the texture of the of the bedload sediment in transport at the sample location.

Page 10: Geomorphology of - King County, Washington › dnrp › library › water-and...Geomorphology of Stream Channels in the Lower Snoqualmie River Watershed. Green-shaded areas have bedrock

Ripple marks in sand on the bed of the Snoqualmie River

near Duvall

Page 11: Geomorphology of - King County, Washington › dnrp › library › water-and...Geomorphology of Stream Channels in the Lower Snoqualmie River Watershed. Green-shaded areas have bedrock

Meandering Channel and natural levees on the Lower Snoqualmie Mainstem

Page 12: Geomorphology of - King County, Washington › dnrp › library › water-and...Geomorphology of Stream Channels in the Lower Snoqualmie River Watershed. Green-shaded areas have bedrock

A com

parison of wetlands show

n on the floor of the S

noqualmie V

alley in 1873 GLO

mapping

(left) with recent U

SG

S m

apping (right).

Page 13: Geomorphology of - King County, Washington › dnrp › library › water-and...Geomorphology of Stream Channels in the Lower Snoqualmie River Watershed. Green-shaded areas have bedrock

Lower Tolt River

Page 14: Geomorphology of - King County, Washington › dnrp › library › water-and...Geomorphology of Stream Channels in the Lower Snoqualmie River Watershed. Green-shaded areas have bedrock

Lower Raging River

Page 15: Geomorphology of - King County, Washington › dnrp › library › water-and...Geomorphology of Stream Channels in the Lower Snoqualmie River Watershed. Green-shaded areas have bedrock

Landslides along the

Lower Tolt

Valley

Page 16: Geomorphology of - King County, Washington › dnrp › library › water-and...Geomorphology of Stream Channels in the Lower Snoqualmie River Watershed. Green-shaded areas have bedrock

Braiding on the Tolt River above Carnation

Page 17: Geomorphology of - King County, Washington › dnrp › library › water-and...Geomorphology of Stream Channels in the Lower Snoqualmie River Watershed. Green-shaded areas have bedrock

Plane-bed Channel in the Raging River

Page 18: Geomorphology of - King County, Washington › dnrp › library › water-and...Geomorphology of Stream Channels in the Lower Snoqualmie River Watershed. Green-shaded areas have bedrock

Approximate Extent, Tolt Fan

Page 19: Geomorphology of - King County, Washington › dnrp › library › water-and...Geomorphology of Stream Channels in the Lower Snoqualmie River Watershed. Green-shaded areas have bedrock
Page 20: Geomorphology of - King County, Washington › dnrp › library › water-and...Geomorphology of Stream Channels in the Lower Snoqualmie River Watershed. Green-shaded areas have bedrock

Gravel bar at the mouth of the Raging River Snoqualmie with bank erosion on the opposite bank.

Page 21: Geomorphology of - King County, Washington › dnrp › library › water-and...Geomorphology of Stream Channels in the Lower Snoqualmie River Watershed. Green-shaded areas have bedrock

East Side Tributaries

Area of Channelways outlined in blue

Page 22: Geomorphology of - King County, Washington › dnrp › library › water-and...Geomorphology of Stream Channels in the Lower Snoqualmie River Watershed. Green-shaded areas have bedrock

Channelways in the Griffin Creek drainage.

Page 23: Geomorphology of - King County, Washington › dnrp › library › water-and...Geomorphology of Stream Channels in the Lower Snoqualmie River Watershed. Green-shaded areas have bedrock
Page 24: Geomorphology of - King County, Washington › dnrp › library › water-and...Geomorphology of Stream Channels in the Lower Snoqualmie River Watershed. Green-shaded areas have bedrock

Cascade Channel in Peoples Creek

Page 25: Geomorphology of - King County, Washington › dnrp › library › water-and...Geomorphology of Stream Channels in the Lower Snoqualmie River Watershed. Green-shaded areas have bedrock

Current excavated Cherry Creek channel

Original Cherry Creek channel

Page 26: Geomorphology of - King County, Washington › dnrp › library › water-and...Geomorphology of Stream Channels in the Lower Snoqualmie River Watershed. Green-shaded areas have bedrock

West Side Tributaries

Page 27: Geomorphology of - King County, Washington › dnrp › library › water-and...Geomorphology of Stream Channels in the Lower Snoqualmie River Watershed. Green-shaded areas have bedrock
Page 28: Geomorphology of - King County, Washington › dnrp › library › water-and...Geomorphology of Stream Channels in the Lower Snoqualmie River Watershed. Green-shaded areas have bedrock

Adair Creek Profile

Page 29: Geomorphology of - King County, Washington › dnrp › library › water-and...Geomorphology of Stream Channels in the Lower Snoqualmie River Watershed. Green-shaded areas have bedrock
Page 30: Geomorphology of - King County, Washington › dnrp › library › water-and...Geomorphology of Stream Channels in the Lower Snoqualmie River Watershed. Green-shaded areas have bedrock

Boulder and wood step-weir on Tuck Creek

Page 31: Geomorphology of - King County, Washington › dnrp › library › water-and...Geomorphology of Stream Channels in the Lower Snoqualmie River Watershed. Green-shaded areas have bedrock
Page 32: Geomorphology of - King County, Washington › dnrp › library › water-and...Geomorphology of Stream Channels in the Lower Snoqualmie River Watershed. Green-shaded areas have bedrock

Severe Incision in a small tributary channel that decends the west wall of the Snoqualmie Valley near Carnation. The erosion is a result of changes to the basin hydrology as a result of upstream land development

The “Little Grand Canyon”

Photo Courtesy of Derek Booth

Page 33: Geomorphology of - King County, Washington › dnrp › library › water-and...Geomorphology of Stream Channels in the Lower Snoqualmie River Watershed. Green-shaded areas have bedrock
Page 34: Geomorphology of - King County, Washington › dnrp › library › water-and...Geomorphology of Stream Channels in the Lower Snoqualmie River Watershed. Green-shaded areas have bedrock

Pen and Ink by Frank Grouberg