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The Landscape of Puget Sound: Tectonics and Glaciers Courtesy Derek Booth

The Landscape of Puget Sound: Tectonics and GlaciersSan Andreas fault. Subducting of Juan de Fuca plate. Resulting N-S shortening in the Puget Lowland. Crescent Fm. Quaternary. Blakeley

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  • The Landscape of Puget Sound: Tectonics and Glaciers

    Courtesy Derek Booth

  • 1) Big hole between the mountains

    2) Advance outwash plain

    3) TroughsHood CanalPuget SoundLk WashingtonKent Valley

    4) Flutes

    E-W cross-section

    Puget Lowland Landscape Elements

  • Tectonic setting of the Puget Lowland

    San Andreas fault

    Subducting ofJuan de Fuca plate

    Resulting N-S shortening in the Puget Lowland

  • Crescent Fm

    Quaternary

    Blakeley Fm

    Blakely Harbor Fm

    Eocene

    Seattle basinSeattle uplift Kingston arch

    km

    South North

    After Johnson et al., 1994

    Bedrock Structure through Puget Sound

    {

    {{

    Seattle fault zone

    {

  • Topographic expression of the Seattle fault

    Bedrock highs

  • Scarp of Utsalady Fault – Whidbey Island

  • 1) Big hole between the mountains

    2) Advance outwash plain

    3) Troughs4) Flutes5) Cross-warps

  • Booth, et al, 2003

  • K. Troost

  • Photographer: Roger Slatt University of OklahomaCaption: This view of the Athabasca Glacier shows depositional features as well as erosional features. The glacier is a feature of Alberta's Jasper National Park and is fed by the Columbia Ice Field.

    Lateral Moraine

    Terminal Moraine

  • Recessional Moraine

    Central Whidbey Island Lidar

    Outwash Channels

    Kettles (holes from melted ice blocks)

    Drumlins, Flutes

  • Double Bluff Section

  • Vashon till at Perkins Lane

    2m

    Photo by K. Troost

  • 2) Advance outwash fill plain, Puget Lowland

  • Flow at snout of Nigardsbreen glacier, Norway

    Water flowing into moulin

  • 3) Troughs (subglacial channelways)—products of glacial meltwater

  • 3) Troughs (subglacial channelways)—products of glacial meltwater

    = troughs filled in bylate-recessional orpostglacial alluviumor mudflows

  • 3) Troughs (subglacial channelways)—products of glacial meltwater

    = troughs filled in bylate-recessional orpostglacial alluviumor mudflows

    Gradients of subglacial water flow

  • 1) Big hole between the mountains

    2) Advance outwash plain

    3) Troughs4) Flutes5) Cross-warps

  • 4) Flutes = glacial scour

    24 kmDEM from Haugerud, 2001

    PresenterPresentation NotesShaded-relief image

  • Oblique aerial view of flutes around Echo Lake

  • Landscape element #5: Cross-warps

    Image from Seattle-Area Geologic Mapping Project

  • Slide Number 1Slide Number 2Slide Number 3Slide Number 4Slide Number 5Slide Number 6Slide Number 7Scarp of Utsalady Fault – Whidbey IslandSlide Number 9Slide Number 10Slide Number 11Slide Number 12Slide Number 13Central Whidbey Island LidarDouble Bluff SectionSlide Number 16Slide Number 17Slide Number 18Slide Number 19Slide Number 20Slide Number 21Slide Number 22Slide Number 234) Flutes = �glacial scourSlide Number 25Slide Number 26Slide Number 27