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Toe Jam Hill Fault

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Journal Article
Journal: GSA Bulletin
Published: 01 November 2003
GSA Bulletin (2003) 115 (11): 1388-1403.
... fault in western Washington. The scarp, the first to be revealed by laser imagery, marks the Toe Jam Hill fault, a north-dipping backthrust to the Seattle fault. Folded and faulted strata, liquefaction features, and forest soil A horizons buried by hanging-wall-collapse colluvium record three...
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TABLE 1. VERTICAL COMPONENT AND RATE OF DEFORMATION INFERRED FROM TRENCHES ...
Published: 01 November 2003
TABLE 1. VERTICAL COMPONENT AND RATE OF DEFORMATION INFERRED FROM TRENCHES ACROSS THE TOE JAM HILL FAULT SCARP
Journal Article
Published: 01 August 2008
Bulletin of the Seismological Society of America (2008) 98 (4): 1681-1695.
... in a trench at Vasa Park. The Newcastle Hills anticline, a broad anticline forming the north part of the Seattle uplift east of Lake Washington, is interpreted to lie between the main blind strand of the Seattle fault and a backthrust. Our profiles, on the northern limb of this anticline, consistently image...
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Journal Article
Journal: GSA Bulletin
Published: 01 November 2008
GSA Bulletin (2008) 120 (11-12): 1581-1597.
... end of Bainbridge Island (cross section located on Fig. 1 ). Bedding-plane reverse faults observed in trench excavations (TJ—Toe Jam Hill fault, IW—Islandwood fault) are depicted. Subsurface dips of faults and bedding are reflectors on seismic line PS-2 (ten Brink et al., 2002 ). (B) Seismic Hazards...
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Series: GSA Special Papers
Published: 01 January 2005
DOI: 10.1130/2005.2400
... evidence for minor left-lateral strike-slip faulting subparallel to the upturned bedding that was concurrent with igneous activity at 4–3 Ma. These relationships, combined with consideration of the mechanical properties of the crust and lithospheric mantle, are the basis for the construction of a series...
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Journal Article
Journal: Lithosphere
Published: 01 August 2015
Lithosphere (2015) 7 (4): 379-407.
...-to-the-hinterland transport, normal faulting, and erosion. We conclude that large, long-duration UHP terranes are fundamentally different from transient smaller ones. The latter are often explained by the paradigm of buoyant exhumation. This paradigm is incomplete, but both types can be explained by control...
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Journal Article
Journal: Geology
Published: 01 July 2006
Geology (2006) 34 (7): 585-588.
... with antithetic faults is required to fit the uplift shape. Two classes of fault geometries are investigated here, a reverse fault with a secondary antithetic thrust (the wedge model), and a roof thrust. The surface location of the modeled faults follows the Toe Jam Hill fault ( Fig. 1A ), identified in Lidar...
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Maps of <b>fault</b> scarps and sites with evidence of surface deformation in (A) ...
in > Geosphere
Published: 01 August 2014
of major faults at depth (light red lines) are from Figure 1C . Green letter A locates the intersection of the Toe Jam Hill fault scarp with marine terraces on the west coast of Bainbridge Island. Green letter B locates a strand of the Seattle fault south of Alki Point. The pronounced north-to-northeast
Journal Article
Journal: Geosphere
Published: 01 December 2015
Geosphere (2015) 11 (6): 1948-1974.
... scarps ( Fig. 4 ; Haugerud et al., 2003 ; Nelson et al., 2003a , 2003b , 2014 ; Kelsey et al., 2008 ; Sherrod and Gomberg, 2014 ). The mapped backthrusts are the IslandWood (“Macs Pond fault” in Haugerud, 2005 ), Toe Jam Hill/Point Glover, Waterman Point, and West Seattle. There also is evidence...
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Journal Article
Journal: GSA Bulletin
Published: 01 February 2002
GSA Bulletin (2002) 114 (2): 169-177.
... and east of Puget Sound. This relatively simple thrust-fault model is complicated by the recent discovery of an east-striking scarp on Bainbridge Island ( Bucknam et al., 1999 ), referred to as the Toe Jam Hill scarp. Contrary to the long-term history on the Seattle fault zone, the topographic...
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Journal Article
Journal: Geology
Published: 01 January 2004
Geology (2004) 32 (1): 9-12.
.... , Sherrod , B.L. , Bradley , L.-A. , Koehler , R.D.I. , Bucknam , R.C. , Haugerud , R. , and Laprade , W.T. , 2002 , Field and laboratory data from an earthquake history study of the Toe Jam Hill fault, Bainbridge Island, Washington : U.S. Geological Survey Open-File Report 02-0060...
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Journal Article
Journal: GSA Bulletin
Published: 01 November 2013
GSA Bulletin (2013) 125 (11-12): 1671-1702.
... an excellent physical explanation of the relationship of the wedge geometry and dips of failure planes (faults) within the wedge to the internal state of stress in the ideal “critical” case. These relationships have been widely used to analyze the primary characteristics of natural wedges and appear to give...
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Journal Article
Journal: AAPG Bulletin
Published: 01 May 1998
AAPG Bulletin (1998) 82 (5): 792-816.
... JA90–23, together with line-drawing interpretation, showing a stacked reef complex (dark shading) in the sequence 6B escarpment zone. Note the strong impedance contrast between the reef upper surfaces and surrounding sediments. The small fault is probably related to differential compaction...
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Series: GSA Field Guides
Published: 01 January 2017
DOI: 10.1130/2017.0049(01)
EISBN: 9780813756493
..., deepens to SW. North of 900 A.D. uplift, marine lowstand shoreline at depth of ~54 m MLLW. (B) Restoration Point, SE corner of Bainbridge Island, deepens to E. Within 900 A.D. uplift, marine lowstand shoreline at depth ~46.5 m MLLW. Note eastern end of Toe Jam Hill fault at upper left, interpolation...
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Schematic interpretation of proposed Seattle <b>fault</b> zone structural geometry...
Published: 01 November 2008
Jam Hill fault; IWf—Islandwood fault.
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Mapped <b>fault</b> strands along the northern and southern flanks of the Seattle ...
Published: 01 August 2004
, Restoration Point; SC, Ship Canal anticline; SI, Sinclair Inlet; SP, Seahurst Park; TJf, Toe Jam Hill fault; TTP, Three Tree Point; VI, Vashon Island; WiP, Winghaven Park; WPf, Waterman Point fault. Study location area shown in inset.
Series: GSA Field Guide
Published: 01 January 2012
DOI: 10.1130/2012.0029(02)
EISBN: 9780813756295
... Ferry Rd. This is down the hill and toward the bridge over the Congaree River. Proceed 0.8 km (0.5 mi) north. Turn left at the first turn after the bridge. This is a sharp turn and the road will loop back down the causeway toward the Congaree River. The total distance is ∼0.6 km (0.5 mi). The total...
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Figure 1. (A) Geologic map of the Puget Lowland region showing location of ...
Published: 01 November 2003
and the location of the Toe Jam Hill fault on southern Bainbridge Island ( Johnson et al., 1999 ; Blakely et al., 2002 ). (C) North-south cross section through Bainbridge Island (cross-section location in B) showing probable structural relationships among the Toe Jam Hill fault and other faults of the Seattle
Journal Article
Published: 01 December 2004
Bulletin of the Seismological Society of America (2004) 94 (6): 2299-2316.
...Samuel Y. Johnson; Alan R. Nelson; Stephen F. Personius; Ray E. Wells; Harvey M. Kelsey; Brian L. Sherrod; Koji Okumura; Rich Koehler, III; Robert C. Witter; Lee-Ann Bradley; David J. Harding Abstract Trenches across the Utsalady Point fault in the northern Puget Lowland of Washington reveal...
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Journal Article
Journal: Geosphere
Published: 01 August 2013
Geosphere (2013) 9 (4): 827-852.
...Brian L. Sherrod; Elizabeth Barnett; Elizabeth Schermer; Harvey M. Kelsey; Jonathan Hughes; Franklin F. Foit, Jr.; Craig S. Weaver; Ralph Haugerud; Tim Hyatt Abstract We use LiDAR imagery to identify two fault scarps on latest Pleistocene glacial outwash deposits along the North Fork Nooksack River...
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