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Bainbridge Island

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Journal Article
Journal: GSA Bulletin
Published: 01 November 2003
GSA Bulletin (2003) 115 (11): 1388–1403.
... and Berghoff, 2000 ; Haugerud et al., 2003 ). Our study of five trenches on Bainbridge Island, dug across the first laser-revealed fault scarp in the lowland ( Figs. 1 and 2 ), is the second trench study on young scarps in western Washington (following the pioneering work of Wilson et al., 1979...
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Journal Article
Published: 08 August 2024
The Seismic Record (2024) 4 (3): 184–193.
... and the entire urban corridor that may be analogous to those on Bainbridge Island west of Puget Sound. * Corresponding author: [email protected] 15 November 2023 © 2024 The Author(s). Published by Seismological Society of America. 2024 The Seismic Record This is an open-access article...
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Figure 1. (A) Geologic map of the Puget Lowland region showing location of ...
Published: 01 November 2003
Figure 1. (A) Geologic map of the Puget Lowland region showing location of Bainbridge Island and selected regional crustal fault zones (dashed lines; after Bourgeois and Johnson, 2001 ). (B) Map showing principal reverse faults and tear faults of the Seattle fault zone in central Puget Sound
Journal Article
Journal: GSA Bulletin
Published: 01 February 2002
GSA Bulletin (2002) 114 (2): 169–177.
... is especially clear over Bainbridge Island west of Seattle and over the region east of Lake Washington. Although attenuated in the intervening region, the pattern can be correlated with the mapped strike of beds following a northwest-striking anticline beneath Seattle. The aeromagnetic and geologic data define...
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Journal Article
Published: 01 March 1977
Journal of Sedimentary Research (1977) 47 (1): 78–88.
...H. McLean Abstract Along the south shore of Bainbridge Island and north shore of the Kitsap Peninsula, Wash., the Blakeley Formation of Weaver (1912), consists of approximately 2,400 m of volcaniclastic sandstone, conglomerate, mudstone, and shale that is interpreted to be part of an ancient...
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Figure 5. Magnetic model of the Seattle fault zone. (A) Calculated and obse...
Published: 01 February 2002
Figure 5. Magnetic model of the Seattle fault zone. (A) Calculated and observed magnetic profiles. See Figure 2A for profile location. Profile extends north-south along the east shore of Bainbridge Island (see Fig. 4 for location). A, B, and C indicate anomalies discussed in text. (B) Magnetic
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Figure 2. Airborne laser swath mapping (ALSM) digital elevation model of th...
Published: 01 November 2003
Figure 2. Airborne laser swath mapping (ALSM) digital elevation model of the southernmost part of Bainbridge Island, Washington (location in Fig. 1B ; model grid cells are 3.7 m square). The south-facing scarp of the Toe Jam Hill fault trends east-west across the island ∼200–500 m south of Blakely
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(A) Map of Seattle fault zone modified from  Blakely et al. (2002) . (B) Li...
Published: 01 November 2008
Figure 1. (A) Map of Seattle fault zone modified from Blakely et al. (2002) . (B) Light detection and ranging (LiDAR) image of southern Bainbridge Island and Waterman Point-Point Glover Peninsula, showing the trace of the Toe Jam Hill, Islandwood, Waterman Point and Point Glover faults
Series: Geological Society, London, Special Publications
Published: 01 January 2007
DOI: 10.1144/GSL.SP.2007.273.01.07
EISBN: 9781862395213
...). The fourth story comes from the Suquamish Tribe on the western side of Puget Sound ( Fig. 5 b: 7; Fig. 1 :16). Oral traditions handed down by elders tell of the creation of Agate Passage (the waterway between the northern end of Bainbridge Island and the Kitsap Peninsula; located on the down-thrown side...
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Journal Article
Journal: Geology
Published: 01 December 1996
Geology (1996) 24 (12): 1123–1126.
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Terrace heights projected onto a north–south transect across the Seattle fa...
Published: 01 June 2012
stratigraphy are projected onto the transect. ten Brink et al. (2006) estimate error in their terrace data to be ±1  m. Ota et al. (2006) estimate the error on terrace heights to be at least the ±30  cm error of the LiDAR data used to measure terrace heights. The highest terrace heights on Bainbridge
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(A) Light detection and ranging (LiDAR) image of a portion of southern Bain...
Published: 01 November 2008
Figure 4. (A) Light detection and ranging (LiDAR) image of a portion of southern Bainbridge Island peninsula (map location on Fig. 1B ) showing the scarp of the Toe Jam Hill fault, location of trenches across the fault scarp, and locations of coastal transects depicted at west end of fault trace
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Colocated chirp and MCS profiles at the west end of Rich Passage. (a) Map o...
Published: 19 August 2022
, Restoration Point. Tb dips 45°–60° north on the Kitsap peninsula between Orchard Point and Point Glover and dips 80°–90° north at Restoration Point and AP; Tbh is dipping 70°–90° north on Bainbridge Island. (b) Chirp image. (c) Colocated MCS profile. The approximate dip values of the north‐dipping beds
Journal Article
Journal: GSA Bulletin
Published: 01 November 2008
GSA Bulletin (2008) 120 (11-12): 1581–1597.
...Figure 1. (A) Map of Seattle fault zone modified from Blakely et al. (2002) . (B) Light detection and ranging (LiDAR) image of southern Bainbridge Island and Waterman Point-Point Glover Peninsula, showing the trace of the Toe Jam Hill, Islandwood, Waterman Point and Point Glover faults...
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Maps of fault scarps and sites with evidence of surface deformation in (A) ...
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
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(A) Cross section showing observed dips of bedding on south end of Bainbrid...
Published: 01 November 2008
Figure 2. (A) Cross section showing observed dips of bedding on south 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
Journal Article
Published: 01 April 1935
Bulletin of the Seismological Society of America (1935) 25 (2): 138–153.
... at Bainbridge Island. C. G. R. (December 6, I V ) ; P. 1880 December 10, 5 a. m.; Bainbridge Island; "vertical shock." U.S.W.R. (Puget Sound, IV) ; P. 1880 December 12, 8:40 p.m.; severe shock near Puget Sound, from Vic- toria, B.C., to Portland, Ore. C. G. R. V I I ; P. 1880 December 14, 7 p.m.; I I I ; slight...
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Mapped fault strands along the northern and southern flanks of the Seattle ...
Published: 01 August 2004
circles with numbers indicating depth to Tertiary sedimentary rocks. Shaded areas west of Puget Sound show outcrops of Eocene volcanic rocks; shaded areas east of Puget Sound show outcrops of Tertiary sedimentary rocks ( Yount and Gower, 1991 ). Abbreviations: AP, Alki Point; BI, Bainbridge Island; Bl.I
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Cross sections illustrating structural models of the Seattle fault zone and...
Published: 01 August 2014
on interpretations of north-south seismic reflection profiles east of Bainbridge Island ( Fig. 2A ), whereas model C is for the eastern part of the fault zone near Lake Washington ( Liberty and Pratt, 2008 ). The main thrust of the Tacoma fault is shown only in model B. Cr—Crescent Formation; Q—Quaternary; T
Journal Article
Journal: Geology
Published: 01 July 2006
Geology (2006) 34 (7): 585–588.
... to the north from volcanic rocks of the Seattle uplift to the south ( Johnson et al., 1994 ). Outcrops of basin-fill and sub-basin rocks along the surface projection of the fault on Bainbridge Island are tilted more than 70° ( Fulmer, 1975 ). Surface exposures of the fault are either largely obscured by dense...
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