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Eustatic bench of islands of north Pacific

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Journal Article
Journal: GSA Bulletin
Published: 30 September 1925
GSA Bulletin (1925) 36 (3): 521–544.
... of the volcanic islands of the Hawaiian chain, without exception. Every island in the chain shows it. One or the other of us has observed the bench on La Perouse Rock at French Frigates Shoal, Necker Island, Nihoa Island, Kaula Island, Kauai, Oahu, Molokai, Lanai, Maui, Kahoolawe, and Hawaii. Study of photographs...
Journal Article
Journal: GSA Bulletin
Published: 01 June 1941
GSA Bulletin (1941) 52 (6): 773–780.
...HAROLD T. STEARNS Abstract Confusion exists in the literature about the three low benches on Pacific Islands, because height alone is not an index of the ocean level which made them. The lowest bench is now being made by erosion and weathering. The other two were made when the sea stood about 5...
Journal Article
Published: 01 December 1972
Bulletin of the Seismological Society of America (1972) 62 (6): 1365–1375.
.... (1969). Archeological evidence for eustatic change of sea level and earth movements in the western Mediterranean during the last 2,000 years, Geol. Soc. Am. Spec. Paper 109. Heusser, C. J. (1960). Late Pleistocene environments of North Pacific North America--an elaboration of late-glacial...
Journal Article
Journal: GSA Bulletin
Published: 01 July 2008
GSA Bulletin (2008) 120 (7-8): 1053–1071.
... prior to the modern shoreline), with the postulated LGM paleoshoreline inner edge marked by the bolder dashed line (NCI-S1). Note that a slope break corresponding to the LGM paleoshoreline was not found on the north side of the islands, although several prominent, possibly pre-LGM benches are seen...
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Journal Article
Journal: GSA Bulletin
Published: 01 August 2000
GSA Bulletin (2000) 112 (8): 1209–1224.
... hiatus (ca. 10.5 Ma) is closely linked with Pacific plate motion changes, observed in a change in orientation of the Hawaiian island-seamount chain, and rotation of the convergence vector between the Juan de Fuca and North American plates to more normal, leading to increased thrusting and uplift along...
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Journal Article
Published: 01 May 2000
Journal of Sedimentary Research (2000) 70 (3): 478–490.
... raised marshes and subtidal flats, wave-cut benches, abandoned wave-cut scarps with fringing marshes and/or beach ridges, and accretionary islands and recurved spits. Other emergent marine features include abandoned compound flood-tidal delta and washover fan complexes attached to barrier islands...
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Journal Article
Published: 29 August 2023
Canadian Journal of Earth Sciences (2024) 61 (1): 58–85.
... just to the north ( Bornhold 1983 ) began about 13 cal ka BP. There are few modern sediment sources to deliver fine sediments to Milbanke Sound during the Holocene transgression and highstand conditions since ∼7 cal ka BP. The Milbanke Strandflat, spanning southwest Swindle Island through...
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Journal Article
Journal: AAPG Bulletin
Published: 01 August 1994
AAPG Bulletin (1994) 78 (8): 1240–1256.
... are approximately 25 m high in this area. (e) Ashburton River mouth. Note how the river mouth is deflected north of the main channel by longshore drift. Relative sea level is rising due to the slow subsidence of the Canterbury basin and the eustatic rise of about 1 mm/yr ( Gornitz et al., 1982 ). Sea level...
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Journal Article
Published: 20 August 2012
Canadian Journal of Earth Sciences (2012) 49 (9): 1053–1086.
... Bridge, this bench-forming interval is mostly grassed over and exposed only patchily in drainages along the base of the section through to Dry Island Buffalo Jump Provincial Park (S28-T34-R21W4). From Morrin Bridge south, this stacked succession comprises estuarine to shallow-marine sandstones...
FIGURES
Series: Geological Society, London, Special Publications
Published: 01 January 2018
DOI: 10.1144/SP466.2
EISBN: 9781786203786
... to lower right and jointing is high-angle upper right to lower left, but the cave entrances are on a horizontal plane. ( c ) Cave entrances in uplifted Plio-Pleistocene reef carbonates, Tinian Island (telephone pole with transformer in left foreground for scale). Fig. 3. Glacio-eustatic sea-level...
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Journal Article
Published: 01 February 2001
Canadian Journal of Earth Sciences (2001) 38 (2): 309–331.
... Cretaceous to Pleistocene sequence stratigraphy of the Beaufort–Mackenzie and Banks Island areas, northwest Canada . Geological Survey of Canada , Bulletin 407. Dowsett H.J. Poore R.Z. 1991 . Pliocene sea surface temperatures of the North Atlantic Ocean at 3.0 Ma . Quaternary Science...
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Journal Article
Journal: Interpretation
Published: 15 October 2019
Interpretation (2019) 7 (4): SK33–SK43.
... heterogeneous rock, consisting of limestone interbedded with shale and sandstones ( Galley, 1958 ; Oriel et al., 1967 ; Robinson, 1988 ; EIA, 2018 ). The Wolfcamp itself is divided into four different benches, namely, Wolfcamp A, B, C, and D. Most of the production is from the Wolfcamp A and B benches (also...
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Journal Article
Journal: PALAIOS
Published: 01 January 2007
PALAIOS (2007) 22 (1): 3–16.
... Formation south of Cucao, Chiloé Island. Locality CUC is the sandstone blockfall. Height of bluff is approximately 40 m. FIGURE 6 —Coastal exposure of the basal Navidad Formation north of Mostazal, north of locality MOS. Igneous intrusions (not shown) confirm that the numerous discontinuous...
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Journal Article
Journal: AAPG Bulletin
Published: 01 November 1968
AAPG Bulletin (1968) 52 (11): 2208–2230.
... data make possible some interpretations concerning modern dispersal patterns on the bank top. Tidal and wave currents acting against the island and shallow bars cause nearshore sand to move westward on the south of the island and eastward north of the island. Sediment movement is particularly intense...
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Journal Article
Journal: GSA Bulletin
Published: 01 July 2004
GSA Bulletin (2004) 116 (7-8): 840–857.
... by periglacial slope processes, is capable of significant denudation; also, the constraints on limited tectonic uplift of the Transantarctic Mountains in the Pliocene would be removed. In this paper we test and refine the alternative models of landscape evolution in a mountain block adjacent to and north...
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Journal Article
Published: 01 December 1927
Bulletin of the Seismological Society of America (1927) 17 (4): 218–248.
..., April 1926. - - . PALMER, HAROLD S., and WENX'WORTH, CI-IESTER "Eustatic Bench of Islands of the North Pacific." See No. 494 of this list. 469. PARDEE,J. T., "The Montana Earthquake of June 27, 1925," United States Department of the Interior, Geological Survey, Professional Paper No. 147-B, 7-23, 1926...
Journal Article
Published: 01 June 2012
Bulletin of the Seismological Society of America (2012) 102 (3): 1059–1078.
... on the Mad River and Little Salmon fault zones. Clarke (1992) grouped the faults and folds of the offshore CSZ into four zones: a zone of north‐ to northwest‐trending reverse and thrust faults, a zone of broad open folds, a zone of en echelon folds and thrust faults trending oblique to the overall...
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Journal Article
Journal: Lithosphere
Publisher: GSW
Published: 01 April 2012
Lithosphere (2012) 4 (2): 131–149.
... clasts into the Trobriand basin, seismic-reflection data indicate that distributed normal faulting in the Trobriand basin north of the islands had ceased ( Stewart et al., 1986 ; Tjhin, 1976 ), while faulting continued in the Goodenough basin to the south ( Fang, 2000 ). Presently, subsidence continues...
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Journal Article
Journal: GSA Bulletin
Published: 01 January 2004
GSA Bulletin (2004) 116 (1-2): 219–232.
... , Facies geometries within Pleistocene reefs in Barbados : American Association of Petroleum Geologists Bulletin , 54 . 1899 – 1917 . Muhs , D.R. , Simmons , K.R. , Kennedy , G.L. , and Rockwell , T.K. , 2002 , The last interglacial period on the Pacific Coast of North America...
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Journal Article
Journal: GSA Bulletin
Published: 01 March 2007
GSA Bulletin (2007) 119 (3-4): 443–451.
... kinematics of continental Pacific crust, South Island, New Zealand : Journal of Geophysical Research , v. 98 p. 16119 - 16148 . Vandergoes , M.J. , and Fitzsimons , S.J. , 2003 , The last glacial–interglacial transition (LGIT) in south Westland, New Zealand: Paleoecological insight...
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