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Arauco Peninsula

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Journal Article
Published: 01 December 2011
Journal of the Geological Society (2011) 168 (6): 1237–1248.
... bathymetric and seismic reflection data for the Chilean continental margin between 36.5 and 39.0°S to: (1) describe the three giant slope failures offshore Arauco Peninsula; (2) provide age estimates for these slides; (3) compare the size of the three slope failures with other slides reported from active...
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First thumbnail for: Pleistocene giant slope failures offshore <span cl...
Second thumbnail for: Pleistocene giant slope failures offshore <span cl...
Third thumbnail for: Pleistocene giant slope failures offshore <span cl...
Journal Article
Published: 11 March 2020
Seismological Research Letters (2020) 91 (3): 1617–1627.
... Concepción earthquake, applying a Bayesian approach that considers uncertainties in the data. Our results show that the M w 8.1 Concepción earthquake ruptured a deep segment of the megathrust, concentrated in a compact zone below the Arauco peninsula between depths of 20 and 50 km. Tsunami generation from...
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First thumbnail for: The 21 May 1960 M w 8.1 Concepción Earthquake: A D...
Second thumbnail for: The 21 May 1960 M w 8.1 Concepción Earthquake: A D...
Third thumbnail for: The 21 May 1960 M w 8.1 Concepción Earthquake: A D...
Journal Article
Published: 01 June 2012
Earthquake Spectra (2012) 28 (1_suppl1): 39–54.
... and subsidence along about 470 km of the central Chilean coast. In the south, deformation included as much as 3 m of uplift of the Arauco Peninsula, which produced emergent marine platforms and affected harbor infrastructure. In the central part of the deformation zone, north of Constitución, coastal subsidence...
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First thumbnail for: Coseismic Tectonic Surface Deformation during the ...
Second thumbnail for: Coseismic Tectonic Surface Deformation during the ...
Third thumbnail for: Coseismic Tectonic Surface Deformation during the ...
Journal Article
Published: 01 December 1963
Bulletin of the Seismological Society of America (1963) 53 (6): 1315–1330.
... and waterside facilities useless; a large expanse of new beach was exposed. Rio Lebu is no longer navigable because of the uplift. Details of tsunami are reported for several towns on the Arauco Peninsula and south to Tolten. 06 2 1963 Copyright © 1963, by the Seismological Society of America...
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Oblique aerial photograph looking north along the western coastline of the Arauco Peninsula, near the town of Lebu, showing uplifted wave-cut platform and exposed intertidal zone (S37.548111° W73.635672°; 03/09/2010). Tidal stage at time of photograph was about +1.0m above mean sea level.
Published: 01 June 2012
Figure 3. Oblique aerial photograph looking north along the western coastline of the Arauco Peninsula, near the town of Lebu, showing uplifted wave-cut platform and exposed intertidal zone (S37.548111° W73.635672°; 03/09/2010). Tidal stage at time of photograph was about +1.0m above mean sea
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FIGURE 4—The Ranquil Formation at Peninsula Arauco. The bluff (RAN) consists mostly of poorly defined beds of massive sandstones with intermittent beds of glauconitic sandstone. Height of bluff is approximately 20 m
Published: 01 January 2007
FIGURE 4 —The Ranquil Formation at Peninsula Arauco. The bluff (RAN) consists mostly of poorly defined beds of massive sandstones with intermittent beds of glauconitic sandstone. Height of bluff is approximately 20 m
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(a) Map of the Chilean coastline surrounding the 2010 M 8.8 Maule, Chile, earthquake. Slip estimates are based on a joint inversion of tsunami and geodetic data by Lorito et al. (2011). Inverted triangles indicate sites where coseismic vertical displacement was measured by Farias et al. (2010). (b) Estimates of coseismic vertical displacement for the 2010 M 8.8 Maule, Chile, earthquake from Farias et al. (2010), compared to the locations of high‐dynamic stress‐drop subevents (i.e., hatched rectangles) determined by Frankel (2016). Sites located on the Arauco Peninsula extend offshore and may have experienced some contribution from splay faulting (Melnick et al., 2012). Red crosses indicate the estimated coseismic vertical displacement based on dislocation modeling and a uniform 10 m slip model from Farias et al. (2010); semitransparent vertical bars denote sites where the estimated offset does not lie within two units of uncertainty from the measured values. The color version of this figure is available only in the electronic edition.
Published: 29 October 2019
et al. (2010) . (b) Estimates of coseismic vertical displacement for the 2010 M 8.8 Maule, Chile, earthquake from Farias et al. (2010) , compared to the locations of high‐dynamic stress‐drop subevents (i.e., hatched rectangles) determined by Frankel (2016) . Sites located on the Arauco Peninsula
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(a, b) Overview maps of the study area between 32 and 46°S, with seismic profiles used for the calculation of a model of the top of the oceanic basement (TOB). The polygon that was used to limit the volume calculation is indicated as a green outline around the dashed contour lines (light grey in printed version). In addition, some patch areas (yellow polygons, white in printed version) were added to account for the different seaward extension of seismic profiles. The position of the terminal moraine front of the last Quaternary (Llanquihué) glaciation according to Caldenius (1932) is indicated as a thick blue line (black in printed version) in (b). The trench is filled by sediments of turbiditic origin south of 32°S (Thornburg &amp; Kulm 1987). ODP Leg 202 Site 1323 is indicated by a star in (b). Isopachs of the trench fill thickness are given in 500 m contours (dashed black lines). Names and outlines of perennial river systems on land and their corresponding submarine canyon systems are indicated. JFR, Juan Fernandez Ridge; CTJ, Chile Triple Junction. Offshore of the Arauco Peninsula, three giant submarine landslides (NGSF, CGSF, SGSF; northern, central and southern giant slope failures) have significantly modified the continental slope. The evacuation areas are shown as shaded regions.
Published: 24 July 2013
). Names and outlines of perennial river systems on land and their corresponding submarine canyon systems are indicated. JFR, Juan Fernandez Ridge; CTJ, Chile Triple Junction. Offshore of the Arauco Peninsula, three giant submarine landslides (NGSF, CGSF, SGSF; northern, central and southern giant slope
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(A) Regional map of the 2010, Mw 8.8 Maule subduction earthquake rupture area, Chile, approximately outlined by the black oval, showing major faults with known kinematics documented by previous work (Katz, 1971; Thiele and Morel, 1981; Gana et al., 1996; Wall et al., 1996; SERNAGEOMIN, 2003; Melnick et al., 2006, 2009; Geersen et al., 2011). Black and gray dots are all the epicenters of upper-plate earthquakes over the Coastal Cordillera, displayed with their moment magnitude and focal mechanisms for the larger events, from the Global Centroid Moment Tensor (CMT, http://www.globalcmt.org/) catalog for the period between 1 January 1976 and 31 May 2013 (excluding events which depth was fixed and not inverted for). The dates of upper-plate events prior to the Maule earthquake (those shown in gray) are shown. The boxes indicate the locations of the two study regions (Figs. 1B and 1C). VP and AP stand for Valparaíso Peninsula and Arauco Peninsula, respectively. Thick black arrow shows the convergence orientation. The Santa María island referred in the text is located in the gulf between AP and the city of Concepción. (B) Map of the O’Higgins study region showing geologic units and faults as mapped on the 1:1,000,000-scale Chilean geologic map (SERNAGEOMIN, 2003); dots show locations visited in our study. (C) Map of the Maule study region; same features as in B. Simplified geologic units in both of the study areas, from older to younger: Pz4ab, Silurian?–Carboniferous metamorphic rocks; CPg, Carboniferous–Permian intrusive rocks; PzTr4, Paleozoic–Triassic metamorphic rocks; Tr1m, Upper Triassic marine and transitional strata; TrJg, Triassic–Jurassic intrusive rocks; Jig, Lower Jurassic intrusive rocks; J3i, Jurassic volcanic sequences; Ks1m, Upper Cretaceous marine-beach strata; MP1m, upper Miocene–Pliocene marine-beach sedimentary sequences, marine terrace deposits (Navidad Formation); PPl1c, Pliocene–Pleistocene continental sedimentary rocks, river deposits; PPl1m, Pliocene–Pleistocene marine-beach sedimentary sequences, marine terrace deposits; Pl3t, Pleistocene pyroclastic deposits; Q1, Pleistocene–Holocene? marine-beach sedimentary sequences, marine terrace deposits and continental river deposits; Qm, Pleistocene–Holocene? marine-beach sedimentary sequences, marine terrace deposits; Qe, Pleistocene–Holocene eolian dune deposits.
Published: 01 March 2015
). VP and AP stand for Valparaíso Peninsula and Arauco Peninsula, respectively. Thick black arrow shows the convergence orientation. The Santa María island referred in the text is located in the gulf between AP and the city of Concepción. (B) Map of the O’Higgins study region showing geologic units
Journal Article
Journal: GSA Bulletin
Published: 01 March 2015
GSA Bulletin (2015) 127 (3-4): 464–479.
... ). VP and AP stand for Valparaíso Peninsula and Arauco Peninsula, respectively. Thick black arrow shows the convergence orientation. The Santa María island referred in the text is located in the gulf between AP and the city of Concepción. (B) Map of the O’Higgins study region showing geologic units...
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First thumbnail for: Constructing forearc architecture over megathrust ...
Second thumbnail for: Constructing forearc architecture over megathrust ...
Third thumbnail for: Constructing forearc architecture over megathrust ...
Journal Article
Journal: GSA Bulletin
Published: 01 November 2006
GSA Bulletin (2006) 118 (11-12): 1463–1480.
...) and detailed study by Nelson and Manley (1992) reported Holocene uplift rates between 5.5 and 10 m/k.y. at Mocha Island (Fig. 1A) , based on 14 C ages of emerged strandlines. Marine terraces of the Arauco Peninsula and surroundings were described by Kaizuka et al. (1973) as three sequences of uplifted...
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First thumbnail for: Coastal deformation and great subduction earthquak...
Second thumbnail for: Coastal deformation and great subduction earthquak...
Third thumbnail for: Coastal deformation and great subduction earthquak...
Journal Article
Journal: Geology
Published: 01 December 2013
Geology (2013) 41 (12): e309.
.... Bookhagen B. Strecker M.R. Echtler H.P. , 2009 , Segmentation of megathrust rupture zones from fore-arc deformation patterns over hundreds to millions of years, Arauco peninsula, Chile : Journal of Geophysical Research , v. 114 , no. B1 , B01407 , doi:10.1029/2008JB005788 . Melnick...
Journal Article
Published: 01 January 2020
Journal of Paleontology (2020) 94 (1): 56–63.
... Santa María Island, was neither described nor illustrated for comparison. Tavera added that Solemya ? antarctica is also present in the Eocene of Arauco Peninsula (Tavera, 1979 , p. 76). A sample in the Tavera collection at MNHNcl is labelled as Solenomya sp. (SGO.PI.19079) coming from Docas...
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First thumbnail for: Solemyidae (Bivalvia, Protobranchia) from the lowe...
Second thumbnail for: Solemyidae (Bivalvia, Protobranchia) from the lowe...
Third thumbnail for: Solemyidae (Bivalvia, Protobranchia) from the lowe...
Journal Article
Published: 01 November 2005
Journal of Paleontology (2005) 79 (6): 1120–1130.
... of Strombus without any spines or axial sculpture. Hemichenopus araucanus ( Philippi, 1887 ) from the ?Eocene of Peninsula Arauco shows strong affinities to Dicroloma zelandica Marshall, 1919 from the Eocene of New Zealand, which is here assigned to Hemichenopus . The New Zealand species Perissoptera...
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First thumbnail for: CENOZOIC STROMBIDAE, APORRHAIDAE, AND STRUTHIOLARI...
Second thumbnail for: CENOZOIC STROMBIDAE, APORRHAIDAE, AND STRUTHIOLARI...
Third thumbnail for: CENOZOIC STROMBIDAE, APORRHAIDAE, AND STRUTHIOLARI...
Journal Article
Published: 18 November 2014
Bulletin of the Seismological Society of America (2014) 104 (6): 2735–2754.
... seismograms will be computed, and solid triangles indicate the towns and cities where ground motions were measured (see  Data and Resources ). The largest predicted uplifts are in the Arauco Peninsula and reach 1.8 m near LBU, while subsidence reached 1.76 m near the CRC and TLC stations, which is consistent...
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First thumbnail for: Synthetic Hybrid Broadband Seismograms Based on In...
Second thumbnail for: Synthetic Hybrid Broadband Seismograms Based on In...
Third thumbnail for: Synthetic Hybrid Broadband Seismograms Based on In...
Journal Article
Published: 01 June 2012
Earthquake Spectra (2012) 28 (1_suppl1): 75–96.
... partially saturated, which seems to be consistent with the observed conditions and the most likely explanation for the relatively small number of slope failures caused by the earthquake. Nevertheless, significant slope failures occurred on the Arauco Peninsula following a relatively straight line ( Figure...
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First thumbnail for: Seismic Performance of Earth Structures during the...
Second thumbnail for: Seismic Performance of Earth Structures during the...
Third thumbnail for: Seismic Performance of Earth Structures during the...
Journal Article
Published: 01 April 1970
Bulletin of the Seismological Society of America (1970) 60 (2): 669–670.
... damage of its own. Concepci6n is located about 200 km from the presumptive epicenter of the main shock, but is included in the foreshock-aftershock area. Well-documented instances of geodetic displacement occurred about 100 km southwest of ConcepciSn. The city is recessed behind the Arauco Peninsula...
Journal Article
Journal: Geology
Published: 12 June 2023
Geology (2023) 51 (8): 707–712.
...) barrier. The Mejillones, the Topocalma, the Arauco peninsulas (Chile), as well as EW-striking reverse fault scarps in the Coastal Cordillera ( Fig. 4C ), formed by trench-parallel shortening, may bound the earthquake rupture extents ( Allmendinger et al., 2005 ; Melnick et al., 2009 ; Victor et al...
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First thumbnail for: Along-strike seismotectonic segmentation reflectin...
Second thumbnail for: Along-strike seismotectonic segmentation reflectin...
Third thumbnail for: Along-strike seismotectonic segmentation reflectin...
Journal Article
Journal: GSA Bulletin
Published: 01 July 2010
GSA Bulletin (2010) 122 (7-8): 1235–1247.
... sediments (Fig. DR1 1 ) ( Illies, 1967 ; Muñoz et al., 2000 ; Jordan et al., 2001 ). The oldest forearc-related sedimentary units south of the Arauco Peninsula are the Eocene San Pedro and Pupunahue Formations, which are characterized by ∼1000-m-thick sandstones with interbedded conglomerates, shales...
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First thumbnail for: Late Pleistocene landscape evolution in south-cent...
Second thumbnail for: Late Pleistocene landscape evolution in south-cent...
Third thumbnail for: Late Pleistocene landscape evolution in south-cent...
Journal Article
Journal: Geology
Published: 01 March 2012
Geology (2012) 40 (3): 251–254.
... , Segmentation of megathrust rupture zones from fore arc deformation patterns over hundreds to millions of years, Arauco peninsula, Chile : Journal of Geophysical Research , v. 114 , B01407 , doi:10.1029/2008JB005788 . Moore J.C. Saffer D. , 2001 , Updip limit of the seismogenic zone beneath...
FIGURES
First thumbnail for: Splay fault slip during the M w 8.8 2010 Maule Chi...
Second thumbnail for: Splay fault slip during the M w 8.8 2010 Maule Chi...
Third thumbnail for: Splay fault slip during the M w 8.8 2010 Maule Chi...