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Termas Hill Landslide

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Figure 7. Schematic of the <span class="search-highlight">Termas</span> <span class="search-highlight">Hill</span> <span class="search-highlight">landslide</span>. (A) Plan view. (B) Block ...
Published: 01 April 2006
Figure 7. Schematic of the Termas Hill landslide. (A) Plan view. (B) Block diagram along dashed line XY in A (regolith in white; Anta Formation in light gray). The subsurface structure in the right half of diagram is speculative. Note the main slip surface cut by a subsequent normal listric fault
Image
Figure 3. Aerial views. (A) View to the south-southeast showing the landsli...
Published: 01 April 2006
Figure 3. Aerial views. (A) View to the south-southeast showing the landslide site on the western flank of Termas Hill. Road 34 follows wind gap. (S  =  Saladillo Creek partly hidden by airplane wing). (B) View east-southeast showing main structural features of the Termas Hill landslide. Note
Journal Article
Published: 01 April 2006
Environmental & Engineering Geoscience (2006) 12 (4): 369–376.
...Figure 7. Schematic of the Termas Hill landslide. (A) Plan view. (B) Block diagram along dashed line XY in A (regolith in white; Anta Formation in light gray). The subsurface structure in the right half of diagram is speculative. Note the main slip surface cut by a subsequent normal listric fault...
FIGURES | View All (7)
Image
Figure 1. Location maps. (A) South America with Argentina outlined and squa...
Published: 01 April 2006
map overlaid on a Thematic Mapper satellite image (white rectangle represents area of landslide; x  =  campsite adjoining large pond; r  =  topographic ridge; f  =  reverse fault affecting Termas Hill landslide; Q  =  Quaternary deposits; A  =  Anta Formation, geology taken from Seggiaro and others
Image
Figure 2. Digital elevation model (DEM) of the <span class="search-highlight">Termas</span> <span class="search-highlight">Hill</span> area and elevati...
Published: 01 April 2006
Figure 2. Digital elevation model (DEM) of the Termas Hill area and elevation profile across the site of the slide, showing the upfaulted rock ledge. This ledge partly protects base-of-slope areas from landslides generated on the western flank of Termas Hill. DEM obtained from Shuttle Radar
Journal Article
Published: 01 December 1963
Bulletin of the Seismological Society of America (1963) 53 (6): 1367–1402.
..., but as the lowland became gradually cleared, farming developed on the flatland and on the lower slopes of the hills. Two large agricultural estates (Culan and Aniques) and five indigenous farm settlements (Reductos Llancatillo, Cafrilat, Antimilla, Lemo- has, and Antiques) were affected by the landslides. Cleared...
Series: Geological Society, London, Geology of Series
Published: 01 January 2007
DOI: 10.1144/GOCH.13
EISBN: 9781862393936
... Cordillera hills. The deeply weathered landscape becomes increasingly desert-like as one approaches Termas de Socos, with the highway roadcuts exposing heterogeneous net-veined and dyked plutonic igneous complexes. At km371 on the Panamericana the Termas de Socos and Ovalle turnoffs lie to the right. Termas...
FIGURES | View All (5)
Journal Article
Published: 01 February 1963
Bulletin of the Seismological Society of America (1963) 53 (2): 225–307.
...), Architectural Institute of Japan, 75:607/616 (1960). 225 Vega de ) Itata 1 3aihueco ., %, o~ . a de los Pinche;ra j ~int~ 30 ~r c ~Termas \, (. it t ' de ChillOn , qolfo de ,.D~o- .op " / v 37 ° -- at~ \ Pta. Lavapie )nio ~ _ '% Laguna i lu6pil Y~ ~:UCO .6~° Pso~i~ ! u . ~, Pta Cam, P e l u I { \ 0 Vn...