Chile in 1941 exported about 1,300 flasks, in 1942 about, 2,300 flasks, and in 1943 at least 2,500 flasks; it exported considerably less in 1944. According to the best information and estimates available, Chile in 1943 held seventh position among nonAxis producers, following Spain, the United States, Mexico, Canada, Kussia, and China, and contributed about percent of the nonAxis ...
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· The Atacama Desert is Chile at its most serrated; Chile without a safety net. Or, at least, that's the theory. When I arrive at the Alto Atacama Desert Lodge Spa, I could barely feel more ...
The most prominent feature in the city is the "Morro," a sheer lava cliff face interbedded with Jurassic limestone, sandstone and shale that is an iconic symbol of Chilean nationalism. Each Sunday morning, some of the city's 180,000 residents hold a parade at the base of the cliff celebrating Chilean victory in the 1883 War of the Pacific between Chile, Peru and Bolivia. .
Chile annexed most of the desert, and cities along the coast developed into international ports, hosting many Chilean workers who migrated there. With the guano and saltpeter booms of the 19th century, the population grew immensely, mostly as a result of immigration from central Chile. In the 20th century, the nitrate industry declined and at the same time, the largely male .
STORMGENERATED SANDSTONE BEDS FROM THE UPPER CRETACEOUS OF SOUTH CHILE AND THEIR REGIONAL SIGNIFICANCE DAVID 10M. MACDONALD British Antarctic Survey, Natural Environment Research Council, High Cross, Madingley Road, Cambridge CB3 OET, Gran Bretaña. ABSTRACT Convolutelaminated sandstone beds with hummocky crossstratifiion are described .
1982. Quiriquina Formation (Chile) The Quiriquina Formation is a geological formation in Chile whose strata date back to the Late Cretaceous. Dinosaur remains are among the fossils that have been recovered from the formation. The glauconitic sandstones and conglomerates of the formation were deposited in a marine environment.
· El Tatio Geysers. The most popular place to visit in the Atacama Desert, outside of San Pedro, is the El Tatio Geysers. Loed a few hours north from San Pedro de Atacama, at an altitude of 4300m, the geysers are constantly shooting jets of water .
gion, Chile (Fig. 1), within a transported block of calcareous sandstone found at an elevation of 243 m The block has approximate dimensions of 80x50x40 cm, and a weight of about 350 kg. The nearest outcrop of calcareous sandstone is in an inaccessible cliff higher up on the slopes of Sierra Dorotea. Field observations allow us to interpret the stratigraphic provenance of the block to ...
The Santa Juana and Puclaro dams in Chile are both founded on deep riverbed alluviums, of 30m and 113m maximum depths, respectively. Santa Juana was commissioned in 1995. The reservoir was filled in 1997 and its performance has been excellent, with total seepage lower than 50 l/s. Puclaro dam, which is due for completion in October 1999, is very similar to Santa Juana. To decrease seepage and ...
The Salar de Atacama basin, the largest bpreAndeanQ basin in Northern Chile, was formed in the early Late Cretaceous as a consequence of the tectonic closure and inversion of the Jurassic–Early Cretaceous Tarapaca´ back arc basin. Inversion led to uplift of the Cordillera de Domeyko (CD), a thickskinned basement range bounded by a system of reverse faults and .
The most prominent feature in the city is the "Morro," a sheer lava cliff face interbedded with Jurassic limestone, sandstone and shale that is an iconic symbol of Chilean nationalism. Each Sunday morning, some of the city's 180,000 residents hold a parade at the base of the cliff celebrating Chilean victory in the 1883 War of the Pacific between Chile, Peru and Bolivia. The Morro not ...
· Abstract Outcrops of the Cretaceous Cerro Toro sandstones within Parque Nacional Torres del Paine (southern Chile) have been described in a submarine channelle
· ABSTRACT Extensive occurrences of Upper Jurassic to Lower Cretaceous aeolian sandstones form part of a thick sequence of terrigenous red beds in northern Chile. These sediments accumulated in a N‐S‐elongated intermontane back‐arc basin on the landward side of an active volcanic chain. This volcanic chain, which was produced by subduction beneath the continental margin, .
Extensive occurrences of Upper Jurassic to Lower Cretaceous aeolian sandstones form part of a thick sequence of terrigenous red beds in northern Chile. These sediments accumulated in .
· ABSTRACT Extensive occurrences of Upper Jurassic to Lower Cretaceous aeolian sandstones form part of a thick sequence of terrigenous red beds in northern Chile. These sediments accumulated in a N‐S‐elongated intermontane back‐arc basin on the landward side of an active volcanic chain. This volcanic chain, which was produced by subduction beneath the .
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