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Landscape features associated with the passive recovery of Mediterranean sclerophyllous woodlands of central Chile [PDF]

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Fuentes-Castillo, T.   +4 more
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Central Chile Finally Breaks

Science, 2010
It has been known for 10 years that the site of the Maule mega-earthquake of 27 February 2010 was fully locked and ready to break.
Madariaga, Raúl   +3 more
openaire   +1 more source

Seismicity clusters in Central Chile

2021
Seismicity along subduction interfaces is usually dominated by large main-shock-aftershock sequences indicative of a continuum distribution of highly coupled large asperities. In the past decades, however, the increased resolution of seismic catalogues at some subduction zone seems to indicate instead a more complex rheological segmentation of the ...
Valenzuela-Malebrán, Carla   +7 more
openaire   +1 more source

Forest Dynamics in South-Central Chile

Journal of Biogeography, 1981
Forest structure and dynamics are analysed and compared for No thofagus-dominated forests in the Andes and for forests lacking Nothofagus in the Coastal Cordillera of the Province of Valdivia (c. 400S latitude), Chile. At mid-elevation (c. 600-950 m) in the Andes, even-aged Nothofagus stands develop on sites devastated by mass movements and volcanic ...
Thomas T. Veblen   +3 more
openaire   +1 more source

Medicinal plants in Central Chile

Economic Botany, 1983
A list of 131 species with medicinal uses in the province of Talca, VII Maule Region in Central Chile, is given. Sixty-six of these are native and the rest introduced.
openaire   +1 more source

The Mediterranean Environment of Central Chile

2007
The Mediterranean-type environment of South America, broadly defined as the continental area characterized by winter rainfall and summer drought, is confined to a narrow band about 1,000 km long on the western side of the Andes in north-central Chile (Arroyo et al., 1995, 1999).
Juan J. Armesto, Mary T. K. Arroyo
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Gravity Variations in Central Chile

1993
Results corresponding to variations of the vertical component of gravity, associated with the March 3, 1985 earthquake are here reported. These processes frequently involve surface modifications near the rupture zone, which can be detected by means of precise gravimetric measurements. In Central Chile, the area affected by the March 1985 earthquake was
Manuel Araneda, M. Soledad Avendaño
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