Results 31 to 40 of about 1,696 (112)
Tephrochronology is the use of primary, characterized tephras or cryptotephras as chronostratigraphic marker beds to connect and synchronize geological, paleoenvironmental, or archaeological sequences or events, or soils/paleosols, and, uniquely, to ...
A Moebis +154 more
core +2 more sources
Abstract The recovery of marine ecosystems in areas heavily impacted by fishing and environmental exploitation depends, to some extent, on the sustainable management of resources and should be complemented by cultural traditions, practices and scientific knowledge.
Ricardo Alvarez +9 more
wiley +1 more source
A Search for the Near‐Surface Particulate Layer Using Venera 13 In Situ Spectroscopic Observations
Abstract Whether or not there is a particulate layer in the lowest 10 km of the Venusian atmosphere is still an open question. Some of the past in situ experiments showed the presence of a detached particulate layer, and a few suggested the existence of finely dispersed aerosols, while other instruments supported the idea of no particulate matter in ...
Shubham V. Kulkarni +3 more
wiley +1 more source
Insights into eruption dynamics from textural analysis: the case of the May, 2008, Chaitén eruption [PDF]
The May, 2008, Chaitén (southern Chile) eruption was characterized by several explosive events, each associated with plumes which reached up to about 19km above sea level on May 6.
Alfano, Fabrizio +2 more
core
The Chiloé Mw 7.6 earthquake of 25 December 2016 in Southern Chile and its relation to the Mw 9.5 1960 Valdivia earthquake [PDF]
On 25 December 2016, a Mw 7.6 earthquake broke a portion of the Southern Chilean subduction zone south of Chiloé Island, located in the central part of the Mw 9.5 1960 Valdivia earthquake.
Carrasco, Sebastian +3 more
core +1 more source
Wood jam mobility in a morphologically active river in northern Chilean Patagonia
This study examined post‐eruption wood jam mobility and channel changes in the Blanco River. Floodplain collapses led to large sediment yields. High wood jam mobility rates were reported. Larger, less compact wood jams persist in stable areas; new and missing jams are smaller and linked to deposition and erosion, respectively.
Lorenzo Martini +4 more
wiley +1 more source
Nueva fuente de obsidiana en la región de la araucanía, centro-sur de Chile: Química y contexto arqueológico de la obsidiana riolítica negra de los Nevados de Sollipulli [PDF]
Un domo de obsidiana negra de composición riolítica aflora entre otras rocas volcánicas en la latitud 38.97716° sur y longitud 71.63528° oeste, en los Nevados de Sollipulli, al oeste del Volcán Sollipulli y al sur del pueblo de Melipeuco en el centro-sur
core +1 more source
Fluvio‐lacustrine response to tephra‐fall events in proximal to mid‐volcanic settings. Characterisation of volcaniclastic remobilisation processes. The differentiation of downstream tephra transportation by floating processes from secondary lahars. Abstract This paper explores the response to Holocene ash inundation in different sub‐environments of two
Nahuel Losano +5 more
wiley +1 more source
Geochemical variations in the Central Southern Volcanic Zone, Chile (38-43°S): The role of fluids in generating arc magmas [PDF]
We present new Sr-Nd-Pb-Hf-O isotope data from the volcanic arc (VA, volcanic front and rear arc) in Chile and the backarc (BA) in Argentina of the Central Southern Volcanic Zone in Chile (CSVZ; 38-43°S).
Amante +107 more
core +1 more source
Abstract The continental crust is produced by the solidification of aluminosilicate‐rich magmas which are sourced from deep below the surface. Migration of the magma depends on the density (ρ) contrast to source rocks and the melt viscosity (η). At the surface, these silica‐rich melts are typically sluggish due to high η > 1,000 Pa s.
Aaron Wolfgang Ashley +2 more
wiley +1 more source

