scholarly journals Analysing explosive volcanic deposits from satellite-based radar backscatter, Volcan de Fuego, 2018

2021 ◽  
Author(s):  
Edna W Dualeh ◽  
Susanna K Ebmeier ◽  
Tim J. Wright ◽  
Fabien Albino ◽  
Ailsa Katharine Naismith ◽  
...  
Author(s):  
E. W. Dualeh ◽  
S. K. Ebmeier ◽  
T. J. Wright ◽  
F. Albino ◽  
A. Naismith ◽  
...  

2013 ◽  
Vol 13 (2) ◽  
Author(s):  
Heru Sri Naryanto

Karanganyar District is a hilly area with steep slopes, rock constituent of young volcanic deposits of Lawu Volcano products, thick soil and relatively high rainfall, so it is potential for large landslides in this region. The landuse in the Karanganyar District including the Tengklik Village is generally dominated by rice fields, seasonal gardens and settlements. Plantation made up in areas with steep topography has great influence on erosion and landslides. Similarly, many settlements are built on a slope so that the area is very vulnerable to the threat of landslides. In the rainy season landslides are common. The potential hazard of landslidesoccurred in 14 sub districts in Karanganyar District. Large landslides have occurred in Karanganyar on December 26, 2007 which claimed the lives of 62 people, with the greatest victims were in the Ledoksari Village, Tawangmangu. The Tengklik Village has already experienced creep type landslides, which have destroyed settlements, roads, seasonalgardens and all existing infrastructure in the area. In order to do the proper handling and anticipation of a catastrophic landslide, a variety of technological applications landslides using geographic information system (GIS) was then carried out, to detect the configuration of 2D geoelectrical subsurface prone areas for landslide risk study and regional planning.


1978 ◽  
Author(s):  
Gerald G. Schaber ◽  
Richard J. Pike ◽  
Graydon Lennis Berlin

1984 ◽  
Author(s):  
Young-Sooxa Kim ◽  
R. K. Moore ◽  
R. G. Onstott

2019 ◽  
Author(s):  
Sverre Planke ◽  
◽  
John M. Millett ◽  
John M. Millett ◽  
John M. Millett ◽  
...  

Elements ◽  
2019 ◽  
Vol 15 (6) ◽  
pp. 405-410 ◽  
Author(s):  
J. Kelly Russell ◽  
R. Stephen J. Sparks ◽  
Janine L. Kavanagh

Kimberlite rocks and deposits are the eruption products of volatile-rich, silica-poor ultrabasic magmas that originate as small-degree mantle melts at depths in excess of 200 km. Many kimberlites are emplaced as subsurface cylindrical-to-conical pipes and associated sills and dykes. Surficial volcanic deposits of kimberlite are rare. Although kimberlite magmas have distinctive chemical and physical properties, their eruption styles, intensities and durations are similar to conventional volcanoes. Rates of magma ascent and transport through the cratonic lithosphere are informed by mantle cargo entrained by kimberlite, by the geometries of kimberlite dykes exposed in diamond mines, and by laboratory-based studies of dyke mechanics. Outstanding questions concern the mechanisms that trigger and control the rates of kimberlite magmatism.


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