scholarly journals Geotechnical soil characterization of intact Quaternary deposits forming the March 22, 2014 SR-530 (Oso) landslide, Snohomish County, Washington

2015 ◽  
Author(s):  
Michael F. Riemer ◽  
Brian D. Collins ◽  
Thomas C. Badger ◽  
Csilla Toth ◽  
Yat Chun Yu
Keyword(s):  
Soil Characterization ◽  
Quaternary Deposits ◽  
Snohomish County

Soil characterization of Tınaztepe region (İzmir/Turkey) using surface wave methods and nakamura (HVSR) technique

2017 ◽  
Vol 16 (2) ◽  
pp. 447-458 ◽  
Author(s):  
Eren Pamuk ◽  
Özkan Cevdet Özdağ ◽  
Şenol Özyalın ◽  
Mustafa Akgün
Keyword(s):  
Surface Wave ◽  
Soil Characterization ◽  
Wave Methods ◽  
Hvsr Technique

scholarly journals Soil Characterization of the Field where Rice has been Cultivated during Five Years

2021 ◽  
Vol 20 (2) ◽  
pp. 8-13
Author(s):  
Eun-Jin Cha ◽  
◽  
Jin-Kyeong Lee ◽  
Min-Ho Jang ◽  
Min-A Choi ◽  
...  
Keyword(s):  
Soil Characterization

scholarly journals Geomorphological characterization and mapping of Cartagena de Indias and adjacencies

2017 ◽  
pp. 5-15
Author(s):  
Max Furrier ◽  
Germán Vargas Cuervo ◽  
Cristian Camilo Moncada
Keyword(s):  
Point Of View ◽  
Field Observations ◽  
Central Theme ◽  
Quaternary Sediments ◽  
Quaternary Deposits ◽  
Spatial Characteristics ◽  
Cenozoic Tectonics ◽  
Geological Formation ◽  
Cartagena De Indias

This work involves a geomorphological characterization of the topographic chart 23 III D, produced by IGAC, in which were developed thematic mappings and other cartographic products where the relief, both, in its morphology and its morphometric and spatial characteristics were the central theme. From the geomorphological point of view, the area in question is located on the Sinú Belt and the unconsolidated Quaternary sediments. Sinú Belt, which oldest geological formation is dated as Oligocene-Miocene, presents the highest altitudes in the mapped area reaching 146 meters in the Cerro La Popa. The lower levels of the relief in the area are the unconsolidated Quaternary deposits, which altitudes do not go over 20 meters. From mapping surveys, interpretation of orbital images, field observations and the integration of the interpretation obtained, it can be concluded that the Cenozoic tectonics is the most important setting factor in the morphological shape of the area.

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