Article citationsPidwirny, M. (2010) Earthquakes. Fundamentals of Physical Geography. 2nd Edition.fundamentals/10m.htmlhas been cited by the following article:.TITLE:AUTHORS:,KEYWORDS:,JOURNAL NAME:,September18,2014ABSTRACT:The last major earthquake in Bantul causingsevere damage occurred on May 27th, 2006. The damages in the flat area ofBantul had a certain pattern. The damages pattern controlled the subsurfacecharacteristic below the flat area. Beirette vsn.
The book does a good job of covering many geology basics in addition to geography and combined with the This Dynamic Earth could probably serve as the basis for an intro physical geology class. The Fundamentals of Physical Geography (2nd Edition) online textbook describes an area of knowledge within Geography known as Physical Geography. Contour maps. Provide the reader with an idea of the lay of the land b. Are also referred to as 'dot maps' c. Show distribution of any feature on Earth's surface d. Are used to show lines. What are Atmospheric Gases? Atmospheric gases are gases located in the Earth’s atmosphere. These gases primarily include oxygen and nitrogen (making up 99% of the air); though greenhouse gases (carbon dioxide, methane, nitrous oxide, water vapor and ozone) make up 1% of the air.
Understanding earthquake damage patternthrough geo-morphological approach is important for earthquake hazard analysis.The techniques of remote sensing and Geographical Information Systems wereapplied to analyze earthquake damage pattern and geomorphologicalcharacteristics. Gravity analysis was used to identify the subsurface structureand the basement depth while geoelectric analysis was used to identify sedimentdepth. Moreover, spatial correlation analysis was used to identify therelationship between the earthquake damage, geomorphological characteristics,and subsurface characteristics. The results show that fluvial, marine, andaeolian landforms have low rock density value based on gravity analysis. Theseindicate that they were composed by thick unconsolidated material of quaternaryalluvium. While denudational, structural, and solutional landforms composed bymaterial of tertiary rocks have high rock density value.
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The severe damageoccurred in the area that has a lower value of local gravity and deeper basement.In contrast, the slight damage occurred in the area that has higher values oflocal gravity and shallower basement. Moreover, the severe damage occurred inareas of thicker sediment that consist of unconsolidated material.Consequently, the area of unconsolidated material that has deeper basement andthicker sediment is prone to earthquake. They were located on fluvial, marine,and aeolian landforms.