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Forensic geology is the study of evidence relating to materials found in the Earth used to answer questions raised by the legal system. In 1975, Ray Murray and fellow Rutgers University professor John Tedrow published Forensic Geology. [1] The main use of forensic geology as it is applied today is regarding trace evidence.
Forensic geophysics is an evolving technique that is gaining popularity and prestige in law enforcement. [ 2 ] Searched for objects obviously include clandestine graves of murder victims, but also include unmarked burials in graveyards and cemeteries, weapons used in criminal activities and environmental crime illegally dumping material.
Forensic geology deals with trace evidence in the form of soils, minerals and petroleum. Forensic geomorphology is the study of the ground surface to look for potential location(s) of buried object(s). [82] Forensic geophysics is the application of geophysical techniques such as radar for detecting objects hidden underground [83] or underwater ...
The tectonics processes in Indonesia formed major structures in Indonesia. The most prominent fault in the west of Indonesia is the Semangko Fault or the Great Sumatran Fault, a dextral strike-slip fault along Sumatra Island (about 1,900 km). The formation of this fault zone is related to the subduction zone in the west of Sumatra.
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Geology determines the relative ages of rocks found at a given location; geochemistry (a branch of geology) determines their absolute ages. By combining various petrological, crystallographic, and paleontological tools, geologists are able to chronicle the geological history of the Earth as a whole.
Geophysics is a highly interdisciplinary subject, and geophysicists contribute to every area of the Earth sciences, while some geophysicists conduct research in the planetary sciences.