Paleoenviroment Reconstruction Using Geoarchaeological Methods

Introduction: The reconstructed ancient environment is important as it allows archaeologists to better understand what an anthropological story scenario is to provide and what people can need and what can be met is. This reconstruction is largely due to geographical archaeological methods such as X-ray diffraction, stratigraphy, particle size distribution, microscopic material research, micro morphology, magnetic susceptibility and pollenology (Alam et al., 2008; Balbo et al .

Geological archeology is a study of earth problems related to the human past. Paleoclimate data (such as the previous ice ages) when humans interacted with the environment was classified as geological archeology. It looks at a wide range of dispersed data like pottery and meteor tools, calculates the close relationship between the primitive of technology - ethnography which is their belief, practice, rank, technique, method and society review This rationalization based on human-based qualitative data is then used to provide a possible explanation for historical human records (20, p13) Value (20, p13). It has its limits. That does not necessarily indicate that primitive things of modern technology in the East Indies were doing something in some way, because the ancient Native American did the same for the same reason. But it helped to study several longstanding mysteries in archeology.

Underwater geological archaeological excavations at shallow (about 10 m in depth) of Caesarea in Israel recorded the tsunami that hit the ancient port of Caesarea. The source of the Talmud recorded the tsunami that occurred on December 13 and the attack on Caesarea and Yabuni. The tsunami may have been caused by an earthquake that destroyed Antioch and occurred somewhere in the Cyprus Arc fault system. Researchers at the University of Cambridge recently used carbon fibers to measure corals on the coast of Crete These corals grew 10 meters in the earthquake without water. This shows that the tsunami was caused by a steep fault earthquake in the Greek trench near Crete. Scientists estimate that such a bulge will only occur once in 5000 years, but in other parts of the fault a similar landslide will occur every 800 years.