By Professor Dr. Ervan G. Garrison (auth.)

ISBN-10: 3642078575

ISBN-13: 9783642078576

ISBN-10: 366205163X

ISBN-13: 9783662051634

The archaeological geology of the Quaternary or the geological epoch in which humankind developed is a systematic undertaking with a lot to supply within the fields of archaeology and palaeoanthropology. Earth technology suggestions provide varied methods of characterizing the weather of prior landscapes and archaeological facies. This ebook is a survey of options utilized in archaeological geology for the examine of soils, sediments, rocks and minerals. The recommendations awarded characterize these most typically used this day. they're mentioned intimately and examples are supplied, in lots of instances, to illustrate their usefulness to archaeologists.

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These latter types of imaging can aid in landform classification by differing levels and types of vegetative cover, surface hydrology and, using newer types of high-resolution imaging spectrometers, mineralogy and rock types can be examined. Ground level studies include walkover surveys and subsurface studies using both hand and mechanical means. From these images and ground investigations the geomorphic map should describe: (1) morphology (2) landform (3) drainage patterns (4) surficial deposits and (5) tectonic features together with geomorphic/geologic processes active in the mapped area.

Where a clear association of archaeological material with a stratigraphic unit is demonstrated, then the lithofacies mapping of the unit based on pedological/sedimentological features assists in bounding the site for a specific occupational period. This method works very well in shallow «1 m) depth sites that can be quickly sampled with handcoring equipment (see Chap. ). 1 Introduction The objective of this chapter is not to make the reader adept in the theory and application of geophysical techniques used in archaeology today.

Of the sediment reflects stream transport. Another way to visualize a lithofacies map is to think of it as an isopach map without contouring. Sometimes archaeologists will use a variant of the lithofacies map in showing the association of archaeological sites with specific landforms or soils. In the latter case, Fig. 13, from Kuper et al. (1977), shows the association of Bandkeramik (LBK) sites with loessic soils in northwestern Germany, west of the Rhine River valley. The lithofacies map is a qualitative representation of surficial and subsurface strata known from isolated soundings.

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Techniques in Archaeological Geology by Professor Dr. Ervan G. Garrison (auth.)


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