The S.E.5 File (Military Monographs) by Ray Sturtivant, Gordon Page

By Ray Sturtivant, Gordon Page

Heritage of S.E.5 fighter.

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Sample text

The presence of those artifacts is proof that man lived along the river course and used the core tools for animal hunting. The Gunung Sewu environment provided various kinds of rock , and the presence of a particular kind of rock in the environment very muc h influenced the pattern of its exploitation . The process of acquiring raw materia l would not have been difficult if the environment provided it in the form of bou lders or exposed bedrock. If the material formed part of bedrock, it would have to be acquired by mining.

Tectonic movements dUring the Middle Miocene caused the units of rock formed to be uplifted to the surface and slowly the silica group of rocks wos formed (che~, jasper, etc). he Holocene formed the alluvial unit tha~ was deposited In dlsconformity above the limestone of G Sewu. unung Plate 16: White limestone in brittle and kl d .. ~~t~:;:'le. This picture is takc~r:r~mea I~~~~~~o~~~~ss~~~~:~s:eoit~~I~~~~~d~~~ . neOusly. Gradually, uplift towards the south became more Intensive and was of younger date.

The rocks that have disconformities on the normal faults are the tuffaceous rock unit, whereas on the strike slip fault are the limestone rock unit, tuffaceous rock unit and igneous rock unit. On the folds the rock unit that were affected were the tuffaceous rocks. Based on these tectonic movements, the Gunung Sewu region can be distinguished into two areas. East Gunung Sewu forms the region with the most active tectonic movements, evidenced by the presence of faults, folds and other geological structures and supported by the volcanic activities.

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