By O. Köhler
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Extra info for A Study of Otjiwarongo District (South West Africa) (Namibia)
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Most of the rocks in the Escalante area are sedimentary. Sedimentary rocks are most commonly composed of fragments (mainly silica) that weathered from surrounding highlands. Geologists call these fragments clastic particles. Volcanic ash is another source of clastic particles. Some sediments, such as limestone and gypsum, are biological or chemical precipitates in seas or lakes. As the clastic particles were swept down from the highlands by wind and water, the environments into which the material was deposited varied.
When camping near isolated potholes, springs, or ponds do not use the water source after dark, because you may scare away wild animals. (2) Use a well-established or totally trashed site. There the damage has already been done. If a site has been lightly used, it is best to find a heavily used site or move to a new site and let the lightly used site recover. (3) Camp on slickrock, sandy benches, or in a dry wash, weather permitting. These are the optimal sites since there are no lasting impacts from camping.
The project would have entailed building two miles of new road. The drilling plan was stopped by environmental groups. In 1995 Viking Exploration, Inc. of Colorado proposed drilling an oil well near upper Middle Moody Canyon within the boundaries of Glen Canyon National Recreation Area. To make this possible, Viking will have to rebuild eight miles of old uranium mining roads that are now closed and construct five new miles of road. This oil well is still a possibility. The 1996 hiking season started with the rhythmic thump-thump-thump of a diesel engine at an oil drilling rig on a state land parcel at the junction of the Hole-in-the-Rock road and the Fortymile Ridge road.
A Study of Otjiwarongo District (South West Africa) (Namibia) by O. Köhler
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