A short excursion into the Small Karoo going through the Kogmanskloof gorge |
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| Geological history Kogmanskloof passes through folded layers of the table mountain sandstone in the Langeberge mountains. Rivers deposited the sediment of which these rock were formed along a coastline some 400 to 450 million years ago. Then about 280 million years ago compression forces in the earth's crust began folding the beds for the next 60 million years. Upon this followed forces which formed large crustal fractures roughly parallel to the present coastline. One of the largest of these, the Worcester Fault passes near the southern entrance to the kloof and displaced beds to the south of it downward by several kilometers. Kogmanskloof is but one of several deep gorges carved through the tough sandstone of the table mountain sandstone by the erosive action of swift flowing rivers for millions of years. |
| It was a lovely winter day on 28 June 2006. This very hot region is
greener in winter than in summer. As on most of our winter trips, the misty weather
was not very good for photos but very much better than the summer heat for walking and
climbing. Rudi loves the climbing. He is geologist so he is used to climb over rocks just
to see what is at the other side of the rock. photos below:- The aloes on the slopes are Aloe comptonii. |
| Rudi is first at the aloes as usual.... or to be honest, he is more often the only one between the two of us who make it to the aloes higher up on the mountains. |
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The very short capitated racemes of Aloe comptonii The leaves ar
broad and short with blunt teeth. . |
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