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It is one of the four formations found within the Uitenhage Group of the Algoa Basin – its type locality – and in the neighbouring Gamtoos Basin. The Kirkwood Formation is composed of sedimentary rocks deposited under fluvial conditions at or near sea level, such as variegated mudstone an iconic feature , medium-grained lithic sandstone often being charcoal-rich , and sporadic conglomerates.
At its base, the Kirkwood Formation includes a significant deposit of fine-to-medium grained, poorly-sorted often quartzitic estuarine sandstone with subordinate dark grey to brow shale layers. This deposit was described as the Swartkops Member. The lower portion of the remainder of the Formation is composed predominantly of siltstones, but includes a smaller sandstone layer described as part of the Bethelsdorp Member.
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Thanks to all photographers. Please contact me if your photo is not credited correctly. The best part of the collection, however, are the old trunks and misc. It recreates the station atmosphere very well, and is the sort of museum that the OTM in George should strive to be – so please, if you are ever in the area, support it.
Clive Botha – The old railway station fondly known by locals as the “Doll’s House” Compare with this postcard image dating back about a century ago Elna Conradie photo by David Perl On the previous Thursday I had made a phone call to the main museum in Uitenhage, to confirm that the Station Museum will be open on that particular Monday. I was most positively assured that the Museum will definitely be open. As we drove by, in the street where the main Drosdy Museum is located, I noted that the museum door was closed [Truth was: The door was closed on account of the weather, the Drosdy Museum was actually open for visitors, we should only have checked!
Elna Conradie We arrived at the Station Museum at about What really happened on that morning of 24 Aug , was that the museum staff member who looked after the station museum, had fell ill for 3 working days. As the museum was running with a serious staff shortage another staff member was already hospitalised at the time nobody could be allocated to man the Station museum on these days, but the Acting Head Natania Schmidt advises that in such cases visitors should phone the emergency number displayed on the Museum sign board see below and someone will come and open the museum.
The photo which was captured on e-film by the photographer above! These five joined ten sister engines class 10A supplied in and built on the design of the earlier original CSAR 10th class.
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CONSERVING UITENHAGE. Franco Frescura and Albrecht Herholdt. 11 Cuyler street, dating back to c, an Cape Dutch manor, a number of important and predominantly domestic buildings and a grouping of religious and domestic buildings which play a prominent role in the heritage of the local Islamic community. This node must be considered.
This is the only one of the three museums in Uitenhage which offers a guided tour and because a large section of the Cuyler Manor houses farm animals, my grandchildren liked this museum the best! For the wander round the farm, it is advisable to wear covered shoes flip-flops too flimsy and offer no protection against typical farmyard landmines and we found that we should have taken sun hats as even the autumn sun can do a lot of damage.
The guided tour was conducted by the wonderful, bubbly-natured custodian of the museum, Ouma Rosie, who gave us such an interesting commentary on everything that we saw – she is an amazing curator and story teller and relates well to all age-groups! What was obvious to us is that she is passionate about what she does and she has a wealth of experience which she has amassed over her years of being employed there. The Cuyler Manor Farm Museum would be a wonderful excursion for a primary school visit – but booking for large groups is essential, as then they can prepare for other interesting activities such as breadmaking etc.
Children are encouraged to feed the animals, but taking along some carrots and a cabbage or two might help, as I have a feeling that they are working under severe financial constraints.
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Jul 08, · Uitenhage was founded on 25 April and named after Jacob Abraham Uitenhage De Mist, the Commissioner-General in service of the Dutch government. It is the oldest town in the Eastern Cape and the fifth oldest in the whole of South Africa.
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Most architectural historians are in general agreement with the claim that the built environment is a reliable yardstick of a people’s cultural values and most laymen tend to judge a town by the charm and character of its buildings. We can therefore begin to understand the concern expressed by the Uitenhage Committee at its inaugural meeting in September when they reviewed the long list of historical landmarks which had been lost to future generations through demolitions in the town since , and the quality of the buildings which had replaced them since.
It was felt that, at this current rate of development, few if any buildings of historical merit would be left in Uitenhage by the time it celebrated its bi-centennial in Yet the story of Uitenhage is the story of most small towns on the southern African platteland where the trimmings and symbols of a more gracious and bygone era are being lost daily through neglect, ignorance or a simple desire for change for change’s sake.
Uitenhage is perhaps more fortunate than most in that it still retains much of the charm and atmosphere which made its lifestyle so envied and desired by outsiders some three or four generations ago.
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The scenery along this route is spectacular. Each bend brings more beauty to the table. In winter, there is plenty of snow covering the mountains and landscape. Treat yourself to a visit to the largest cherry farm in Africa. Taste the famous Ionia Cherry Liqueur that has become a landmark. Ionia offers cherry tours in season from October to November.
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Geology[ edit ] The Enon Formation was formed along the southern section of South Africa during the break up of Gondwana when there was widespread erosion of rocks comprising the Cape Fold Belt. Underlying strata are separated by unconformities in most locales expect where the Enon is underlain by deposits of the Cape Fold Belt. The clasts are usually pale or white quartzite , and the most common matrix is a gypsiferous sometimes iron-oxide rich sandy clay.
At some places, clasts of various sizes are intermixed, with large amounts of sandy matrix; at others however, water-sorted clasts of similar size occur in layers, separated by infilled sandstone lenses. Groupings within the formation have occasionally been informally identified, such as the basal Enon Sandstones that occur in the Algoa Basin. Much of the formation tends to comprise smaller clasts in a more iron-rich matrix, giving it a more reddish colour.
The conglomerates consist of large, sub-rounded to rounded clasts of sheared or unsheared quartzite and sometimes slate , shale , and charcoal. Quartzite clasts are generally more rounded whereas the slate and shale clasts are angular. These are interbedded with subordinate sandstone lenses ranging from white, yellow, red and green in colour, claystones , and rare mudstone units. These were deposited in a high-energy alluvial environment where debris flows were common [6/p>