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1-11 OF 11 RESULTS FOR
Ntwetwe Pan
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Image
Outline of the Makgadikgadi Pans in north-central Botswana. The Boteti Rive...
in Factors leading to sub-surface pan silcrete formation in north-central Botswana
> South African Journal of Geology
Published: 01 March 2023
Figure 2. Outline of the Makgadikgadi Pans in north-central Botswana. The Boteti River extends along the western side of Ntwetwe Pan and previously fed into Ntwetwe Pan through a number of older channels. Later the river extended southwards to Lake Xau then northwards into the Pan through
Journal Article
Factors leading to sub-surface pan silcrete formation in north-central Botswana
Journal: South African Journal of Geology
Publisher: Geological Society of South Africa
Published: 01 March 2023
South African Journal of Geology (2023) 126 (1): 93–112.
...Figure 2. Outline of the Makgadikgadi Pans in north-central Botswana. The Boteti River extends along the western side of Ntwetwe Pan and previously fed into Ntwetwe Pan through a number of older channels. Later the river extended southwards to Lake Xau then northwards into the Pan through...
Image
Kalahari sand isopachs straddling the Botswana-Zimbabwe border. These are i...
in Drainage evolution in south-central Africa since the breakup of Gondwana
> South African Journal of Geology
Published: 01 March 2001
Figure 9. Kalahari sand isopachs straddling the Botswana-Zimbabwe border. These are interpreted to reflect a major sub-Kalahari valley with headwaters located to the north-east. Isopachs in the north of Sowa Pan are from Figure 8 . A photo-feature to the north of Ntwetwe Pan has been interpreted
Image
Surface textures in Henry crater, Mars. (A) Fine layering that typifies the...
in Potential aeolian deposition of intra-crater layering: A case study of Henry crater, Mars
> GSA Bulletin
Published: 06 June 2019
) Plan-view aeolian dune strata preserved in evaporitic lake sediments in the Ntwetwe Pan in Botswana. Strata from multiple dunes are preserved with interactions. Paleo migration is toward the west, same as (C). Image centered at 20.69°S, 024.90°E. (F) Exposed aeolian cross strata from interdune areas
Journal Article
Makgadikgadi Pans Complex of Central Botswana
Journal: GSA Bulletin
Publisher: Geological Society of America
Published: 01 February 1979
GSA Bulletin (1979) 90 (2_Part_II): 289–312.
...Thomas A. Baillieul Abstract The Makgadikgadi Pans Complex forms a large and unusual surface feature in the central part of the Republic of Botswana (Figs. 1, 2). The two major pans of the complex, Sua and Ntwetwe, comprise an area in excess of 8,400 km 2 (Fig. 3). The pans occupy a basin...
Image
( A ) Overview of the Makgadikgadi Basin illustrating major landforms and f...
in THE EVOLUTION AND AGES OF MAKGADIKGADI PALAEO-LAKES: CONSILIENT EVIDENCE FROM KALAHARI DRAINAGE EVOLUTION SOUTH-CENTRAL AFRICA
> South African Journal of Geology
Published: 01 September 2012
; Ng = Lake Ngami; Ok = Okavango Fan. Line marked Fig. 8 denotes the approximate location of the sediment profile shown in Figure 8 . ( B ) Detail of the Makgadikgadi Pans Complex, showing the location of major sand ridges and the distribution of documented Stone Age localities. The Ntwetwe and Sowa
Journal Article
Size distribution of Baobabs on Kubu “Island”, Sowa Pan (northern Botswana): an indicator of late-stage evolution of the Makgadikgadi palaeo-lake and climate change?
Journal: South African Journal of Geology
Publisher: Geological Society of South Africa
Published: 01 September 2016
South African Journal of Geology (2016) 119 (3): 535–544.
...-mail: [email protected] e-mail: [email protected] © 2016 September Geological Society of South Africa 2016 Geological Society of South Africa The Makgadikgadi Pans complex of north-central Botswana, dominated by Ntwetwe and Sowa (Sua) Pans ( Figure 1 ), is the desiccated relict...
Journal Article
Drainage evolution in south-central Africa since the breakup of Gondwana
Journal: South African Journal of Geology
Publisher: Geological Society of South Africa
Published: 01 March 2001
South African Journal of Geology (2001) 104 (1): 47–68.
...Figure 9. Kalahari sand isopachs straddling the Botswana-Zimbabwe border. These are interpreted to reflect a major sub-Kalahari valley with headwaters located to the north-east. Isopachs in the north of Sowa Pan are from Figure 8 . A photo-feature to the north of Ntwetwe Pan has been interpreted...
Journal Article
THE EVOLUTION AND AGES OF MAKGADIKGADI PALAEO-LAKES: CONSILIENT EVIDENCE FROM KALAHARI DRAINAGE EVOLUTION SOUTH-CENTRAL AFRICA
Journal: South African Journal of Geology
Publisher: Geological Society of South Africa
Published: 01 September 2012
South African Journal of Geology (2012) 115 (3): 385–413.
...; Ng = Lake Ngami; Ok = Okavango Fan. Line marked Fig. 8 denotes the approximate location of the sediment profile shown in Figure 8 . ( B ) Detail of the Makgadikgadi Pans Complex, showing the location of major sand ridges and the distribution of documented Stone Age localities. The Ntwetwe and Sowa...
Journal Article
Dryland dunes and other dryland environmental archives as proxies for Late Quaternary stratigraphy and environmental and climate change in southern Africa
Journal: South African Journal of Geology
Publisher: Geological Society of South Africa
Published: 01 December 2021
South African Journal of Geology (2021) 124 (4): 927–962.
... , K. and Taylor-Perryman , R.C.A. , 2011 . Erb Tanks: a Middle and Later Stone Age Rockshelter in the Central Namib Desert, Western Namibia . PaleoAnthropology , 2011 , 398 – 421 . McFarlane , M.L. and Long , C. W. , 2015 . Pan floor ‘barchan’ mounds, Ntwetwe Pan...
Journal Article
Potential aeolian deposition of intra-crater layering: A case study of Henry crater, Mars
Journal: GSA Bulletin
Publisher: Geological Society of America
Published: 06 June 2019
GSA Bulletin (2020) 132 (3-4): 608–616.
...) Plan-view aeolian dune strata preserved in evaporitic lake sediments in the Ntwetwe Pan in Botswana. Strata from multiple dunes are preserved with interactions. Paleo migration is toward the west, same as (C). Image centered at 20.69°S, 024.90°E. (F) Exposed aeolian cross strata from interdune areas...