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Modder River

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Journal Article
Published: 01 July 2013
Journal of Sedimentary Research (2013) 83 (7): 541–561.
... exposures of Cenozoic alluvial successions, which enable assessment of the controls on their genesis, sedimentary architecture, and preservation potential. This paper focuses on the incised Modder River at Erfkroon, Free State, located ∼ 1480 km (river distance) inland from the Atlantic Ocean. At Erfkroon...
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Photographs illustrating the present-day situation of deep channel incision and donga formation in shale bedrock at Erfkroon: A) View downstream, showing that in the central part of the valley, the Modder River has incised up to ∼ 5 m into the shale bedrock below the base of the alluvial succession, which is represented here by the lower sandy gravel facies association (∼ 1-m-thick exposure located below the seated figure). B) The top part of a 4–5-m-high knickpoint developed in the floor of a donga a few hundred meters above its junction with the incised Modder River. Here, the base of the alluvial succession is represented by the upper sandy gravel with bivalves facies association (∼ 2-m-thick exposure located adjacent to the standing figure), and another 2–3-m-tall knickpoint is located farther up the donga.
Published: 01 July 2013
Fig. 9.— Photographs illustrating the present-day situation of deep channel incision and donga formation in shale bedrock at Erfkroon: A) View downstream, showing that in the central part of the valley, the Modder River has incised up to ∼ 5 m into the shale bedrock below the base
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A) Direction of Permo-Carboniferous ice movement in the lower Vaal, lower Riet, and middle Orange river catchments, as reconstructed from striations (after Helgren 1979). In many locations, glacial activity modified existing pre-Karoo river valleys, and the present-day rivers have exhumed sections of these ancient valleys. The eastern margin of the map corresponds with the approximate contact between tillite of the Dwyka Group (to the west) and shales of the Ecca Group (to the east) (see Part C). B) Longitudinal profiles of the Modder, lower Riet, and middle–lower Vaal rivers (reconstructed from contour crossings on 1∶50,000 topographic maps, available from National Geo-Spatial Information, South Africa). Along much of their courses, the rivers flow atop sedimentary rocks of the Karoo Supergroup (e.g., sandstone, shale, tillite), but where the rivers traverse resistant outcrops of Karoo dolerite or Ventersdorp andesite, channel gradients steepen markedly (e.g., below the confluence of the Modder and Riet rivers). Many shorter high-gradient reaches are not visible at this scale. C) Generalized distribution of dolerite and andesite outcrops occurring within approximately 5 km of either bank of the middle Modder River and the Riet River just below the confluence with the Modder (based on 1∶250,000 geological maps, available from Council for Geoscience, South Africa). Numerous smaller dolerite sills and dikes that occur near or at river level are not visible at this scale, including outcrops at the Erfkroon study site and at Waterval farther downstream (Fig. 11B). The numerous dolerite and andesite outcrops on the plains at greater distances from the rivers are not illustrated.
Published: 01 July 2013
exhumed sections of these ancient valleys. The eastern margin of the map corresponds with the approximate contact between tillite of the Dwyka Group (to the west) and shales of the Ecca Group (to the east) (see Part C). B) Longitudinal profiles of the Modder, lower Riet, and middle–lower Vaal rivers
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Photographs illustrating the characteristic features of the overbank deposits at Erfkroon: A) View looking south towards the incised Modder River (in far distance), showing the lower gray paleosol, red paleosol, upper gray paleosol, and the brown paleosol facies associations. The informal color terms serve as convenient descriptors (i.e., weathered surfaces appear “gray,” “red,” or “brown” to the naked eye under ambient light conditions). The lower two figures mark the location of some of the overbank samples collected for luminescence dating (MODD8 and MODD9; see Fig. 4B and Table 3). B) View looking east towards a donga wall, illustrating thinning of the upper gray paleosol towards the northern valley margin (to the left of the photograph) and onlap of the silty sand facies association (the incised present-day Modder River is on the extreme far right of the photograph). C) Example of an erosional contact (dotted line) between a remnant of the paleodonga fill facies association and the red paleosol. Note the contrast between the blocky structure of the paleosol and the weakly developed, low-angle (< 12°) stratification in the paleodonga fill that dips towards the incised present-day channel (located several hundred meters distant on the extreme right of the photograph). D) Example of the displacive development of pedogenic calcrete in the red and brown paleosols close to the northern valley margin.
Published: 01 July 2013
Fig. 7.— Photographs illustrating the characteristic features of the overbank deposits at Erfkroon: A) View looking south towards the incised Modder River (in far distance), showing the lower gray paleosol, red paleosol, upper gray paleosol, and the brown paleosol facies associations
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Oblique aerial photograph with the view oriented approximately south, showing part of the donga complex along the middle Modder River at Erfkroon (see Fig. 4B for the area covered by the photograph). For scale, note the vehicle on the left of the image (circled). Flow direction in the incised present-day channel (arrowed) is from upper left to middle top.
Published: 01 July 2013
Fig. 3.— Oblique aerial photograph with the view oriented approximately south, showing part of the donga complex along the middle Modder River at Erfkroon (see Fig. 4B for the area covered by the photograph). For scale, note the vehicle on the left of the image (circled). Flow direction
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A) The distribution and extent of dongas along part of the middle Modder River as traced from aerial photographs, also showing spot heights and contours in meters above sea level (taken from 1∶50,000 topographic maps, available from National Geo-Spatial Information, South Africa). B) Sketch map highlighting the location of selected sedimentological logs and transects (S1–S6) at Erfkroon (see Fig. 8 for details) and the location of luminescence samples (see Table 3).
Published: 01 July 2013
Fig. 4.— A) The distribution and extent of dongas along part of the middle Modder River as traced from aerial photographs, also showing spot heights and contours in meters above sea level (taken from 1∶50,000 topographic maps, available from National Geo-Spatial Information, South Africa). B
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A) Schematic illustration of the controls on river and floodplain development that occur in a region underlain by resistant dolerite sills and dikes (modified after Tooth et al. 2004). Above intact dolerite barriers, river activity (e.g., lateral migration, aggradation, incision) occurs in response to changes in flow and sediment supply that may be climatically driven (for key stages at Erfkroon, see Fig. 10, Stages 1–8). Once barriers have been breached, local base-level fall results in knickpoint migration, deep channel incision, and donga formation in upstream reaches (see Fig. 10, Stage 9). B) Upstream view of the Modder River at Waterval, located downstream of Erfkroon. This part of the channel has incised ∼ 5 m into a dolerite barrier, which is now marked by a concrete dam wall (just visible behind the reeds and trees). Contact-metamorphosed shale (hornfels, locally known as lydianite) crops out in the near and middle foreground.
Published: 01 July 2013
Fig. 10 , Stage 9). B) Upstream view of the Modder River at Waterval, located downstream of Erfkroon. This part of the channel has incised ∼ 5 m into a dolerite barrier, which is now marked by a concrete dam wall (just visible behind the reeds and trees). Contact-metamorphosed shale (hornfels
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Examples of sedimentological logs selected from six transects (S1–S6) oriented approximately west–east and north–south that illustrate key aspects of the sedimentary architecture at Erfkroon (see Fig. 4B for location of logs and transects). The elevations of the tops of the logs are given relative to a common arbitrary datum (see Fig. 4B), which approximately represents the nearly level floodplain surface prior to the recent incisional phase. The tops of many sections have been eroded, and the elevations thus provide a sense of the erosional topography that has developed. The transects illustrate how older channel deposits lie atop shale or dolerite outcrops (S1, S2, S4), with local exposures at distances several hundred meters from the incised present-day channel (S1, S2, S3, S6). These channel deposits commonly underlie an overbank succession characterized by four paleosols (S2, S6). In some locations, a paleochannel of the Modder River and associated paleodongas eroded the older channel deposits and paleosols, before depositing fills of dominantly silty sand that are several meters thick near to the incised present-day channel (S1, S3) but thin distally (S2, S4, S5).
Published: 01 July 2013
(S2, S6). In some locations, a paleochannel of the Modder River and associated paleodongas eroded the older channel deposits and paleosols, before depositing fills of dominantly silty sand that are several meters thick near to the incised present-day channel (S1, S3) but thin distally (S2, S4, S5).
Journal Article
Published: 01 September 2018
South African Journal of Geology (2018) 121 (3): 327–335.
...’ gravels/sediments along the Vaal River in the Northwest Province ( Marshall, 1990 ; Wilson et al., 2006). The Riverton Formation sediments may be the time equivalents of lithologically similar alluvial successions deposited along the Modder River ( Tooth et al., 2013 ). In the Free State, the Quaternary...
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Journal Article
Published: 01 December 2021
South African Journal of Geology (2021) 124 (4): 963–976.
... to major phases of incision into bedrock that are controlled by the breaching of downstream resistant rock barriers, at sites on the South African Highveld. Alluvial successions and associated palaeosols of the Modder River near Erfkroon, Free State, have provided a rich record of climatic fluctuations...
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First thumbnail for: Characterising the late Quaternary facies stratigr...
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Journal Article
Published: 01 December 2021
South African Journal of Geology (2021) 124 (4): 927–962.
..., although there are not enough dated horizons to get a sense of accumulation rates. At a second Florisian fossil site of Erfkoon (site 71) ( Churchill et al., 2000 ), there is an overbank alluvial-palaeosol sequence associated with the Modder River that contains a three phase record of shifting...
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Journal Article
Published: 01 May 2016
The Journal of Geology (2016) 124 (3): 423–434.
.... S. ; Jacobs , Z. ; and Woodborne , S. M. 2013 . Controls on the genesis, sedimentary architecture, and preservation potential of dryland alluvial successions in stable continental interiors: insights from the incising Modder River, South Africa . J. Sediment. Res. 83 : 541 – 561...
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Journal Article
Published: 01 September 2021
South African Journal of Geology (2021) 124 (3): 783–794.
... may show evidence of secondary (hydrothermal?) leaching of the rock mass with little to no biotite present. The Twakputs Gneiss occurs as a major rock unit in the lower Orange River region of the Northern Cape and in south-eastern Namibia. Good, accessible exposures of the Twakputs Gneiss can...
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Journal Article
Published: 01 December 2021
South African Journal of Geology (2021) 124 (4): 843–862.
..., South Africa, with ages of 65 and 47 ka ( Boardman et al., 2005 ). Luminescence dating of overbank deposits from the Modder River, central South Africa, shows a millennial scale pattern of flood variability from 43 to 19 ka ( Lyons et al., 2014 ). Lunette sand deposition took place between 52 to 46 ka...
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First thumbnail for: A proposed chronostratigraphic framework for the l...
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Journal Article
Published: 01 December 2021
South African Journal of Geology (2021) 124 (4): 863–878.
.... and Woodborne , S. , 2013 . Controls on the genesis, sedimentary architecture, and preservation potential of dryland alluvial successions in stable continental interiors: Insights from the incising Modder River, South Africa . Journal of Sedimentary Research , 83 , 541 – 561 . Verleysdonk , S...
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Journal Article
Journal: GSA Bulletin
Published: 14 May 2018
GSA Bulletin (2018) 130 (11-12): 1825–1841.
..., and preservation potential of dryland alluvial successions in stable continental interiors: Insights from the incising Modder River, South Africa : Journal of Sedimentary Research , v. 83 , p. 541 – 561 , https://doi.org/10.2110/jsr.2013.46 . Tseng , C.-M. , Lin , C.-W. , Dalla Fontana , G...
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Journal Article
Published: 18 February 2021
Journal of Sedimentary Research (2020) 90 (12): 1770–1801.
..., and preservation potential of dryland alluvial successions in stable continental interiors: insights from the incising Modder River, South Africa : Journal of Sedimentary Research , v. 83 , p. 541 – 561 . Tucker, G.E...
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Journal Article
Published: 01 March 2000
South African Journal of Geology (2000) 103 (1): 81–96.
... a continuous normal regression from Ecca to Beaufort times. This diachronous shoreline is associated with deltaic progradation within ahighstand systems tract. Sediment deposition was mainly a result of ephemeral flash floods, but perennial rivers also flowed from melting ice-capped highlands...
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First thumbnail for: Sequence analysis of the Ecca—Beaufort contact in ...
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Journal Article
Published: 01 June 2024
South African Journal of Geology (2024) 127 (2): 271–284.
... Reef Leader, Geldenhuis Deep Mine). Most sand-sized grains are made of detrital pyrite. ( c ) Pyrite-quartz pebble conglomerate (Pyrite Leader Reef, Black Reef Formation, Modder East Mine). Scale bar is in millimetres. Different gold mineralisation models have been proposed over the decades (e.g...
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Journal Article
Journal: SEG Discovery
Published: 01 October 2005
SEG Discovery (2005) (63): 1–52.
... Shield, where recent 1973). Following the Hebgen Lake mary formation. As Woodall (2005) seismicity is rare, where the climate is earthquake of Montana in 1959, three wetter, and where sediments of glacial rivers increased in ow by ~50%, the implies, pathways for uid and energy, increases continuing...