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DATING IN NEAR ELLIOT SOUTH AFRICA

The Stormberg Group is one of the four geological groups that comprises the
Karoo Supergroup in South Africa. These estimates are based on means of
geological dating including "The contact of the Molteno and Elliot formations
through the main Karoo Basin, South Africa: a second-order sequence boundary" .
South.


DATING IN NEAR ELLIOT SOUTH AFRICA

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RS9 was sampled from a surface outcrop in a shallow mine pit that occurs about
11 m SW of the projected surface position of the excavation pit in the Dinaledi
Chamber Figure 3d. The sample site occurs along strike of the same fracture
along which the Dinaledi Chamber was formed at depth, and it is therefore
possible that this surface outcrop in the past could have linked to the cave
system below. The flowstone consists of a 12—25 mm thick layer of carbonate
overlying an irregular surface of consolidated mud clast breccia similar to
sediments of Unit 2 in the Dinaledi Chamber.

The grey-white flowstone preserves 1—5 mm scale laminations visible due to
colour variations and the presence of several thin brown marker surfaces. The
laminations are locally recrystallized and overgrown by radiating, elongated
crystals of calcite growing from the base to the top of the flowstone layer.
Additionally, fibrous aragonite needles are widely distributed in sheaf-like
patterns.

Sample RS9 was taken from a 4 mm-thick white horizon, 2 mm above the basal
contact of the flowstone layer Figure 3d. RS10 was sampled from a thin crust of
Flowstone Group 2, about 2 m W of the excavation pit and 0. The flowstone
directly overlies mud clast breccia of Unit 3 and hominin bone fragments. This
flowstone is white to grey in colour and is finely laminated and partly
recrystallized, with recrystallization visible as white, fine, radiating needles
of aragonite growing upward from the basal contact, along an irregular
alteration front into grey-white, laminated calcite near the top of the layer.

RS10 was taken from the laminated bottom 3 mm of the flowstone layer Figure 3e.
RS11 and RS21 represent two samples taken from the top and bottom, respectively,
of the same flowstone unit developed along the floor below an active drip point,
1. This flowstone consists of a basal layer of grey flowstone interpreted as
Flowstone Group 2 overlying Unit 3 sediments, covered by a white flowstone layer
containing small stalagmites interpreted as Flowstone Group 3 Figure 3f.

The sample collected for dating consists of a 20—28 mm thick, finely laminated
flowstone including the two distinct layers described above Figure 3f. The basal
layer RS21; Figure 3f is 3—12 mm thick, and consists of brown-grey calcite
resting on Unit 3 sediment. This layer is strongly recrystallized with radial,
acicular crystals of calcite growing upward from the lower contact, which
locally appears to have replaced an earlier generation of acicular aragonite.

These crystals overgrow mm-scale laminations defined by white to brown colour
variations. RS21 was sampled from the basal-to-central segment of this layer.
The basal layer is overlain by an 8—16 mm thick layer of finely laminated sub-mm
scale white speleothem.

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The basal 2—3 mm of this layer is recrystallized with fine aragonite needles
radiating out from the base. Above that the flowstone consists of fine lamellae
defined by subtle grey to white colour variations. Each lamina is composed of
botryoidal aggregates of acicular aragonite. RS11 was taken from the top 3 mm of
this white flowstone Figure 3f. RS13 and RS18 are two samples taken from the
same stalactite developed along the lip of an erosional remnant of Flowstone 1c
near the entrance into the Dinaledi Chamber Figure 1b.

In this location, Flowstone 1c covers the erosional remains of a mud clast
breccia containing a long bone consistent with the H. The stalactite connects to
part of the speleothem layers that cover the bone. The stalactite preserves
well-developed internal layering, with layers asymmetrically developed around a
core, in which layers thicken towards the outward facing side of the stalactite.

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From core to rim the stalactite reaches a maximum thickness of 53 mm and
includes three separate zones that can be distinguished based on internal
texture, layering, and colour Figure 3g. The innermost zone forms an 8 mm-thick,
finely laminated sub-mm scale core centred on a small mud clast and is
terminated by a thin brown, mud-rich rim. This outermost zone is characterized
by extensive replacement of abundant, older aragonite needles by coarse-grained
calcite, creating a patchy texture. The sample has been affected by
recrystallization resulting in the formation of radiating acicular crystals of
calcite that grow from the core outward.

The white outer layer also shows evidence of further recrystallization, with the
formation of coarse 2—4 mm , equant calcite grains, many with highly irregular
grain boundaries that overgrow the acicular grains. RS18 was sampled from a 3
mm-thick horizon near the base of the central zone.

RS13 was sampled from the outermost part of the outer zone Figure 3g. RS14 was
sampled from an irregularly shaped, cascade-like crust of Flowstone Group 2,
along the side-wall of the main floor drain, between the entry shaft and
excavation pit Figures 1b and 3h. The sample of flowstone crust consists of an
8—11 mm thick layer of cream coloured carbonate displaying mm-scale laminations
and a sugary, recrystallized texture with numerous, fine pore spaces along
laminar surfaces.

RS16 and RS17 are two separate samples from a cascade-like crust of Flowstone
Group 2 that formed within the main floor drain between the entry shaft and
excavation pit Figure 1b. This flowstone developed on top of the dolomite
back-wall of the drain Figure 3h.


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Elliot South Africa - Eastern Cape. Current local time: pm. Monday, The
timezone; City Info. The timezone. Timezone Title: Africa/. Elliot, Province of
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The sample consists of a mostly cream coloured flowstone that is up to 73 mm
thick, with a massive sugary, recrystallized texture, preserving mm-scale
laminations visible due to subtle colour variations. Many of the equant calcite
grains contain remnant aragonite needles, reflecting an earlier phase of
aragonite growth.

Laminations along the basal 3—4 mm of this flowstone are brown in colour,
whereas the top 10—12 mm of this flowstone layer consists of what is possibly a
separate, younger unit of laminated grey-brown carbonate with small pore spaces
developed along some of the laminar surfaces. Sample RS16 was taken from a 3—4
mm-thick layer directly above the basal zone with brown laminations. Sample RS17
was taken from a 4 mm-thick zone at the top of the cream-coloured laminated
flowstone, immediately below the darker coloured top unit Figure 3h.


STORMBERG GROUP

RS19 was taken from a wedge-shaped sample of Flowstone Group 2 that formed along
the lip of a drip pool directly overlying Unit 3 sediments, 1. The flowstone is
cream-coloured and up to 30 mm thick, and overlies a flat sediment surface. It
preserves complex internal layering and a variety of textures Figure 3j.

A basal 2—4 mm-thick layer characterised by fine calcite needles growing at
right angles to layering is overlain by an irregular mass of darker cream
coloured, unstructured calcite with a sugary texture and numerous fine voids.
Towards its top this unstructured mass is interlayered with and covered by
several 1—4 mm-thick lamellae characterised by fine calcite needles growing at
right angles to layering similar to the basal layer, but containing pore spaces.
RS19 was taken from the basal flowstone layer with radiating calcite crystals
Figure 3j.

The flowstone forms a cascade-like drape that directly overlies orange mudstone
of sub-unit 1a from which sample OSL5 was taken Figure 3k. RS20 occurs directly
above sample RS10, which was taken at the foot of the cascade Figure 1b.


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The sampled flowstone layer is irregular in shape as it covers sediments with
topography. RS20 was sampled from the basal layer of the sample Figure 3k. This
flowstone overlies erosional remnants of well-indurated mud clast breccia
assigned to Unit 2 Figure 3l , and mostly consists of coarsely recrystallized
white carbonate. The flowstone sample from which RS22 and RS23 were taken occurs
down dip from the palaeo-magnetic sample taken from Flowstone 1a as described
below Figures 2b and The basal layer corresponds to phase B carbonate described
for the palaeo-magnetic sample, and is overlain by a clean white calcite unit i.

Small voids occur in the interstitial spaces between the coarse calcite grains.
RS23 was taken from the grey basal unit i. In this sample, flowstone belonging
to the older phase A carbonate is no longer present, as this layer pinches out
along dip between the point where the palaeomagnetic sample was taken and the
point where the U-Pb sample was taken as can be seen in Figures 2b and Three H.
Sample full catalogue number U. This tooth is deeply weathered, and preserved
only a small rim of enamel on the buccal margin with a maximum height of 4.

Otherwise the crown is a concave dentine surface worn to the cervix, with bright
white, highly bleached dentine. The tooth is brittle and appears strongly
affected by water action. This tooth is partly broken at the root, but has an
otherwise well preserved crown with thick, light-grey enamel. The distal root of
the tooth is present and complete, but the lingual root is broken off just below
the cervix. The tooth is morphologically consistent as an antimere of U. The
dentine is highly bleached and brittle and appears affected by water action.

This tooth is well-preserved with thick, light-blue-grey enamel, and shows
little evidence of bleaching or weathering, with only a very slight polishing
wear on the distal crest of the protoconid. The morphology of the crown is
similar to other lower third premolars in the collection, however, it is
slightly shorter than many of those. This is a complete enamel crown of an
unerupted tooth with no wear facets or interproximal facets in evidence, and the
roots had not formed Figure 7.

The specimen was recovered from a sediment sample taken at a depth of 55—60 cm
below the original ground surface of the cave floor near the base of the sondage
dug in the centre of the excavation pit Figures 1b , 2d and 4. These sandy
intercalations were targeted because they contain fine-grained quartz and
feldspar grains that can be extracted for analysis. For each sample a 30 cm
length of aluminium piping with a diameter of 5 cm was hammered into the
sediments in a horizontal direction or parallel to sedimentary laminations
visible within the units.

A core sample within the pipe was extracted for OSL analyses together with a
sediment sample from the same unit to determine background radiation from
measured values of U, Th and K. Sample OSL4 is obtained from sub-unit 1b
directly below a thin, partly resorbed flowstone sheet attributed to Flowstone
Group 1 Figure 3a. The Unit 1 sediments in this location are partly covered by
Unit 3 sediments and a cascade of Flowstone Group 2 Figure 3k. The speleothem
sampled for palaeomagnetic analysis comes from Flowstone 1a near the entry zone
into the Dinaledi Chamber Figure 2b.

The sample is layered and comprises three distinct phases from base to top: A-C
separated by thin clastic horizons that mark disconformities Figure 13a,b. The
lower phase phase A is interstratified with visible clastic laminations. The
internal laminations are truncated along the lower surface of the sample
indicating that phase A flowstone was partly dissolved during a phreatic event
after the flowstone had been deposited. The middle phase phase B consists of
intercalated flowstone speleothem and detrital sediment layers, with the
detrital layering concentrated towards the downslope part of the sample.

Detrital material is generally less than in phase A, indicating decreasing
amounts of clastic contamination. Like phase A, the internal layering of phase B
is truncated along the lower surface of the sample, indicating that the phreatic
dissolution event occurred after deposition of phase B. There is no apparent
truncation surface between phase A and B flowstone, indicating that phase B
formed on top of phase A after a period of non-deposition during which detrital
material accumulated on top of phase A.

The upper surface of phase B truncates internal layering reflecting dissolution
during a phreatic event. This was followed by a period of non-deposition of
flowstone during which a thin layer of detrital clastic material accumulated,
before deposition of the upper layer phase C of flowstone occurred.

Phase C comprises younger, cleaner flowstone which displays extensive
recrystallization along the base of the unit with the formation of elongated
calcite crystals. This zone of recrystallization could potentially also indicate
a younger infill of a cavity that had formed between phase B and C flowstone,
and has been avoided during sampling. Phase C flowstone contains little to no
detrital inclusions, and suggests that sediment influx into the chamber was not
occurring during its deposition.

The inclination was accounted for by marking the sample on a completely flat
surface of the block. All samples were collected from the surface of Unit 3 as
isolated fragments near the excavation pit. Cave carbonates are proven archives
of sediment chronology and terrestrial climate variation e.




DATING TIMES IN LINDLEY SOUTH AFRICA

Contents:
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results, photos, dates & archives – In the Bunch All Public Member Trees results
for John J Lindley Lindley, NY Weather Rent a car for your Lindley stay


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The camp was divided into two parts, with people from the Lindley district on
the south side of the Valsch River and the remaining 1, on the north side.
Flooding cut off the Lindley people completely, making it impossible to feed
them. He was not surprised that the families did not want to move, for they had
put in hard floor, and built themselves kitchens and ovens.

Breaking up their homes would only cause unhappiness. But the situation was
impossible and the Lindley people were transferred across the river. On this
occasion Webb objected, for it seemed unfair to uproot the families yet again.
None of the camp authorities liked this, for it made management extremely
difficult but it was some time before everyone could be taken into the camp.
Webb was also responsible for a black camp, which grew up at the same time as
the white camp, for the fate of black and white on the farms was closely tied.

In the early months they were little supervised and, apparently, not rationed,
since they possessed some grain and livestock. Superintendent Webb, however,
dismissed the claims of exceptional ill health. He had personally inspected, the
camp, he declared, and was convinced that the statements were untrue.


FILE:SADF ERA LINDLEY COMMANDO INSIGNIA VER 2.JPG

In May General Knox wired the Deputy Administrator, Major Goold Adams, asking
for the appointment of a superintendent of native refugees immediately, because
of the numbers suffering from sickness and starvation. Gresson was appointed. He
was forced to battle against sickness without a doctor until August , when
someone was finally put in place.

He also found himself at odds with the military authorities, who repeatedly
commandeered the men for labour. Without them he could not complete the huts
which the men had been building for the women and children. The chief
superintendent agreed that enough men should be left to do the basic camp work,
including the digging of graves a comment which surely indicates high mortality.


LINDLEY GRAVEL GRIND | NEWS, RESULTS, PHOTOS, DATES & ARCHIVES – IN THE BUNCH

The Kroonstad camp was closed down and the inmates transferred to Honingspruit
and Serfontein. We have very little information about life in the black camps,
or their relationship with the white camps but, in the case of Kroonstad there
are a few brief glimpses. The Molope family, who had been farming on the
Vereeniging Estates, were in Kroonstad camp.

Hill wrote to the chief superintendent in Bloemfontein to the effect that his
client, D. Botha of Kroonstad, had requested that some black families, then in
the Bloemfontein black camp, be transferred to the Kroonstad camp. The families
concerned had worked for Mr Botha, who had left them to care for his farm and
stock when he had come into Kroonstad for protection against the Boer commandos.
In February , however, the military had sent them to Bloemfontein. The
Bloemfontein superintendent admitted that Manel and Malgas and their families
were in his camp, but Jan had gone to the No 6 Transport Depot, leaving his
family in Bloemfontein, while Adam was working for the South African
Constabulary.


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South Africa Hotels Apartments. The commander of the latter detachment, Colonel
A. Dating times in Lindley South Africa Enter a destination to start searching.
Spragge, meanwhile, ordered one of his men to Kroonstad and hoped for relief.
Analysis confirmed that the water was muddy but not necessarily dangerous but
problems continued for some months despite a considerable investment in pumps
and pipes. Serfontein, Keurskrif vir Kroonstad. Essay preparing for a zulu turn
off translation for dating sites. Seeing the futility of further effort, Spragge
also surrendered. You will find information about additional drivers on your
booking voucher. Superintendent Webb, however, dismissed the claims of
exceptional ill health. Caracal Rooikat. Putnam,

In any case, there was no railway transport for such moves although white camp
inmates were moved at their own cost. From the first Kroonstad lacked
accommodation as Boer families poured in. He was informed by head office that
the tents were expected to house fifteen people each, the same rule as applied
to the troops. Nutrition was also critical and it was months before the camp
authorities admitted that the ration scale, based on military rations and scaled
down for women, children and men who were not performing hard labour, was
inadequate.

In March the camp inmates petitioned the superintendent. Worse still, the very
old and the very young suffered from the monotonous diet, with no vegetables or
rice. They received no candles nor soap and could not keep clean. Only twelve
passes a day were issued so people could not get into town to buy food, clothing
or do business. The superintendent was not inclined to stir himself. He assured
the chief superintendent that he was satisfied that there were no grounds for
complaint.

The meat contractor added extra if the meat was bony and he did not think it
necessary to vary the scale of rations. Concessions would only give rise to
further demands. Although he was unsympathetic, Webb was not responsible for the
passes, which was the province of the military and, over time, he came to agree
that the lack of passes, reduced to only six a day by June , caused considerable
hardship.


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The length of stay in Kroonstad camp also took its toll. By August the MO was
reporting cases of scurvy and it was decided to issue lime juice to inmates who
had been in the camp for more than six months.


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She was desperate enough to bypass the superintendent and go directly to the
magistrate for help. At the ending of the Second World War there was a large
surplus of Douglas Dakota twin engine aircraft that were sold off at bargain
prices, this effectively kick started the modern airline industry. The following
article on the history of the Port Elizabeth Railway Station was originally
published in the October edition of Restorica, the journal of the Simon van der
Stel Foundation today the Heritage Association of South Africa.

Thank you to the University of Pretoria copyright holders for giving us
permission to publish. Railway enthusiast Richard Eades posted a wonderful reply
which has been reproduced below. The railway line that connects South Africa to
Namibia is now years old and owes its origin to the outbreak of the First World
War in August Skip to main content. Get driving directions. Yes, the driving
distance between Vereeniging to Lindley is km.

It takes approximately 2h 24m to drive from Vereeniging to Lindley. There is no
direct connection from Vereeniging to Lindley. However, you can take the bus to
Kroonstad then take the taxi to Lindley. Alternatively, you can take the taxi to
Lindley. Rome2rio's Travel Guide series provide vital information for the global
traveller.

Read our range of informative guides on popular transport routes and companies -
including Travelling around the UAE , Which London airport should I choose?
Learn More. How to get from Vereeniging to Lindley by bus, taxi or car.


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