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Upcoming Events Meet South African Singles Obituaries 2002



Language Testing Centre, Johannesburg Tests are taking place regularly. Durban
1, km.


UPCOMING EVENTS

Good Hope Studies Good Hope Studies provides international clients with an all
encompassing language travel experience of the highest quality, measured against
internationally recognised standards. Our name combines this ancient Nama word
Kurus with English, signifying a bridge to the use of a modern, global language
which, indeed, requires no introduction.

University of the Western Cape The University of the Western Cape is a national
university, alert to its African and international context as it strives to be a
place of quality, a place to grow. It is committed to excellence in teaching,
learning and research, to nurturing the cultural diversity of South Africa, and
to responding in critical and creative ways to the needs of a society in
transition.

International House Cape Town The International House World Organisation IHWO is
a network of language schools worldwide that are committed to implementing high
standards of quality and innovation in education and training. There are
currently over schools in more than 50 countries. GetSmarter GetSmarter's unique
competence is based on our people-driven approach to online learning, coupled
with our ability to offer a full-service, turnkey online education solution for
our valued University partners.

This model has resulted in an average course completion rate of Differential
thermal and thermogravimetric TG analysis done on the same samples presented in
Fig. Individual samples generally responded in one of three ways to
demagnetization Fig. Some samples displayed no to very low remanence during
demagnetization, others were dominated by single magnetic components, while a
third group of samples were easily characterized by between two to a maximum of
four magnetic components.

Five different component directions could be identified in our samples from both
thermal and AF demagnetizations. Representative sample behaviour during
demagnetization for essentially. These samples record high-coercivity components
with random orientation. One cannot that the sample GCED shows a high unblocking
temperature certainly due to the adverse effects of lightning strikes, while the
sample GCED presents a progressive demagnetization from the NRM. The alteration
of ferromagnetic phases during weathering or an initial low content of such
phases would explain this behaviour.

These sites will not be further discussed in this paper. GCED; Fig. The
remanence in such cases can be reasonably linked to lightning induced
magnetizations. Such enigmatic behaviour was also observed by several other
authors in similar age rocks e. Two-component samples are quite common, and this
behaviour is revealed during both thermal and AF demagnetizations.


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Among the six sampled sites located in the Potchefstroom syncline, five
responded well to demagnetization Fig. Site PWD yielded only single, randomly
magnetization vectors Fig. We attribute these to lightening. All but three
samples from the site PWF display the same behaviour. The other samples and
sites yielded two to four magnetic components.

Equal-area plots of remanence components from sites showing lightening induced
remanence PWD. Summary of least-squares component directions and component means
for the Hekpoort Formation. The sites PWD, GCE-A and all the ERA sites either
showing lightening induced magnetization or magnetization linked to none primary
ferromagnetic grains see the text for more explanations are not included here.

They occur over a generally similar, but large range of temperatures and AF
values, and are never present together within the same sample. HKB components
are northeast with positive inclination i.

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In one sample, HKB was the last component removed as a demagnetization
trajectory towards the origin, in all other samples it is present as a
demagnetization trajectory that miss the origin, revealing the presence of a
higher stability component. HKA was readily identifiable as clusters toward the
vertical direction of the upper hemisphere in the majority of samples Fig. Three
samples coming for the highest part of the site PWA show a downward inclination
i. There is some scatter in the direction of the components we designate as HKA,
but we feel justified in their inclusion given a match in lower stability
components among samples.

This area, which includes five sites, yielded the same five groups of components
identified in the PW—sites Fig. Site GCE-A also presents single-component
vectors characteristic of lightening induced remanent magnetization. The other
GCE sites present again low number of single-component vectors 1—3 samples. The
last column represents the same average based this time on the mean component
direction of each site if the component is present in at least one sample of the
site.

We represent either the in situ IS or the tilt corrected TC data according to
the best cluster of vectors we obtained for each component. We choose to let
both types of equal-area plot in the fourth and fifth columns part to allow the
reader to graphically compare the two categories. Twenty-nine samples coming
from all GCE sites present the HKA component, which is again defined by a
northeasterly upward cluster toward the vertical axis Fig.

Two samples present a southwesterly downward component. This suggests a dual
polarity magnetic overprint. Four samples have the HKB components as the highest
stability component, all others also display HKA vectors at higher
demagnetization levels. This area is containing eight sites but several of them
were showing results complicated to interpret or inappropriate to characterized
palaeopoles. First, the majority of the samples from the sites ERA-A and ERA-B
show very low magnetizations making these two sites unsuitable for
palaeomagnetic investigation.

Secondly, most samples of site DK present lightening induced remanence marked by
randomly oriented single-component vectors. Several samples from the four ERA
sites are also showing this behaviour. Much more troublesome, however, is the
observation that the ERA sites are characterized by very scattered results even
after discarding all the samples presenting obvious conflicting issues. Hence,
we decided to discard the results from all the ERA sites. The HKB component was
not identified here.

However, we cannot exclude that they may correspond to two different events as
the samples from site DTH-C present this component as the highest coercivity
vector, and samples from the DTH-B site as the second one after HKA. In summary,
at the first order, the DTH sites have a bimodal behaviour. Note that sites
containing less than four samples for one component, making unreliable the
Fisher's mean values, were discarded for the calculation of the fold test.

We obtained positive results for both tests Fig. However, the fold test improves
the dispersion parameter k , by a factor of 2. Such results suggest that the HKA
component can be considered as a primary magnetization or at least recorded
before any of the main folding deformation events i. The red ellipses represent
the mean of the considered site averages; and the blue ellipses the mean of all
the considered component of magnetization from the whole studied area.

We performed the same tests on the sites and samples showing the HKB component
in order to compare the timing acquisition of this component to the one of the
main folding period, intrusion of the Bushveld Complex or formation of the
Vredefort impact structure. The fold test is not significant as the dispersion
is not really improved during backtilting of the bedding Fig.

For the PW sites, a detailed analysis of the trajectory of unfolding highlights
that the means of these sites move apart during backtilting implying a better
grouping in situ. In addition, the GCE-site means converge to the in situ PW
site means upon restoring beds to palaeohorizontal. As a consequence, the
dispersion of the HKB components is optimized when considering the PW sites
means in situ with the GCE sites means after bedding correction.

The HKD and HKC components are competing overprints, and both are assumed to be
thermoviscous, with HKC possibly being a chemical remanent magnetization, as it
will be explained in this section. Only one sample GCE-B5 records both
components. The HKC component presents an unblocking temperature globally higher
than HKD component, suggesting a relative anteriority of the event responsible
of the HKC components. The HKD components have possibly totally remagnetized the
same range of coercivity of the minerals bearing the HKC component.

The relatively low and consistent range of temperature i. The mean direction for
the HKD magnetization has a declination of The tilt correction of bedding only
results in a small change and does not provide a better cluster, and both
components seem to have been acquired after the tilting of the units. The
geographic i. Occurrence of dykes and sills of the Karoo large igneous province
LIP in the Kaapvaal craton and their overprint on the surrounding rocks are
commonly observed e.

Corresponding palaeomagnetic poles from this study and some selected palaeopoles
from the Kaapvaal craton. The HKC magnetization is characterized by declination
of This location fits with none of the known directions from the Kaapvaal
craton. Two likely hypothesis can explain this magnetization: 1 a thermoviscous
remagnetization or a chemical remanent magnetization related to a metamorphic
related thermal event and 2 a thermoviscous remagnetization linked to an igneous
event. The relatively low unblocking temperature of ca. The Umkondo LIP is
represented by widespread mafic intrusions in the Kalahari craton corresponding
to the gathering of both Kaapvaal and Zimbabwe cratons.

One can argue that no dyke or sill linked to the Karoo and Umkondo LIP or to any
other event was observed in the sampled area. Yet, most of the study area
display poor outcrops except for the most silicified rocks. The less than
perfect match between our poles with the ones of the Karoo and Umkondo LIP can
also be linked to uncertainties in the bedding estimates: it is not compulsory
that lava flows are cooled in a pure planar way whereas we always considered it
as being the case in this work. However, we compared the bedding of lava units
of most sites with those measured in the closest sedimentary layers Fig.

The mean direction for the HKB magnetization has a declination of The
tilt-correction pole position is located at These two events present poles
location relatively similar Fig. Hence, the downward and upward components in
the GCE sites can be explained by polyphased thermoviscous remagnetization due
to the Bushveld Complex during the periods of normal and inverse magnetic
fields. On the other hand, similar thinking cannot be done concerning the PW
sites. The absence of reversal in such suites being linked to the implementation
of either the Bushveld Complex during an epoch showing no reversal or to the
Vredefort impact structure.

Regarding the DTH sites, it is hardly possible to declare with certitude if
either they never contained the HKB components or it was actually recorded until
a later event completely overprinted it. If the HKB components of the PW sites
are related to the Vredefort impact structure, similar results can be expected
concerning the DTH sites, situated at comparable distance to the main Vredefort
impact area Fig. According the bimodal behaviour of the DTH sites i.

The primary component HKA, present in 80 samples, shows, respectively, 69 upward
and 11 downward subvertical components. The mean direction of the HKA
magnetization present a declination of The corresponding tilt-corrected pole
position is located at — The only poles close to the HKA ones are the pole of
the 2. A comparison between the Transvaal and the Griqualand West basins is
represented in Fig. The majority of the age determinations on them matched in
the lower sections of the stratigraphies, but less convincing for the upper
parts of the stratigraphies.

In Fig. Yet, even if those two formations were supposed to be part of the
Transvaal Supergroup e.


OBITUARIES 2002

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The current geochronological database implies that the two basins at least
partly evolved during different periods and not synchronously as suggested by
different works e. He specialised in anaesthetics then practised in Durban in
the sixties. He married Pamela Reardon in and they had two children.

The family returned to England where Akerman studied histopathology, becoming a
Fellow of the Royal College of Pathologists in He published extensively in
conjunction with the Natal Medical School and, at his retirement in , was
department head at both Addington and the Natal Regional Laboratory Services.
Charles John Adkinson Barrat was born in a small village in the Transkei.


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Puhelinnumero Prostituoituja Nivala Check your booking conditions



Pick your preferred language. We speak English and 43 other languages. Check for
travel restrictions. Travel might only be permitted for certain purposes, and
touristic travel in particular may not be allowed. Read more. Due to the
coronavirus COVID , make sure you're booking this property in accordance with
the destination's local government guidelines, including but not limited to the
purpose of travel and maximum group size. Reasonable evidence must be provided
on arrival. If it isn't provided, your booking will be canceled on arrival.

In accordance with government guidelines to minimize transmission of the
coronavirus COVID , this property may request additional documentation from
guests to validate identity, travel itinerary, and other relevant info on dates
where such guidelines exist. In response to the coronavirus COVID , additional
safety and sanitation measures are currently in effect at this property.

Food and beverage services at this property may be limited or unavailable due to
the coronavirus COVID Due to the coronavirus COVID , this property is taking
steps to protect the safety of guests and staff. Certain services and amenities
may be reduced or unavailable as a result. Excellent location — rated 9. Lock in
a great price for A1 Kynaston Accommodation — rated 9.

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Enter dates to get started. Tall palm trees shade the green garden. The
individually decorated units of this three-star property feature the colors of
South-African art. Some include a furnished wooden terrace overlooking the
ocean, or a private patio opening onto the garden. Each room is equipped with a
TV, and some offer satellite channels. Breakfast is available at a surcharge at
A1 Kynaston Accommodations, served daily in the dining room or on the sun deck.
Activities in the area include surfing, as well as whale and dolphin watching.

More information is available from the staff, and tours can be arranged with the
in-house tour guide. An airport shuttle is provided to Port Elizabeth Airport,
just under 50 mi away.

Secure off-street parking is available. Couples in particular like the location
— they rated it 8. A1 Kynaston Accommodation has been welcoming Booking. We're
sorry, but there was an error submitting your comment. Please try again. Good
for couples — they rated the facilities 8. Very Good Coffee!

Get instant confirmation with FREE cancellation at most properties on our site!
Starting April 6, , your chosen cancellation policy will apply, regardless of
the coronavirus. We recommend booking an option with free cancellation in case
your travel plans change. Find more info in the questions and answers. Need
something else? Send your own question to the property below. Welcoming Booking.
You'll receive an email as soon as the property answers your question. You found
this answer helpful.

You found this answer unhelpful. No just room ,breakfast is an extra charge
,please read advert careful it mentions it. Sharon and Paul would love to
welcome you into their home at A1Kynaston.


SOUTH AFRICA

Two Red-necked Phalaropes P. Unusual inland tern records concerned a Greater
Crested Tern T. Book image:. Specials: Roseate, Damara S. In Mpumalanga, an
out-of-range a pair of Yellow Weavers Ploceus subaureus was found near Tonga on
20 August; this is the first record in the province since the mids. Ready To
Move In! Two Red Phalaropes P. Private Apartments. Unavailable: Smoke alarm
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to set up dates while out and. Lucia estuary, from 29 August until at least 9
September.

I love every minute of it. We are situated in a quiet peaceful area of j bay
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all singles ,couples ,families ,tour groups ,large groups ,all very welcome to
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Free taxi services are available to selected restaurants. Love meeting guests.
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Languages spoken: Afrikaans, English , Dutch. Prices you can't beat! WiFi is
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Free public parking is available at a location nearby reservation is not
possible. It looks like something went wrong submitting this. Try again?
Cancellation and prepayment policies vary according to accommodations type.
Please enter the dates of your stay and check what conditions apply to your
preferred room.

To see correct prices and occupancy info, add the number and ages of children in
your group to your search. Additional fees are not calculated automatically in
the total cost and will have to be paid for separately during your stay. The
maximum number of cribs allowed depends on the room you choose. Double-check the
maximum capacity for the room you selected. No age restriction. Cards accepted
at this property. A1 Kynaston Accommodation accepts these cards and reserves the
right to temporarily hold an amount prior to arrival.

Quiet hours. Please inform A1 Kynaston Accommodation of your expected arrival
time in advance. You can use the Special Requests box when booking, or contact
the property directly using the contact details in your confirmation. If you
require an invoice when booking a prepaid rate, write this and your company
details in the Special Requests box. Guests are required to show a photo ID and
credit card upon check-in. Please note that all Special Requests are subject to
availability and additional charges may apply.

Dear visitor, this region is currently experiencing drought conditions. A
Madagascar Olive Bee-eater M. A pair of Crested Barbets Trachyphonus vaillantii
was photographed at a nest c.

A Grey Wagtail Motacilla cinerea, which remained at Debegeni Falls,
Magoebaskloof, Limpopo, from 27 November until late December at least, was
presumed to be the same individual that has returned to this site for the last
few seasons the species was first recorded here on 25 December ; from 8
December, two were present for some time and another was located in the Tugela
River gorge, Royal Natal NP, KwaZulu-Natal, on 1 December.

A Sickle-winged Chat Cercomela sinuata was observed between Velverdiend and
Klerkskraal Dam, North West Province, on 7 August; the distribution of this
species is apparently also moving east.


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Several Collared Sunbirds Hedydipna collaris were present on the edge of
Kruisfontein Indigenous Forest, Western Cape, on 6 July; this is yet another
record west of the traditional western limit of the species' range at Nature's
Valley. In September - December, a southerly influx of Black-headed Canaries
Serinus alario occurred in Western Cape, with flocks of up to 50 birds, mainly
along the west coast, but also further east, around Oudtshoorn and George; both
the black-headed and the more strikingly patterned 'Damara' forms were present.

Records from December - June include the following. A Grey-backed Storm-petrel
Garrodia nereis observed 16 nautical miles south-west of Cape Point on 27
December was only the second record for southern Africa and the African
continent.


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Other noteworthy records made at sea south-west of Cape Town include a Wandering
Albatross Diomedea exulans c. In May, a Grey Petrel P. A pelagic trip c.
Following the influx of African Openbills Anastomus lamelligerus throughout the
country in November - December , birds were being seen during the entire period.
Most records involved singles or small groups, but in Western Cape a flock of 27
was at Elgin on 24 March second largest for the province , whilst 11 were near
Sedgefield on 9 June.

Francis Links Golf Estate on 29 April.

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