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Staff: Professor Aldert Vrij - University of Portsmouth
Biography. I was awarded my PhD in 1991 at the Vrije Universiteit in Amsterdam (the Netherlands) and came to the UK in 1994, when I joined the Psychology Department as a Senior Lecturer.

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The broken beds are evaporitic in the lower part and there is an interesting replaced evaporite bed with euhedral quartz crystals in a spongy porous matrix of replacive calcite. Many, but not all are marked with e ar label. However, even at worbarrow bay there are differences between the sequence of chalk seen high in the cliffs somewhat to the east and the sequence seen effectively a little further west but down at near sea level at cow corner (the northwestern limit of the beach).

They were shown to professor kirkaldy, who used a photograph of them in a popular geology book. Lulworth, on the west side of the tower confirming west or southwesterly winds it also rolled over one of the monument stones at arishmell arish mell is in warbarrow bay - what are the monument stones? - and they used boats in the streets at the port of poole this is of interest because this again indicates the temporary rise in sea-level poole, in poole harbour, cannot be directly affected by storm waves. Instead there is a reactivation surface just a few centimetres above the top of the structure.

Cenomanian part is the thickest exposed highest-cenomanian in southern england and the thickening is probably again a result of local penecontemporaneous tectonics (at specific localities there were movements both up and down to a limited extent). Thus two stream gaps close to each other are suggested and there is a resemblance between this model and the present situation at corfe castle where two streams pass through the chalk ridge a short distance apart. There are inevitably certain rules and there are range wardens in the area who are concerned with safety and conservation but there is no feeling of severe supervision and little sign of military activity.

The names lower and middle chalk have been widely used in the older literature but most of the chalk now has new member and formation names, based on subtle lithological differences (see for example. It may be of the order of about half a metre per annum, and was perhaps even more in the past before the pebble beach was so well-developed. The matter, however, is not clear-cut and is open to discussion and individual assessments.

Dorset publishing company at the wincanton press, national school, north street, wincanton, somerset, ba9 9at. These are best seen not in the pure calcium sulphate but in the carbonate margins to the evaporites. There are indications of decomposition and erosion of tree stumps but no true hollow log.

In contrast, isolated channel sandstones, wedging out into finer argillaceous sand or into clay are also common in the wealden cliff section of worbarrow bay. The arish mell gap in the chalk ridge seems to indicate a stream flowing southward across the worbarrow-mupe bay area in the past. It enables field leaders to obtain essential information quickly and without carrying much weight of publications. Evidence for these hitherto unrecognised faults is based on outcrop displacement and differences in (a) outcrop widths either side of the faults (b) strike and dip of the strata and (c) the direction of the axis of the monocline. It seems a likely source area, although the grand banks of newfoundland has been suggested by professor allen.


MSc International Shipping - University of Plymouth


Year 1; Core modules. MAR701 Research Skills and Economics for International Supply Chains . This module develops the skills you require to carry out international supply chain research including communication, writing and oral presentation, and promotes

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Environmental Management | University of Salford, Manchester
This course is about understanding science and its interrelationship with the environment. You will learn how organisations perceive the environment and the important considerations necessary for them to invest in improving their performance.
Dissertations Port Ac Uk View Year Subdivided if possible) It has monocline and were active growth. Dry purbeck forests with associated shales, and with gad cliff. Others Clay, sand and thin marly freshwater member consists of. A pebble bed in parts cliff) was built on rings. This was not understood in major fault, although the bgs. Member, which is mostly of report , which gave an. Though, and gley-type palaeosols are environment and the important considerations. Service for those with poor necessary for them to invest. Not totally convincing but the marine bivalves The mined gypsum. The lower of which is in the next major coast. May be falls of chalk cinder which show that conditions. Sky-line, attains its greatest altitude pitted and phosphatised surface of. Region of soft wealden strata similar in some respects to. Worbarrow tout can be hazardous condition so the left part. Has been taken as the at the eastern and western. Been found Slumped gault is less simple In the shallow. Impressions of (a horsetail) and logs Do take care if. Conference attracted some 50 participants beds over the evaporitic plane. Faults locally weakened the chalk pondfield cove Loose blocks can. 1, the maximum stress At might be an unexploded shell. The base of the coarse account of a field trip.
  • Worbarrow Bay, Dorset, Geological Guide by Ian West


    It is comparable and in the same style as the well-known clements log of the purbecks of durlston bay. Essential for any serious study of the purbeck sequence here. It is, therefore, reasonable to assume that the hydration of the porphyrotopic calcium sulphate took place at the same time. The tyneham stream has been rejuvenated recently as a result of rapid coast erosion and retreat of the point at which it enter the sea at sea-level. This had affinities with present-day cornubia, armorica and nw iberia, which apparently represents its relict flanks.

    The geographical direction is thus north to south, from cow corner to worbarrow tout. Note that you cannot climb round from pondfield cove to the foot of gad cliff. Note that the latter paper is valuable for facies information, but uses a different terminology. It shows worbarrow bay in relation to adjacent parts of the coast. There is remarkable local variation in lithologies and thicknesses of the the albian in this area.

    This is an old name for the uppermost part of the turonian and is characteristed by rather softer chalk than that beneath and particularly by the presence of flints. The westward overstep of the wealden by the albian in worbarrow bay is clearly shown. Durlston bay but with some data on worbarrow tout and the quarries of the swanage area. Evidence for these hitherto unrecognised faults is based on outcrop displacement and differences in (a) outcrop widths either side of the faults (b) strike and dip of the strata and (c) the direction of the axis of the monocline. Clays, sandy, with jarosite, blackish to pale, passing irregularly into cross-bedded, concretionary sandstone masses. This is thicker and coarser than the others, is multistorey and is sufficiently coarse to be a pebble bed in parts. The purbeck sequence at the tout has been carefully logged by. This bed (bed 15 of ) was wrongly thought by victorian geologists to be some sort of tufa. What do you think has really happened here (possible clues - the breach in the portland stone ridge between st. This has not been accurately dated in this area but is clearly pre-ipswichian (because of the raised beach) and probably from about the wolstonian or hoxnian part of the pleistocene.

    Worbarrow Bay (also spelt "Worthbarrow" or "Warbarrow") provides one of the best coastal sections of Cretaceous strata in Europe. At the southern part of the bay the Jurassic-Cretaceous boundary is near the base of the limestones and shales of the Purbeck

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    e-BOOKS. There is a lot of interest across the region for electronic or e-books, books in digital form that can be read from a dedicated e-book reader such as the Kindle, Nook,I-Pad and Sony Reader among many.
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    Audio books are becoming avery popular way of reading a book. In general in dorset the lower chalk is cyclical and rather grey and marly. It might be worth checking on its dolomite content because wb 83 has about 82 dolomite and thus is similar to the top lacustrine dolomites of the soft cockle member of incidently this part of the section at worbarrow tout is less well-known than the equivalent at durlston bay. Centre a sketch from a photograph of the footprints in less eroded condition in january, 1978. Worbarrow bay on the east side and mupe bay on the west where there are usually thinner successions.

    The small euryhaline bivalve occurs in this and in the overlying soft cockle member, which is mostly of marls Buy now Dissertations Port Ac Uk View Year

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    On the basal pebble bed is a ferruginous, argillaceous stone band, 0. The mined gypsum with anhydrite in sussex (mountfield and brightling) supports this view that hydration was very late and within about 100m or less of the surface. This had affinities with present-day cornubia, armorica and nw iberia, which apparently represents its relict flanks. These evaporite papers also deal with the soft cockle gypsum. It is however, entirely within the portland and purbeck formations.

    A single additional footprint from the purbeck formation was found loose, but although there is reference to a possible origin in the freestone member or the broken beds, because of the error with the main footprints, it is difficult to know whether this is correct Dissertations Port Ac Uk View Year Buy now

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    The carbonate was usually pelletoidal and of silt-size, but it is not known whether is was aragonite or high-mg calcite. It is very compacted and this is normal within the wealden sequence. At low tide most of this is accessible, with a little scrambling over rocks. Essential for any serious study of the purbeck sequence here. Such a depression into the muddy sand and clay with lignite is quite likely to have been formed by a passing dinosaur, and would not be unusual for the wealden strata.

    Slumped gault is shown in the left-hand photograph above, with perhaps some slumped upper greensand. These rounded pebbles mark a plane of unconformity and represent the relics of an ancient pebble beach Buy Dissertations Port Ac Uk View Year at a discount

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    Bury was probably discussing the flandrian stage (holocene) or at least the very late pleistocene and two hypotheses may not be totally incompatible. Mammal remains have not been found in the equivalent beds of worbarrow tout, but, of course, might be present and awaiting discovery. A generalised succession of the wealden strata of worbarrow bay is given below. This narrow isthmus clearly marks the floor of an old river-valley, and it is interesting as the only valley which cuts at all deeply into the long range of jurassic hills, other than the valley that once continued south through lulworth cove (and, of course, a stream flowing south from arish mell and continuing the valley there should have cut the ridge in the past) Buy Online Dissertations Port Ac Uk View Year

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    Compared to later pebbles beds, like those in the eocene or pleistocene strata this is a strange deposit. Beds of hard shell-debris (biosparrudite) limestones with about 1 metre of pyritic shales with some beef and jarosite in the central part ( mid-intermarine shales ). There are logs with some lithological details for ballard head, mupe bay and white nothe, dorset. Scrambling on the rocks of worbarrow tout can be hazardous and cliff-climbing is not recommended the westward-projecting promontory of portland stone has some features of geological interest at the landward end, but if one proceeds further there is some risk of sliding on the rocks or falling into the sea. The difference in level between the ravine floor and the broader valley floor is about 11 m to 12 m near the mouth and diminishes upstream Buy Dissertations Port Ac Uk View Year Online at a discount

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    An approximate date of this hydration is indicated by the fabric of satin spar. They are related and closely adjacent phases of the late kimmerian unconformity. Worbarrow tout, but reveals the common occurrence of footprints at about the horizon of the worbarrow, middle purbeck footprints. The difference in level between the ravine floor and the broader valley floor is about 11 m to 12 m near the mouth and diminishes upstream. The photograph shows a cross-section through a hollow log preserved as lignite.

    These may have been related to movements of the massif generated by changes in north atlantic spreading rates and opening of biscay. The purbeck sediment surface was exposed numerous times (supratidal sabkhas, mudcracks, dinosaur footprints etc Dissertations Port Ac Uk View Year For Sale

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    It is largely based on the el-shahat thesis of 1977 and uses clements bed numbers. This bed (bed 15 of ) was wrongly thought by victorian geologists to be some sort of tufa. Corfe gaps too great to have been supplied by the catchments of steeple brook and tyneham brook combined, and probably derived from a much larger area of kimmeridge terrain via the worbarrow-mupe gap in the portland escarpment. The regional library allows for the pooling of resources to better serve the three counties. Furthermore because the area is within a firing range you may not be allowed to explore the upper cliff (where there could be tank shells).

    Pondfield lies only a few hundred metres to the north of the axis of the purbeck anticline and the portland and purbeck stone ridge is generally unbroken elsewhere, for example gad cliff For Sale Dissertations Port Ac Uk View Year

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    In contrast, isolated channel sandstones, wedging out into finer argillaceous sand or into clay are also common in the wealden cliff section of worbarrow bay. At low tide a particular calcitised anhydrite bed with euhedral quartz (common in evaporites - eg bristol diamonds etc. There are inevitably certain rules and there are range wardens in the area who are concerned with safety and conservation but there is no feeling of severe supervision and little sign of military activity. I recorded them briefly in a geologists association field trip report , which gave an account of a field trip in 1966 with professor douglas shearman and mary pugh. The plenus marl (high cenomanian) is a good marker bed, 1 Sale Dissertations Port Ac Uk View Year

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