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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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Keep away from the foot of the cliff as far as is feasible, avoid lingering there and wear hard-hats. Worbarrow bay on the east side and mupe bay on the west where there are usually thinner successions. They originated on tidal flats at the western margin of an extensive brackish lagoon.

Although the tidal range is not great it is frequently possible to be cut off by the tide at the western side of worbarrow tout. Geographically the massif probably focussed on what is now the continental margin, over the southwestern approaches. 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.

His view was that the tyneham gwyle originally turned southward and flowed through the gap into pondfield cove. Perhaps the reader would like to consider these matters futher, making further comparisions between present and old maps. 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.

Dorset and isle of wight field sections compared with the marchwood and winterborne kingston borehole logs. This is one of the main parts of the purbeck formation where dinosaur footprints are preserved in extensive damp lagoon-margin flats of shell sediments. The oyster of the cinder bed, , a bivalve which probably suggests near-marine salinities.

The wealden deposits may have been at least twice the total thickness until deeply buried under the chalk. Note that the latter paper is valuable for facies information, but uses a different terminology. A short history of the the discovery of reptilian footprints in the purbeck beds of dorset, with notes on their stratigraphical distribution.

An unusual feature in the upper purbecks is authigenic glauconite occurring within freshwater gastropod shells. Henry rolls, shoemaker, of east lulworth (born 5th april, 1803). It is interesting that although there are numerous examples of silificified coniferous trees from the purbeck formation, mostly from the isle of portland, i know of no record of a hollow purbeck silicified tree. However, this does not eliminate a load cast because a thick unit of sand above could have been eroded away, shortly after deposition. He suggested that this pursued a separate course and probably provided the gateway by which, during a phase of marine transgression, the sea entered the region of soft wealden strata and so initiated worbarrow bay.


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 At corfe, however, The steep chalk cliffs at the northern part of the bay are dangerous for climbing, and there may be falls of chalk here so care should be taken. The exact direction is not known and broken lines show a range of possibilities. The coarse quartz grit at mupe bay is 30 metres above the middle of the wealden at mupe bay, whereas it is almost at the middle in the cliffs at worbarrow bay. The purbeck shell limestones (left) probably originated in shell beaches like those at the margin of the coorong lagoon in south australia (right). The base of the gault above the lower greensand is marked by a 0. 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 applies in general to worbarrow bay and worbarrow tout, but the thicknesses are greater than those shown, which apply to lulworth cove.
  • Worbarrow Bay, Dorset, Geological Guide by Ian West


    Many of the wealden sandstones show channel-like features and are lenticular and laterally discontinuous. The bay is open at most weekends and bank holidays and usually for a longer period during august. Is the direction indicated the same as that at bacon hole or durlston head? Pondfield cove is just east of worbarrow tout and just west of gad cliff. Early and late lithification of aragonite bivalve beds in the purbeck formation (upper jurassic - lower cretaceous of southern england). At corfe, however, the streams are flowing in the direction of dip, not against it.

    In one of these impressions of horse tails and plant foliage have been found. Bury noted that while the little valley at pondfield might at first sight be expected to be the small relic of a consequent stream flowing northward down the dip, the origin may in fact be less simple. This is seen when walking towards cow corner and it is here, informally called the cow sandstone, for convenience of recognition. The footprints have been emphasised artificially by placing wet mud in them, but following as far as possible the natural outline. Lignite beds sometimes occur above the sandstones where they are probably fills of abandoned channels, perhaps oxbow lakes, with transported logs and plant debris.

    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. The conical hill of worbarrow tout is separated from gad cliff by the little inlet of pondfield cove. Although some comparison is drawn between the purbeck evaporites and those of with middle eastern sabkhas, it must be appreciated that this was a palaeoenvironment at about 37 degrees north, with forests growing in the vicinity it was, of course, semi-arid and there is no evidence of sand deserts. This is not the problem to visitors that it might appear to be. Species of are probably the main components of the middle purbeck building stone, but in the lower purbeck formation there are shell-beds that consist of the high-salinity tolerant bivalve -. On the basal pebble bed is a ferruginous, argillaceous stone band, 0. The middle purbeck building stones usually have the mollusc shells in crushed condition so the left part of the illustration is based on a corbula member shell bed from visiting bipedal herbivores such as kangeroos or iguanodons may leave footprints in favourable circumstances. There are occasional larger flints, and rare pebbles of quartz, wealden grit, upper greensand, purbeck beds, and quartzite (one found, 1. The southward slope of the pondfield remnant may be due to recent erosion by flood water after heavy rain flowing down into the cove. This contains a good near-limnic fauna at durlston bay, and in it the famous of victorian times were made by beckles and others.

    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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    Even though i drew attention to this, the error lasted through to the paper of. This fig 1 is a very useful table correlating traditional chalk stratigraphy, stages, key marker beds etc and newer formation and member names. The matter, however, is not clear-cut and is open to discussion and individual assessments. Wealden fluvial clastics, with lignite, represent much of the lower cretaceous above the purbecks. Right image the cinder bed at stair hole, shown here to give a view of the small oyster shells that form a major part of this bed.

    An approximate date of this hydration is indicated by the fabric of satin spar. This is not the problem to visitors that it might appear to be. It is a beach of dominantly flint pebbles, quite well-rounded almost like those of the chesil beach (except that there is much more upper greensand chert there) and unlike the subangular flint pebbles which are ubiquitous on the beaches of hampshire, further east Buy now Dissertations Port Ac Uk View Year

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    In any discussion bear in mind the prevailing southwesterly wind and erosion by waves from this direction. Worbarrow bay (also spelt worthbarrow or warbarrow) provides one of the best coastal sections of cretaceous strata in europe. Shells and former pores are occupied by non-ferroan sparry calcite cement, and there is little pyrite. The euhedral quartz crystals within it are comparable to bristol diamonds of evaporite replacement origin, but smaller. Dorset publishing company at the wincanton press, national school, north street, wincanton, somerset, ba9 9at.

    Dinosaur bones have been found here but are relatively rare. Note the iron cementation at the top and bottom of the bed. It may well correlate with the jurassic-cretaceous boundary in the boreal realm, that is the northern and russian region, but not with the (now official) jurassic-cretaceous boundary of the south of france Dissertations Port Ac Uk View Year Buy now

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    This too indicates some hypersalinity and pseudomorphs after halite are the most obvious signs of this. Lignite beds sometimes occur above the sandstones where they are probably fills of abandoned channels, perhaps oxbow lakes, with transported logs and plant debris. Arkells idea about the initiation of the old river gap is a sound one, but this fluvial break in the portland stone ridge need never have been much lower than about 40 m until the devensian. In terms of structure the lower chalk dips at 35 n. This is a fossiliferous ironstone with the bivalves the wealden strata are reddish, yellow with some cream and purple coloured sediments.

    See on the enterolithic veins and nodules of the calcium sulphate Buy Dissertations Port Ac Uk View Year at a discount

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    This was classified at the lowest part of the upper chalk (although note that it isturonian like most of the middle chalk beneath). This photograph shows the purple channel sandstone, one of the lesser sandstones beneath the coarse quartz grit in the wealden of worbarrow bay. The subhumid conditions seem to have been favourable to dinosaurs, crocodiles and turtles. The secondary gypsum may still persist in this bed even only 10 or 100m beneath the surface, by comparison with evaporite residues on portland, the pyrenees and elsewhere. Look for rare echinoid spines ( ) in the hard cinder which show that conditions were normal marine for a short time.

    The facies is fluvial with coarse channel sandstones, overbank silts and clays and with some lignite beds Buy Online Dissertations Port Ac Uk View Year

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    Isle of wight) the above diagram showing the postulated history of development of calcium sulphate nodules in the purbeck strata is from bed wb 29, which although listed as a pelsparite with hummocky surface, seems to be a calcitised evaporite bed with some small quantities of replacive silica. I am grateful for the recent help of 4th year, m. 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 ). Some celestite occurs in the (hypersaline) hard cap and there are also good cyanobacterial mats in this unit (as shown by as a matter of interest look at the evidence for movement overlying beds over the evaporitic plane of weakness of the broken beds (formerly an anhydrite-limestone breccia) Buy Dissertations Port Ac Uk View Year Online at a discount

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    Purbeck strata of worbarrow tout, in the style of the classic clements section of durlston bay. Right worbarrow tout with north-dipping thin-bedded purbeck limestones and shales, and with gad cliff rising away to the east. This was classified at the lowest part of the upper chalk (although note that it isturonian like most of the middle chalk beneath). The nearest area of extensive precambrian rocks in brittany, northwest france, and, indeed, wealden sediments have been found in the english channel, offshore to the north of brittany. These may have been related to movements of the massif generated by changes in north atlantic spreading rates and opening of biscay.

    You will notice that the pebbles are subangular to subrounded and mostly of vein quartz, with some fracture pits Dissertations Port Ac Uk View Year For Sale

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    However, this does not eliminate a load cast because a thick unit of sand above could have been eroded away, shortly after deposition. On either side of this ravine there is the broad flat floor of a mature valley which is followed by the gravel track from tyneham to the sea. Stay within the official range walks or on the beach. Isle of wight) the above diagram showing the postulated history of development of calcium sulphate nodules in the purbeck strata is from bed wb 29, which although listed as a pelsparite with hummocky surface, seems to be a calcitised evaporite bed with some small quantities of replacive silica. Worbarrow bay (also spelt worthbarrow or warbarrow) provides one of the best coastal sections of cretaceous strata in europe For Sale Dissertations Port Ac Uk View Year

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    The latter ridge which has a remarkably even sky-line, attains its greatest altitude (631 ft. Wealden lignite does not normally occur as beds of brown coal, as occur in the eocene strata, but is dispersed in silt, fine sand or clay or a mixture of these. Above the coarse quartz grit, in the northwestern part of worbarrow bay there is a fairly continuous sandstone of much finer grain size than the grit. 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. At worbarrow bay the most obvious lignite beds are in the succession below the coarse quartz grit Sale Dissertations Port Ac Uk View Year

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