poole harbour peninsular
Other Webpages on Studland and Adjacent Area: |Studland - South Haven Peninsula (the main page on Studland) Deviated drilling is extensively used at the Wytch Farm Oilfield and few wells proceed down vertically. Hook Island, if it had been built, might have had some consequence. With it is some weathered Palaeozoic-type slate. This is a nature reserve, so do not disturb bird life and avoid the remote shore areas where possible. Faculty of Natural and Environmental Sciences, Studland - South Haven Peninsula (the main page on Studland), Studland - South Haven Peninsula (main page), Redend Sandstone at Redend Point, Studland. The sandstone is almost horizontal with conspicuous, fairly small-scale, cross bedding. Field trips shown in photographs do not necessarily have any connection with Southampton University and may have been private or have been run by various organisations. The outer banks are only 0.3 metres high, but may be up to 6 metres across (Legg, 1987). In warm weather there may be occasional adders in the heathland. |Swanage Bay Oilfield Beneath the South Haven Peninsula. Studland - South Haven Peninsula (main page). No liability is accepted. Discussion of geological and geomorphological features, coast erosion, coastal retreat, storm surges etc are given here for academic and educational purposes only. Contact 01202 440200. This is a good representation of the type of mixed sediment that can occur on the harbour shores in this area. This oilfield is one of the largest onshore in northwest Europe, and is noted for its excellent record regarding the environment (BP have awards for this) and concealment. (Here is another question for students: Compare the relatively natural South Haven Peninsula with a fully-developed or almost fully-developed sand spit in southern England. The most famous of the 15th century privateers operating from Poole Harbour was the notorious Harry Paye. It is not actually a coincidence that the harbour entrance is so neatly positioned in relation to this reservoir (this is a good point for student discussion - Why is this? (Other theories include the former presence of oak trees in the centre, with acorns for pigs, but no access for ponies, for which they are poisonous: a certain answer to the qeustion of origin is not available at present. Geological fieldwork involves some level of risk, which can be reduced by knowledge, experience and appropriate safety precautions. Their official website can be found at https://www.pooletourism.com and is a great resource to help plan you visit to Poole and surrounding area. The large car park for Sandbanks Beach is towards the bottom right of the photo. No liability for death, injury, damage to, or loss of property in connection with a field trip is accepted by providing these websites of geological information. There are also some superb mountain biking routes around the harbour and through the Purbecks and along the Jurassic Coast. In Brand's Bay further to the south there is at present (June 2007) a very large accumulation of algal slime or filamentous green algae. He burnt Gigon and Finisterra and carried off the holy crucifix from Santa Maria de Finisterra. This should not cause much problem at Studland, and in webpages dealing largely with the Chalk, a conversion table is provided. A Poole Park family. Not all places need be visited and the descriptions and photographs here can be used as an alternative to visiting. Sandbanks peninsular. There are apparently no less than seventy-one circles in the area between Redhorn Quay and Jerry's Point (Gerry's Point on an old map). The Peninsula is surrounded by Poole Harbour on one side and Poole Bay on the other. This is typical of the harbour environments and would not normally occur on the open sea beaches where abrasion would destroy such coatings. In providing field guides on the Internet no person is advised here to undertake geological field work in any way that might involve them in unreasonable risk from cliffs, ledges, rocks, sea or other causes. It is about the northernmost limit of gravel, as opposed to sand on the beaches of the Poole Harbour side of the South Haven Peninsula. With it, on the shore, are numerous small shells of Hydrobia, the common harbour and lagoon gastropod, which probably browses on the algae. Redend Point is a consequence of the more resistant sandstone lying within clays and unconsolidated sands and forming a small headland and ridge. Persons undertaking field work should assess the risk, as far as possible, in accordance with weather, conditions on the day and the type of persons involved. Re regard to the Chalk note that the Portsdown Chalk Formation is in the zone of Belemnitella mucronata. 5.5 STUDLAND PENINSULA - POOLE HARBOUR SIDE - LOCATIONS: Gravel Point Near South Haven Point on the Poole Harbour side is a very small promontory known as Gravel Point (map reference SY 033864). This is now done by an extended-reach borehole (horizontal and even upward drilling) from Goathorn Peninsula to somewhere off Bournemouth Pier. The experienced geologist will know whether an old or new scheme is being used. The Palaeogene or Tertiary strata are not quite so easy to deal with. Copyright Unexplained Circles between Jerry's Point and Redhorn Quay, Unexplained Circles between Jerry's Point and Redhorn Quay. (Legg (1987) quoted the Royal Commission on Historical Monuments: "Many held rainwater for short periods, displaying a wet bog flora; others are heath-covered. This is because of supply of coarse grains from the gravel (not available in the blown sand). Poole Harbour is Europe’s largest natural harbour and the perfect destination for visitors looking to enjoy a mix of world class beaches as well as unspoilt countryside and coastal walks. Permission should be sought for entry into private land and no damage should take place. This map by Ralph Treswall in 1585-6 (also with a personal interpretation) shows the South Haven Peninula before development of the main area of blown sand. The upper reservoir, not shown here, is in the Jurassic Bridport Sands and was discovered in 1974. Incidently, note that the BGS maps show "Head" associated with and mainly to the west of the dune ridges. Stay very close to the heath and watch out for any patches of soft mud. It shows no evidence of marine origin and is presumably fluviatile like the Redend Sandstone and the Agglestone Grit. There is a gap in the ridge at Corfe Castle. Payne (1953) has said that local tradition is that Harry Paye could reach Round Island either by the normal route through Wytch Channel or by the South Deep Channel which is north of Ower. Aerial view of Poole Harbour showing the Sandbanks Peninsula in the foreground, Brownsea Island in the middle of the harbour and Poole Quay and Poole in the background.
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