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The Isle of Wight Coast Path Guided Trail Holiday
The Isle of Wight Coast Path Guided Trail Holiday Tour Style: Guided Trails Destinations: Isle of Wight & England Trip code: FWLIC Trip Walking Grade: 3 HOLIDAY OVERVIEW The Isle of Wight Coast Path circuits the island in an anti-clockwise direction and provides a wonderful opportunity to view the island’s beautiful and varied coastline, including the chalk headlands of the Needles and Culver Cliff. The trail is interspersed with pretty coastal villages and Victorian resorts such as Ventnor. It includes some inland walking around Queen Victoria’s Osborne Estate, Cowes and Newtown Harbour National Nature Reserve. WHAT'S INCLUDED • High quality en-suite accommodation in our country house • Full board from dinner upon arrival to breakfast on departure day • The services of an HF Holidays' walks leader • All transport on walking days www.hfholidays.co.uk PAGE 1 [email protected] Tel: +44(0) 20 3974 8865 HOLIDAYS HIGHLIGHTS • A circuit of the Isle of Wight coast • The dramatic chalk headlands of the Needles and Culver Cliff • Stay at Freshwater Bay House TRIP SUITABILITY This Guided Walking/Hiking Trail is graded 3 which involves walks/hikes on generally good paths, but with some long walking days. There may be some sections over rough or steep terrain and will require a good level of fitness as you will be walking every day. It is your responsibility to ensure you have the relevant fitness required to join this holiday. Fitness We want you to be confident that you can meet the demands of each walking day and get the most out of your holiday. -
Historic Environment Action Plan the Undercliff
Directorate of Community Services Director Sarah Mitchell Historic Environment Action Plan The Undercliff Isle of Wight County Archaeology and Historic Environment Service October 2008 01983 823810 archaeology @iow.gov.uk Iwight.com HEAP for the Undercliff. INTRODUCTION This HEAP Area has been defined on the basis of geology, topography, land use and settlement patterns which differentiate it from other HEAP areas. This document identifies essential characteristics of the Undercliff as its geomorphology and rugged landslip areas, its archaeological potential, its 19 th century cottages ornés /marine villas and their grounds, and the Victorian seaside resort character of Ventnor. The Area has a highly distinctive character with an inner cliff towering above a landscape (now partly wooded) demarcated by stone boundary walls. The most significant features of this historic landscape, the most important forces for change and key management issues are considered. Actions particularly relevant to this Area are identified from those listed in the Isle of Wight HEAP Aims, Objectives and Actions. ANALYSIS AND ASSESSMENT Location, Geology and Topography • The Undercliff is identified as a discrete Landscape Character Type in the Isle of Wight AONB Management Plan (2004, 132). • The Area lies to the south of the South Wight Downland , from which it is separated by vertical cliffs forming a geological succession from Ferrugunious Sands through Sandrock, Carstone, Gault Clay, Upper Greensand, Chert Beds and Lower Chalk (Hutchinson 1987, Fig. 6). o The zone between the inner cliff and coastal cliff is a landslip area o This landslip is caused by groundwater lubrication of slip planes within the Gault Clays and Sandrock Beds. -
HEAP for Isle of Wight Rural Settlement
Isle of Wight Parks, Gardens & Other Designed Landscapes Historic Environment Action Plan Isle of Wight Gardens Trust: March 2015 2 Foreword The Isle of Wight landscape is recognised as a source of inspiration for the picturesque movement in tourism, art, literature and taste from the late 18th century but the particular significance of designed landscapes (parks and gardens) in this cultural movement is perhaps less widely appreciated. Evidence for ‘picturesque gardens’ still survives on the ground, particularly in the Undercliff. There is also evidence for many other types of designed landscapes including early gardens, landscape parks, 19th century town and suburban gardens and gardens of more recent date. In the 19th century the variety of the Island’s topography and the richness of its scenery, ranging from gentle cultivated landscapes to the picturesque and the sublime with views over both land and sea, resulted in the Isle of Wight being referred to as the ‘Garden of England’ or ‘Garden Isle’. Designed landscapes of all types have played a significant part in shaping the Island’s overall landscape character to the present day even where surviving design elements are fragmentary. Equally, it can be seen that various natural components of the Island’s landscape, in particular downland and coastal scenery, have been key influences on many of the designed landscapes which will be explored in this Historic Environment Action Plan (HEAP). It is therefore fitting that the HEAP is being prepared by the Isle of Wight Gardens Trust as part of the East Wight Landscape Partnership’s Down to the Coast Project, particularly since well over half of all the designed landscapes recorded on the Gardens Trust database fall within or adjacent to the project area. -
View of What Is Now Known About
A PHASE OF THE UPPER DEVONIAN OF WESTERN HIGHLAND COUNTY, VIRGINIA By Helen F. Pulver A. B., Berea College, 1946 A thesis submitted to the Faculty of Oberlin College in partial fulfillment of the requirements for the Degree of Master of Arts in the Department of Geology 1948 PLATE I Chemung formation, Alleghany Mountain locality, 3145 A fossiliferous bed of arenaceous shale, containing predominantly Douvillina cayuta; Schizophoria stria tula in the upper and lower right hand corners, and a part of Tylothyris mesacostalis and Camarotoeehia eximia in the center. PLATE 1 PREFACE '!his paper is a study of the Brallier and Chemung formations - of west Highland County, Virginia. '!he limits of the Brallier forma t.ion are determined on the basis ot faunal and lithological evidence, and correlations made with format.ions in New York, Pennsylvania, Maryland and West Virginia. 'Ihe field work was carried on during the lat ter part of the summer of 1947 and the identification and correlations worked out in the winter of 1947 and the spring of 1948. I wish to thank Mr. Minor B. Long and 1fr. Bruce Weber for help in measuring .the section of the field. I am. grateful to Dr. E. C. Stumm for his interest and original suggestion of the problem. ~ Dr. C.W• .Carlston I should like to express my thanks for valuable suggestions in the field and in the preparation of this manuscript. Above all I should. like to express my deep appreeiation to Dr. Fred Foreman under whose direction this problem was completed, for his continued encouragement and constant assistance. -
Brachiopods from the Mobarak Formation, North Iran
GeoArabia, 2011, v. 16, no. 3, p. 129-192 Gulf PetroLink, Bahrain Tournaisian (Mississippian) brachiopods from the Mobarak Formation, North Iran Maryamnaz Bahrammanesh, Lucia Angiolini, Anselmo Alessandro Antonelli, Babak Aghababalou and Maurizio Gaetani ABSTRACT Following detailed stratigraphic work on the Mississippian marlstone and bioclastic limestone of the Mobarak Formation of the Alborz Mountains in North Iran, forty-eight of the most important brachiopod taxa are here systematically described and illustrated. The ranges of the taxa are given along the Abrendan and Simeh Kuh stratigraphic sections, located north of Damgham. The examined brachiopod species date the base of the Mobarak Formation to the Tournaisian, in absence of age-diagnostic foraminifers. Change in brachiopod settling preferences indicates a shift from high energy, shallow-water settings with high nutrient supply in the lower part of the formation to quieter, soft, but not soppy substrates, with lower nutrient supply in the middle part of the Mobarak Formation. Brachiopod occurrence is instead scanty at its top. The palaeobiogeographic affinity of the Tournaisian brachiopods from North Iran indicates a closer relationship to North America, Western Europe and the Russian Platform than to cold-water Australian faunas, confirming the affinity of the other biota of the Alborz Mountains. This can be explained by the occurrence of warm surface-current gyres widely distributing brachiopod larvae across the Palaeotethys Ocean, where North Iran as other peri- Gondwanan blocks acted as staging-posts. INTRODUCTION The Mississippian Mobarak Formation of the Alborz Mountains (North Iran) has been recently revised by Brenckle et al. (2009) who focused mainly on its calcareous microfossil biota and refined its biostratigraphy, chronostratigraphy and paleogeography. -
English Nature Research Report
Maritime Natural Area: MIO. Whitstable to Geological Significance: Notable North Foreland (provisional) General geologicaVgeomorpholugicaIcharactcr: The Whitstable to North Foreland Maritime Natural Area has a varied coastline with relatively low-lying coast in thc cast rising to boulder clay and chalk cliffs towards the Isle of Thanet. Geological Htrtory: This coastline is characterised by the Cretaceous chalk of the Isle oTThanet bounded to the west by clays, silts and sands of the Lower ‘I’ertiary. Upper Cretaceous Santonian chalk (87-83 Ma) is exposed dipping gently to the west from Margatc to the eastern side of Herne Bay. Unconformably overlying the chalk is a sequence of Lower Tertiary scdiments which are exposed in I Ierne Bay; the Palaeocenc Thanet, Woolwicli and Oldhaven Formations overlain by the Eocene London Clay Formation. The Chalk was deposited by a shallow sea which covered much of Northwestern Europe towards the end of the Cretaceous. Sea lcvel fall was followed by the unconformabie deposition of Tertiary Palaeocene and Ikcene sedirnents. Dominantly marine in origin, these scdiments were deposited by a rising, but fluctuating sea, which covered much of Southeast England. Marine conditions were well established by the Eocene leading to the deposition ofthe i,ondon Clay Formation. Thc fossil fauna and flora from the Tertiary rocks indicates a gradually warming climate with sub-tropical conditions established by the Eocene. Subsequent uplilt (associated with the Alpine Orogeny) and resultant erosion removed much of the remaining Tertiary sediments, the next deposition occurring during the Pleistocene. Though not covercd by ice, the area was affectcd by periglacial erosion in a tundra-like environment during the last glaciation (Devensian). -
Biodiversity Patterns Across the Late Paleozoic Ice Age
Palaeontologia Electronica palaeo-electronica.org Biodiversity patterns across the Late Paleozoic Ice Age Barbara Seuss, Vanessa Julie Roden, and Ádám T. Kocsis ABSTRACT The Late Palaeozoic Ice Age (LPIA, Famennian to Wuchiapingian) witnessed two transitions between ice- and greenhouse conditions. These alternations led to drastic alterations in the marine system (e.g., sea-level, habitat size, sea-surface temperature) forcing faunal changes. To reassess the response of the global marine fauna, we ana- lyze diversity dynamics of brachiopod, bivalve, and gastropod taxa throughout the LPIA using data from the Paleobiology Database. Diversity dynamics were assessed regarding environmental affinities of these clades. Our analyses indicate that during the LPIA more taxa had an affinity towards siliciclastic than towards carbonate environ- ments. Deep-water and reefal habitats were more favored while grain size was less determining. In individual stages of the LPIA, the clades show rather constant affinities towards an environment. Those bivalves and brachiopods with an affinity differ in their habitat preferences, indicating that there might have been little competition among these two clades. Origination and extinction rates are similar during the main phase of the LPIA, whether environmental affinities are considered or not. This underlines that the LPIA marine fauna was well adapted and capable of reacting to changing environ- mental and climatic conditions. Since patterns of faunal change are similar in different environments, our study implies that the changes in faunal composition (e.g., diversity loss during the LPIA; strong increase of brachiopod diversity during the Permian) were influenced by the habitat to only a minor degree but most likely by yet unknown abiotic factors. -
Isle of Wight Settlement Coalescence Study Report.Docm Last Saved: 26/04/2018 17:02
Isle of Wight Settlement Coalescence Study Prepared by LUC April 2018 Project Title: Isle of Wight Settlement Coalescence Study Client: Isle of Wight Council Version Date Version Details Prepared by Checked by Approved by 4.0 26/4/2018 Final Jon Pearson Jon Pearson Philip Smith Richard Swann Ben Gurney Calum McCulloch Victoria Goosen Isle of Wight Settlement Coalescence Study Report.docm Last saved: 26/04/2018 17:02 Isle of Wight Settlement Coalescence Study Prepared by LUC April 2018 Planning & EIA LUC LONDON Offices also in: Land Use Consultants Ltd Registered in England Design 43 Chalton Street Bristol Registered number: 2549296 Landscape Planning London Edinburgh Registered Office: Landscape Management NW1 1JD Glasgow 43 Chalton Street Ecology T +44 (0)20 7383 5784 Lancaster London NW1 1JD FS 566056 EMS 566057 LUC uses 100% recycled paper GIS & Visualisation [email protected] Manchester Contents 1 Introduction 1 Context and key issues 1 Purpose of study 1 2 Methodology 3 Overview 3 Tasks undertaken 3 3 Results - nature of gaps and guidelines for maintenance 5 West Wight area 6 Cowes–Newport area 13 Ryde area 26 ‘The Bay’ area 39 4 Policy review and recommendations 46 Policy review 46 Recommended policy approach to avoiding settlement coalescence 53 1 Introduction Context and key issues 1.1 The Isle of Wight has a unique identity characterised by a predominantly rural landscape. Almost half of its coastline is designated as Heritage Coast and over half of the Island is a designated Area of Outstanding Natural Beauty. The majority of residents live in the Island’s larger settlements, in particular the main towns of Newport, Cowes, East Cowes, Ryde, Sandown and Shanklin. -
Historic Environment Action Plan Brading Haven and Bembridge Isle
Directorate of Community Services Director Sarah Mitchell Historic Environment Action Plan Brading Haven and Bembridge Isle Isle of Wight County Archaeology and Historic Environment Service October 2008 01983 823810 archaeology @iow.gov.uk Iwight.com HEAP for Brading Haven and Bembridge Isle INTRODUCTION The Brading Haven and Bembridge Isle HEAP Area comprises land surrounding the former Brading Haven together with the reclaimed land of the haven itself. It includes the settlement of Brading in the west of the Area, St Helens and Nettlestone in the north, Bembridge in the east and Yaverland in the south. Part of this Area, including Bembridge and Yaverland, was for much of its history an island in its own right, cut off from the Wight mainland by arms of the sea at high tide and muddy gulfs at low tide, hence its former name of ‘Bembridge Isle’. A wide area of sea flowed up between Bembridge and St. Helens, past Brading and Yaverland and then joined up with another branch of sea that entered through a gap between Yaverland and Sandown where the boating lake is today. The area between Yaverland and Sandown became known as the ‘Sandown Level’ after it had been drained. A further branch struck off west towards Alverstone. These tidal inlets effectively cut Bembridge Isle off from the rest of the Island until the construction of a causeway at Yar Bridge in the Middle Ages. However, Brading Haven remained as a wide tidal inlet at the mouth of the Eastern Yar River, extending as far inland as Brading, until it was drained between 1878 and 1880, leaving the much smaller area of Bembridge Harbour (Martin 2004a). -
Barnacle Paper.PUB
Proc. Isle Wight nat. Hist. archaeol. Soc . 24 : 42-56. BARNACLES (CRUSTACEA: CIRRIPEDIA) OF THE SOLENT & ISLE OF WIGHT Dr Roger J.H. Herbert & Erik Muxagata To coincide with the bicentenary of the birth of the naturalist Charles Darwin (1809-1889) a list of barnacles (Crustacea:Cirripedia) recorded from around the Solent and Isle of Wight coast is pre- sented, including notes on their distribution. Following the Beagle expedition, and prior to the publication of his seminal work Origin of Species in 1859, Darwin spent eight years studying bar- nacles. During this time he tested his developing ideas of natural selection and evolution through precise observation and systematic recording of anatomical variation. To this day, his monographs of living and fossil cirripedia (Darwin 1851a, 1851b, 1854a, 1854b) are still valuable reference works. Darwin visited the Isle of Wight on three occasions (P. Bingham, pers.com) however it is unlikely he carried out any field work on the shore. He does however describe fossil cirripedia from Eocene strata on the Isle of Wight (Darwin 1851b, 1854b) and presented specimens, that were supplied to him by other collectors, to the Natural History Museum (Appendix). Barnacles can be the most numerous of macrobenthic species on hard substrata. The acorn and stalked (pedunculate) barnacles have a familiar sessile adult stage that is preceded by a planktonic larval phase comprising of six naupliar stages, prior to the metamorphosis of a non-feeding cypris that eventually settles on suitable substrate (for reviews on barnacle biology see Rainbow 1984; Anderson, 1994). Additionally, the Rhizocephalans, an ectoparasitic group, are mainly recognis- able as barnacles by the external characteristics of their planktonic nauplii. -
Metal Detectors on Isle of Wight Council-Controlled Beaches
Metal detectors on Isle of Wight Council-controlled beaches The council allows metal detecting on any beaches Crown Estate permits (but no other land) it owns or controls. A Crown Estate metal detecting permit is not needed Most of the Isle of Wight’s popular urban beaches (including Ryde, to go metal detecting on Council controlled foreshore, Ventnor, Shanklin and Sandown) are owned by the Isle of Wight but may be elsewhere. Council, and many other stretches of coast are controlled by the It is possible to obtain a permit from the Crown Estate to use a council under lease from the Crown Estate. metal detector on Crown Estate beaches. However, a Crown Estate There are many other beaches, not owned by the council, on permit does not give a detectorist the right to use detecting which metal detectorists may or may not be able to enjoy their equipment on Crown land which has been leased to a third party. hobby lawfully subject to necessary permissions. This map is In the case of beaches controlled by the Isle of Wight Council intended to help metal detectorists by giving guidance on where there is no need for such a permit. In the case of all other beaches council beaches are located. It does not give information about you should check with the landowner or occupier. any other beaches which are not owned or controlled by the council, or other permits you might need. Note To gain permission to use metal detecting equipment on other Many beaches owned and controlled by the council are also beaches, metal detectorists should approach the owner or designated as Sites of Special Scientific Interest, on which occupier of that beach. -
Military HEAP for the Isle of Wight
Island Heritage Service Historic Environment Action Plan Military Type Report Isle of Wight County Archaeology and Historic Environment Service April 2010 01983 823810 Archaeology @iow.gov.uk Iwight.com Military HEAP for the Isle of Wight 1.0 INTRODUCTION Page 3 2.0 ASSESSMENT OF THE HISTORIC ENVIRONMENT Page 4 2.1 Location, Geology and Topography Page 4 2.2 The Nature of the Historic Environment Resource Page 4 2.3 The Island’s HEAP overview document Page 4 3.0 DEFINING MILITARY STATUS Page 5 4.0 ANALYSIS AND ASSESSMENT OF MILITARY/DEFENCE Page 5 ASSETS 4.1 Principle Historical Processes Page 5 4.2 Surviving Archaeology and Built Environment Page 7 4.3 Relationship with other HEAP Types Page 21 4.4 Contribution of Military/Defence Type to Isle of Wight Historic Page 22 Environment and Historic Landscape Character 4.5 Values, Perceptions and Associations Page 22 4.6 Resources Page 23 4.7 Accessibility and Enjoyment Page 24 4.8 Heritage Assets of Particular Significance Page 26 5.0 CONSERVATION AND MANAGEMENT Page 28 5.1 Forces for Change Page 28 5.2 Management Issues Page 30 5.3 Conservation Designation Page 31 6.0 FUTURE MANAGEMENT Page 33 7.0 GLOSSARY OF TERMS Page 34 8.0 REFERENCES Page 36 2 Iwight.com 1.0 INTRODUCTION The Isle of Wight Historic Environment Action Plan (HEAP) consists of a set of general documents, 15 HEAP Area Reports and a number of HEAP Type reports which are listed in the table below: General Documents HEAP Area Reports HEAP Type Reports HEAP Map of Areas Arreton Valley Agricultural Landscapes HEAP Introduction