Reconstructing the Recent Wind Erosion History of a Field in East Anglia, UK.

2013 ◽  
Author(s):  
Dr. Adrian Chappell ◽  
Dr. Andrew D. Thomas
1902 ◽  
Vol 9 (9) ◽  
pp. 385-388 ◽  
Author(s):  
E. T. Newton

The history of this gigantic rodent began to be written in 1809, when M. Gothelf Fischer described a skull from a sandy deposit on the borders of the Sea of Azof, to which he gave the name of Trogontherium. Since then, at varying intervals, to the present time, new chapters have been added to this history by both Continental and British workers, describing specimens of a more or less fragmentary character which have from time to time been discovered. The English specimens have been chiefly obtained from the ‘Cromer Forest Bed,’ that rich and remarkable series of beds occupying a position in time between the Crags and the Glacial deposits of East Anglia. The ‘Forest Bed’ specimens were first made known by Sir Charles Lyell in 1840, but were more fully described by Sir R. Owen in 1846 and referred to Fischer's Trogontherium Cuvieri. It will not be necessary at this time to refer specifically to each of the additions to our knowledge of this animal or to detail the varying opinions as to affinities and nomenclature, as these particulars will be found in the Memoirs of the Geological Survey of the United Kingdom. Although most of the British specimens of Trogontherium Cuvieri have been found in the ‘Cromer Forest Bed’ a few examples have been met with in the Norwich and Weybourn Crags. The smaller species, which has been called T. minus, was obtained from the nodule bed below the Red Crag of Felixstowe, and an incisor tooth from the Norwich Crag was referred to the same species.


Elements ◽  
2007 ◽  
Vol 3 (1) ◽  
Author(s):  
Dmitri Phillips

The history of England did not begin with the Industrial Revolution and not everything supposed about the Anglo-Saxons reduces to the myth of King Arthur and the Round Table. Contrary to commonly held beliefs, the Dark Ages of the North were full of splendor and brilliance; the only thing dark about them is their enshrouded history, but that only makes them all the more fascinating. The great burial mound at Sutton Hoo in East Anglia, discovered just before World War II, shines as one of the most grandiose sepulchers in history, yet the identity of its occupant remains a mystery. Was it a wealthy merchant, a warrior from overseas, or a great king? This paper gathers, presents, and scrutinizes the evidence and arguments from ancient records, opulate grave-goods, and contemporary investigations in an attempt to determine the most likely candidate for the individual interred in Mound 1 at Sutton Hoo.


2007 ◽  
Vol 31 (3) ◽  
pp. 140-148
Author(s):  
Jurgis Bučas

The Curonian Spit was inhabited six thousand years ago. During this period its survival was menaced by natural forces. The 17th–18th centuries faced unreasonable deforestation of the Curonian Spit and opened its dunes to wind erosion. In the 18th century 14 settlements were hid under moving sand. The Spit survival was in danger of being flown under the Curonian Lagoon waters. At the begining of the 19th century radical actions were taken to save the Curonian Spit damaged by wind erosion. Tremendous ecological awareness of some natural powers as wind and flora helped man to create a landscape which was described at UNESCO General Conference as a worldwide worth cultural heritage and enrolled in the World Heritage List as a cultural landscape of universal worth illustrating the history of dramatic coexistence of nature and man. The paper describes the Curonian Spit as a cultural landscape, its historical formation and present managment, discusses its creation and management traditions and evaluates them while preparing the Curonian Spit National Park managment plan as well as the Master Plan of Neringa city. Gamtosauginė direktyva ar kraštotvarkinės tradicijos ? Santrauka Kuršių nerijoje žmonės įsikūrė ketvirtajame tūkstantmetyje prieš Kristų. Visą istorinį laikotarpį pusiasaliui grėsmę kėlė gamtos jėgos. XVI-XVIII a. neapgalvotas nerijos miškų naikinimas atidengė pusiasalio smėlynus vėjo erozijai. XVIII a. smėliu užpustyta 14 gyvenviečių. Kilo grėsmė, kad ir pats pusiasalis bus nupustytas į Kuršių marias. Pasitinkant XIX a., imtasi radikalių priemonių gelbėti vėjo erozijos naikinamą Kuršių neriją. Su didžiule ekologine išmintimi panaudodamas pačios gamtos jėgą (vėją) ir medžiagą (augalus), per XIX a. supustyto jūros smėlio kopose žmogus sukūrė kraštovaizdį, kuris UNESCO Generalinės konferencijos buvo įvardytas pasaulio reikšmės nekilnojamojo kultūros paveldo vertybe ir įrašytas į Pasaulio paveldo sąrašą kaip universalios reikšmės kultūrinis kraštovaizdis, iliustruojantis gamtos ir žmogaus dramatiško sambūvio istoriją. Nagrinėjama Kuršių nerijos kultūrinio kraštovaizdžio istorinio formavimo ir dabartinio jo tvarkymo veikla, aptariamos jo kūrimo bei priežiūros tradicijos ir kaip jos vertinimos rengiant Kuršių nerijos nacionalinio parko tvarkymo planą bei Neringos miesto savivaldybės bendrąjį planą.


2019 ◽  
Vol 85 ◽  
pp. 61-81 ◽  
Author(s):  
Mark White ◽  
Nick Ashton ◽  
David Bridgland

A better understood chronological framework for the Middle Pleistocene of Britain has enabled archaeologists to detect a number of temporally-restricted assemblage-types, based not on ‘culture historical’ schemes of typological progression but on independent dating methods and secure stratigraphic frameworks, especially river-terrace sequences. This includes a consistent pattern in the timing of Clactonian and Levalloisian industries, as well as a number of handaxe assemblage types that belong to different interglacial cycles. In other words, Derek Roe’s hunch that the apparent lack of coherent ‘cultural’ patterning was due to an inaccurate and inadequate chronological framework was correct. Some variation in handaxe shape is culturally significant. Here we focus on twisted ovate handaxes, which we have previously argued to belong predominantly to MIS 11. Recent discoveries have enabled us to refine our correlations. Twisted ovate assemblages are found in different regions of Britain in different substages of MIS 11 (East Anglia in MIS 11c and south of the Thames in MIS 11a), the Thames, and the MIS 11b cold interval separating the two occurrences. These patterns have the potential to reveal much about hominin settlement patterns, behaviour, and social networks during the Middle Pleistocene.


2016 ◽  
Vol 446 ◽  
pp. 33-53 ◽  
Author(s):  
Nicolas J. Bonnet ◽  
Anicet Beauvais ◽  
Nicolas Arnaud ◽  
Dominique Chardon ◽  
Mudlappa Jayananda

1979 ◽  
Vol 45 ◽  
pp. 165-178 ◽  
Author(s):  
P. R. Sealey

Torcs made from the gold/silver alloy known as electrum are among the most striking features of British Iron Age craftsmanship; yet despite the interest they generate, little effort has been directed towards unravelling the problems of their development. This paper seeks to correct this neglect by considering the reasons for the decline of electrum torc art, with particular reference to those found in East Anglia.


2020 ◽  
Author(s):  
Karina Marques ◽  
Thierry Allard ◽  
Guillaume Morin ◽  
Benoît Baptiste ◽  
Cécile Gautheron ◽  
...  

<p>Ferruginous duricrusts record a part of the Earth’s geodynamical and climatic history in tropical area, because they can be formed over a wide geologic period. However, the events and processes related to their formation, transformation and distribution are still obscure. This is mainly due to the complexity arising from their finely divided and polycrystalline nature together with the coexistence of various generations of supergene minerals, such as iron and aluminum oxides, oxyhydroxides or hydroxides (e.g. goethite, hematite and gibbsite) and kaolinite, even at microscopic scale. Classical mineralogical investigations are often realized using powders samples, which hinders subsequent analyses on the same sample, such as SEM or (U-Th)/He dating. Thus, the aim of this study was to propose a new way to investigate the mineralogy of supergene ferruginous samples on micrometric grains that will be analyzed by (U-Th)/He dating method. Prior to this analysis, we first compare the X-ray diffraction data of grains and small amounts of powders looking to reveal the mineralogical composition of populations of secondary minerals of a ferruginous duricrust by taking into account the heterogeneity of the material. Samples were collected from a ferruginous duricrust with pisolitic structure developed over epiclastic conglomerates and sandstones deposited by alluvial fan and fluvial streams from the Upper Cretaceous at the western Minas Gerais state (Brazil). The geomorphology of the study area is delineated by remnants of paleosurface (up to 1,000 m a.s.l.), which comprises an important record of long-term Brazilian continental history.Macroscopic facies recognized on duricrusts sections were described, which allowed the identification of various populations of secondary minerals. After this detailed description, grains (size < 0.5 mm) were collected and powder samples of each population were prepared by crushing. Overall, the results point out that the grain and powder samples could be used to identify mineralogical composition at fine resolution of secondary minerals from ferruginous duricrusts. In addition, XRD results are similar for both types of sample preparation, however the < 0.5 mm grain samples are more advantageous because they are not destructive and thus allow to get a finer description of the mineralogy of different populations and can subsequently be used for e.g. (U-Th)/He dating, providing critical information for interpreting and discussing the ages of iron oxides.</p><p><strong>Grant:</strong> 19/10708-7; 17/22292-4; 17/20788-2, São Paulo Research Foundation (FAPESP)</p><p><strong>References</strong></p><p>Allard, T., Gautheron, C., Riffel, S.B., Balan, E., Soares, B.F., Pinna-Jamme, R., Derycke, A., Morin G., Bueno, G.T., Nascimento, N., 2018. Combined dating of goethites and kaolinites from ferruginous duricrusts. Deciphering the Late Neogene erosion history of Central Amazonia. Chemical Geology 479, 136-150.</p><p>Monteiro, H.S., Vasconcelos, P.M.P., Farley, K.A., Spier, C.A., Mello, C.L., 2014. (U-Th)/He geochronology of goethite and the origin and evolution of cangas. Geochim. Cosmochim. Acta  131, 267–289.</p><p>Vasconcelos, P.M., Heim, J.A., Farley, K.A., Monteiro, H.S., Waltenberg, K., 2013. <sup>40</sup>Ar/<sup>39</sup>Ar and (U–Th)/He - <sup>4</sup>He/<sup>3</sup>He geochronology of landscape evolution and channel irondeposit genesis at LynnPeak, Western, Australia. Geochim. Cosmochim. Acta 117, 283-312.</p>


Terra Nova ◽  
2000 ◽  
Vol 12 (4) ◽  
pp. 163-170 ◽  
Author(s):  
C. Spiegel ◽  
J. Kuhlemann ◽  
I. Dunkl ◽  
W. Frisch ◽  
H. von Eynatten ◽  
...  

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