Relevant bibliographies by topics / East Dover

Academic literature on the topic 'East Dover'

Author: Grafiati
Published: 10 December 2022
Last updated: 28 January 2023

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Journal articles on the topic "East Dover"

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Wallace, Lacey, and Alex Mullen. "Landscape, Monumentality and Expression of Group Identities in Iron Age and Roman East Kent." Britannia 50 (June 20, 2019): 75–108. http://dx.doi.org/10.1017/s0068113x19000308.

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ABSTRACTThe Canterbury Hinterland Project (CHP) has combined aerial photographic and LiDAR analysis, synthesis of HER and other data across east Kent with targeted survey south and east of Canterbury. We present possible hillforts, temples, large enclosures, a major trackway, linking paths, burials and high-status Roman-period complexes and argue that people organised the landscape to communicate meaning in two main ways: a ‘public’ face oriented towards the Dover–Canterbury road and expressions of ritual and remembrance for local groups. The character of this rural population has traditionally been understood in terms of its relationship to thecivitascapital and villas; we look beyond this to examine a more detailed vision of possible social interactions.
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Slate, Nico. "East Indian, West Indian: Colored Cosmopolitanism, World Literature, and the Dual Autobiography of Cedric Dover and Claude McKay." Modern Language Quarterly 76, no. 3 (August 18, 2015): 305–31. http://dx.doi.org/10.1215/00267929-2920042.

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Morooka, Fuki Saito, Hari Nugroho, Alan Handru, and Jun Ichi Kojima. "TAXONOMIC NOTES ON THE HOVER WASP GENUS EUSTENOGASTER (VESPIDAE, STENOGASTRINAE), WITH DESCRIPTION OF TWO NEW SPECIES FROM SUMATRA ISLAND, INDONESIA." TREUBIA 47, no. 2 (December 30, 2020): 133–54. http://dx.doi.org/10.14203/treubia.v47i2.4006.

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Wasps of the genus Eustenogaster van der Vecht, 1969, with 17 species currently recognized, are distributed from the Indian subcontinent in the west to the Philippines, Sulawesi Island and Java Island in the east. Two new species of hover wasp genus Eustenogaster (E. multifolia sp. nov., E. sumatraensis sp. nov.) are described from specimens collected in Sumatra Island. The female of E. vietnamensis occurring in Vietnam are described for the first time. The lectotypes of Paravespa eva Bell, 1936 and Ischnogaster ornatifrons Cameron, 1902 are designated. The new taxonomic status is proposed for Stenogaster eximioides Dover and Rao, 1922 as a good (=valid) species of Eustenogaster. The synonymy of Ischnogaster ornatifrons Cameron, 1902 with Eustenogaster micans (de Saussure, 1852) has been confirmed. A revised key to species and a taxonomic and distributional checklist of all the species of Eustenogaster are provided.
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Lee, John J., O. Roger Anderson, Bibi Karim, and Juhi Beri. "Additional Insight into the Structure and Biology of Abyssotherma pacifica (Brönnimann, Van Dover and Whittaker) from the East Pacific Rise." Micropaleontology 37, no. 3 (1991): 303. http://dx.doi.org/10.2307/1485892.

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Jeans, C. V., D. Long, M. A. Hall, D. J. Bland, and C. Cornford. "The geochemistry of the Plenus Marls at Dover, England: evidence of fluctuating oceanographic conditions and of glacial control during the development of the Cenomanian–Turonian δ13C anomaly." Geological Magazine 128, no. 6 (November 1991): 603–32. http://dx.doi.org/10.1017/s0016756800019725.

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AbstractThe sediments and organic calcite geochemistry (Fe2+, Mn2+, Sr, Mg, δ18O, δ13C) of the Plenus Marls at Dover (southeast England) reflect the changing oceanographic conditions associated with the development of the late Cenomanian-early Turonian S1SC excursion.The Plenus Marls of Dover consist of five marl-chalk couplets with a total thickness of up to 3 m. The sediments were deposited in an increasingly shallowing sea during a major regressional phase of the Chalk Sea over Europe. Each marl horizon was deposited in slightly cooler water of lower productivity and higher energy level than the overlying chalk, and represents a phase of enhanced regression. Inoceramus prisms and shell fragments from the marls have enhanced Mg values, whereas all the biogenic calcite from the chalks is enriched in Fe2+. The high clay content of the Plenus Marls probably originated from the post-depositional argillization of unstable silicate detritus (possibly of volcanoclastic origin) introduced into the regressing sea by rejuvenated river systems. The δ18O values of individual planktic and benthic foraminifera species have been lightened by diagenetic reaction; however they demonstrate (1) the presence of a constant temperature gradient in the water column with warmer surface waters relative to the bottom waters, and (2) the association of a marked temperature drop with the appearance of Jefferies' cold water occidental fauna and the development of a Mn2+ anomaly (Bed 5) in the average calcite skeletons of all particle size fractions. The δ13C values of individual planktic and benthic foraminifera species show that a normal oceanic gradient existed except at two levels (Beds 3, 5), where this is reversed with heavier values shown by the benthic forms. The normal δ13C gradient steepened rapidly as the water shallowed and the δ13C excursion reached maximum values. Dysaerobic and anaerobic water conditions were completely absent and the level of oxygenation (macrofaunal diversity) increased in parallel with the shallowing and the enhanced δ13C excursion.Comparison with the Plenus Marls section at Flixton (east Yorkshire), which shows evidence of restricted faunas and deposition under anoxic conditions (black bands rich in terrestrial organic matter), demonstrates that between these two localities there is unequivocal correlation of the δ13C excursion and the temperature drop associated with Jefferies' cold water occidental fauna. Anomalous geochemical features of the Dover Plenus Marls are explained by the redeposition of Flixton-type coccolith-rich chalk (very low Fe2+ content) and by the occasional introduction of cold northern bottom waters enriched in 13C.The status of the Cenomanian-Turonian oceanic anoxic event and its supporting evidence is discussed and is considered to be untenable on present evidence. An alternative hypothesis based upon a glacial mechanism is put forward; this is supported by evidence of widespread regression, restricted ocean circulation, lower ocean temperatures, enhanced input of terrestrial organic matter, and the presence of dropstones.
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Stoyle, Mark. "“The Gear Rout”: The Cornish Rising of 1648 and the Second Civil War." Albion 32, no. 1 (2000): 37–58. http://dx.doi.org/10.1017/s0095139000064206.

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In July 1648 John Bond, Master of the Savoy, delivered a thanksgiving sermon to the House of Commons, in which he praised God for the series of victories that the New Model Army had recently won in many parts of England and Wales. The tangled, multi-layered conflict known to posterity as the Second Civil War was still raging, rebel forces were holding out in Colchester and the Scottish army of the Engagement was marching south, but Bond—anxious to buoy up the Army’s allies and to cast down the spirits of its enemies—did everything he could to emphasise the universality of the recent successes. “The garment of gladnesse reacheth all over…the Land,” he declaimed, “the robe [of victory] reacheth from…Northumberland in the North, to…Sussex in the South…[and] from Dover…in the East, to Pensands, the utmost part of Cornwall, in the West.” Bond’s reference to Penzance would have struck a chord with many of his listeners, for accounts of an insurgent defeat in the little Cornish town had been read out in the House some weeks before. Yet, from that day to this, the rising at Penzance—and indeed the entire “Western dimension” of the Second Civil War have been largely forgotten.
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Bridgland, D. R., and P. L. Gibbard. "Quaternary River Diversions in the London Basin and the Eastern English Channel." Paléoréseaux hydrographiques quaternaires : centenaire W.M. Davis 51, no. 3 (November 30, 2007): 337–46. http://dx.doi.org/10.7202/033132ar.

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ABSTRACT The principal river of the London basin, the Thames, has experienced a number of course changes during the Quaternary. Some, at least, of these are known to result directly from glaciation. In the early Quaternary the river flowed to the north of London across East Anglia to the north coast of Norfolk. By the early Middle Pleistocene it had changed its course to flow eastwards near the Suffolk - Essex border into the southern North Sea. The Thames valley to the north of London was blocked by ice during the Anglian/Elsterian glaciation, causing a series of glacial lakes to form. Overflow of these lakes brought the river into its modern valley through London. It is thought that this valley already existed by the Anglian in the form of a tributary of the north-flowing River Medway, which joined the old Thames valley near Clacton. Also during the Anglian/Elsterian glaciation. British and continental ice masses are thought to have joined in the northern part of the North Sea basin, causing a large lake to form between the east coast of England and the Netherlands. It is widely believed that the overflow from this lake caused the first breach in the Weald-Artois Ridge, bringing about the formation of the Strait of Dover. Prior to the glaciation the Thames, in common with rivers from the continent (including the Rhine and Meuse), flowed into the North Sea Basin. It seems that, after the lake overflow, these rivers together drained southwards into the English Channel. Whether this southern drainage route was adopted during all later periods of low sea level remains to be determined, but it seems certain that this was the case during the last glacial.
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Esterik, Penny Van. "Health Planning and Community Participation: Case Studies in South-East Asia. By Susan B. Rifkin. Dover, N.H.: Croom Helm, 1985. xviii, 184 pp. Figures, Appendix, Bibliography, Index. $22.50." Journal of Asian Studies 45, no. 3 (May 1986): 659–60. http://dx.doi.org/10.2307/2056592.

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Stephan, J. J. "Book Reviews : Richard H. Solomon and Masataka Kosaka (eds), The Soviet Far East Military. Buildup: Nuclear Dilemmas and Asian Security. Dover, Massachusetts: Auburn House Publishing Company, 1986. 301 pp., maps, glossary, appendix; n.p." Journal of Asian and African Studies 22, no. 3-4 (January 1, 1987): 285–86. http://dx.doi.org/10.1177/002190968702200311.

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Kott, Tama I. "■ Guide to the Practical Study of Harmony. By Piotr Ilyich Tchaikovsky Translated by Emil Krall and James Leibling. Dover Publications, 31 East 2nd Street, Mineola, NY 11501; fax, 516-742-6953; www.doverpublications .com. 2005. 137 pp. Music examples. Paperback, $10.95." Music Educators Journal 93, no. 4 (March 2007): 18–19. http://dx.doi.org/10.1177/002743210709300406.

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Dissertations / Theses on the topic "East Dover"

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Slipper, Ian Jeffrey. "Turonian (Late Cretaceous) Ostracoda from Dover, south-east England." Thesis, University of Greenwich, 1997. http://gala.gre.ac.uk/6302/.

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Ostracod assemblages from samples collected through the Turonian Stage of the Late Cretaceous from Dover, Kent, south-east England, consist of one hundred and three species group taxa. These are described and illustrated. This represents a significant increase in the knowledge of the Turonian fauna, since previous estimates of the number of species present during the Turonian are less than thirty. This improvement has been brought about by the selection of an appropriate processing method. Freeze-thaw processing is recommended for chalks and hardgrounds which comprise much of the Turonian Stage. The white spirit, solvent method is shown to be preferable for marls. Nineteen species and six subspecies are here described as new: Polycope lunaplena sp. nov, Cytherella truncatoides sp. nov., Cytherella vulna sp. nov., Cytherella weaveri sp. nov., Cytherelloidea granulosa parca ssp. nov., Cardobairdia longitecta sp. nov., Bairdoppilata turonica sp. nov., Pontocyprella robusta cometa ssp. nov., Pterygocythereis (Diogmopteron) carolinae sp. nov., Bythoceratina (Bythoceratina) saxa sp. nov., Bythoceratina (Bythoceratina) staringi conmacula ssp. nov., Monoceratina minangulata sp. nov., Patellacythere weaveris sp. nov., Schulerides langdonensis sp. nov., Karsteneis nodifera tabasca ssp. nov., Karsteneis oculocosta sp. nov., Karsteneis petasus petasus sp. et ssp. nov., Karsteneis petasus antecursor sp. et ssp. nov., Karsteneis praekarsteni sp. nov., Idiocythere carburnensis sp. nov., Isocythereis postelongata sp. nov., Mauritsina? paradordoniensis sp. nov., Rehacythereis stellatus sp. nov., Rehacythereis venticursus venticursus sp. et ssp. nov., Rehacythereis venticursus patbrowni sp. et ssp. nov., and one new name, Bythoceratina (Bythocertatina) antetumida nom. nov. is introduced for a secondary junior homonym. By comparison with faunas from Devon and the Czech Republic, the biostratigraphical analysis is shown to only have only local significance due to diachronism of Ostracoda. This diachronism is used to explore migration pathways which suggest that the origin of the Turonian ostracod fauna may have had more than one source. A model relating ostracod diversity inversely to sea-level is given for the Cenomanian to Santonian stages of the Late Cretaceous which suggests that the sea-level at Dover during the Turonian was greater than previously thought, given its marginal setting.
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Jampol, Justinian. "Swords, doves, and flags : political symbols and their appropriation in the GDR 1949-1989." Thesis, University of Oxford, 2011. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.547764.

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Books on the topic "East Dover"

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Joan, Spence, ed. Harlem Valley pathways: Through Pawling, Dover, Amenia, North East, and Pine Plains. Charleston, SC: Arcadia, 1998.

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Great Britain. Hydrographic Dept. Dover Strait pilot: South-east coast of England, Bognor Regis to Southwold and north-west coast of Europe, Cap d'Antifer to Scheveningen. 2nd ed. [Taunton, Somerset]: Hydrographer of the Navy, 1985.

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Bachman, L. Joseph. Assessment of natural attenuation of contamination from three source areas in the east management unit, Dover Air Force Base, Kent County, Delaware. Baltimore, Md: U.S. Dept. of the Interior, U.S. Geological Survey, 1998.

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Dept, Great Britain Hydrographic. Dover Strait pilot: South-east coast of England, Bognor Regis to Southwold and north-west coast of Europe, Cap d'Antifer to Scheveningen. 2nd ed. [Taunton, Somerset]: Hydrographer of the Navy, 1985.

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Alexander, Kristen C. Ground-water sampling, analytical results, and water-level measurements at sites FT03, LF13, and WP14/LF15, East Management Unit, Dover Air Force Base, Delaware, January-October 2000. Baltimore, Md: U.S. Dept. of the Interior, U.S. Geological Survey, 2003.

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Helprin, Mark. A dove of the East, and other stories. San Diego: Harcourt Brace Jovanovich, 1990.

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GM Johnson & Associates Ltd. Dover/New Philadelphia/East Liverpool/Coshocton Street Map. GM Johnson & Associates Ltd., 2006.

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map, Ordnance Survey. Canterbury and East Kent, Dover and Margate (Landranger Maps). 2nd ed. Ordnance Survey, 1998.

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Canterbury and East Kent, Dover and Margate (Landranger Maps). 4th ed. Ordnance Survey, 2004.

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map, Ordnance Survey. Canterbury and East Kent, Dover and Margate (Landranger Maps). 2nd ed. Ordnance Survey, 1998.

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Book chapters on the topic "East Dover"

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Frankel, Refael. "Millstones, Mortars, and Stone Bowls from Tel Dover and the Southern Levant." In Stone Tools in the Ancient Near East and Egypt, 234–77. Archaeopress Publishing Ltd, 2019. http://dx.doi.org/10.2307/j.ctvndv6xd.21.

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Reid, Peter H. "Friends of Peppy." In Every Hill a Burial Place, 84–89. University Press of Kentucky, 2020. http://dx.doi.org/10.5810/kentucky/9780813179988.003.0012.

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Betty Clemmer attended Mt. Holyoke with Peppy. She and her husband, Dan, are teachers in Mwanza as part of the Teachers for East Africa Program. The Clemmers welcomed the Kinseys into their home and introduced them to me. During the weekend before Peppy died, the Clemmers stayed with the Kinseys in Maswa. The Clemmers saw a happily married couple. Aileen Dower and her husband, Hal, were in the same training group with Peppy and Bill. Although the Dowers are stationed on the other side of Mwanza, Peppy and Aileen often met for lunch in Mwanza, and Peppy sought out Aileen’s marriage experience to understand her own marriage problems.
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Miccoli, Dario. "Verso dove? Migrazioni geografiche e identitarie nella letteratura ebraica moderna." In Diaspore. Venice: Edizioni Ca' Foscari, 2020. http://dx.doi.org/10.30687/978-88-6969-396-0/024.

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This chapter discusses modern Hebrew literature – from early 20th-century authors like Haim Nahman Bialik and Shmuel Yosef Agnon to more recent ones, such as Erez Biton and Ronit Matalon – as a ‘migrant literature’, whose history is rooted in a set of shifting physical and cultural geographies and in the circulation of people, ideas and styles from the Diaspora to the Land of Israel and viceversa. By conceiving modern Hebrew literature as a ‘migrant literature’, it is possible to better understand its inner heterogeneity and multilingualism, as well as its being part of a wide landscape of ‘Jewish literatures’ that cuts across Europe, the Middle East and other spaces.
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Kelly, Matthew. "Sylvia Sayer." In The Women Who Saved the English Countryside, 233–317. Yale University Press, 2022. http://dx.doi.org/10.12987/yale/9780300232240.003.0005.

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This chapter follows the early life of Sylvia Sayer, noting that she was not born into such grandeur as Pauline Dower, but she was firmly placed within the English middle classes. It emphasizes that she inherited her political commitments from her grandfather, Robert Burnard, but her social standing and the ease with which she dealt with male officials surely reflected the record of distinguished naval service on her father's side. The chapter also elaborates on the subject of Sayer's letter to Sir Patrick Duff, chair of the National Parks Commission, which was the need to expedite the designation of Dartmoor National Park. The chapter then considers Sayer's preservationism and her belief that Dartmoor's natural characteristics gave it an essential purpose as grazing land or pasture, primarily pursued through the exercise of common rights, which had to be protected at all cost. The chapter concludes by reviewing how Sayer opposed virtually all forms of enclosure or disturbance to the existing surface of the moor. Sayer believed Dartmoor provided a single essential resource — rough grazing — and with it benefits to the public — health and happiness — and it should not be exploited in any other way.
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"10. Revolt of the Doves: The Movement in the Pacific, Asia, Africa, the Near and Middle East, Latin America, and Eastern Europe, 1981-85." In Toward Nuclear Abolition, 202–25. Stanford University Press, 2003. http://dx.doi.org/10.1515/9781503624320-012.

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Hoyt, Douglas V., and Kenneth H. Shatten. "Variations in Solar Brightness." In The Role of the Sun in Climate Change. Oxford University Press, 1997. http://dx.doi.org/10.1093/oso/9780195094138.003.0006.

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In the last chapter we saw that sunspots, aurorae, and geomagnetic disturbances vary in an 11-year cycle. So do many other solar features, including faculae and plages, which are bright regions seen in visible and monochromatic light, respectively. If both bright faculae and dark sunspots follow 11-year cycles, does this mean the sun’s total light output varies? Or are these two contrasting features balanced so that the sun’s output of light remains constant? The light output of the sun is often discussed in two different ways: either as the solar luminosity, which is the sun’s omnidirectional radiant output, or as the solar constant, the output seen in the direction of the Earth. In this chapter, we explore the variable solar light output that has been the subject of vigorous discussions. The total solar irradiance or solar constant is defined as the total radiant power passing through a unit area at Earth’s mean orbital distance of 1 astronomical unit. Today the most common units of solar irradiance are watts per square meter (W/m2). Power is defined as energy per unit time, so the solar irradiance can also be expressed in calories per square centimeter per minute. Modern experiments indicate that the sun’s radiant output is about 1367 W/m2, with an uncertainty of about 4 W/m2. About 150 years of effort by many people have been required to establish the value to this accuracy. The sun’s radiant output is not an easy quantity to measure, and we will discuss some of the struggles required to measure it. In the late 1800s, many scientists considered the solar total irradiance or solar irradiance to be constant. Oceanographers Dove and Maury vigorously supported this viewpoint, so the solar irradiance was called the solar constant. For the next century, virtually every paper concerning the sun’s radiant output used the term solar constant. No physical justification for this nomenclature existed, only a philosophical bias. Yet by the 1950s this bias proved so strong and so prevalent that support for individuals who wished to measure variations in the solar constant became almost nonexistent.
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Conference papers on the topic "East Dover"

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McQuiggan, Rachel, Mary Hingst, A. Scott Andres, Changming He, Chelsea Peters, and Holly A. Michael. "INVESTIGATING THE DYNAMICS OF COASTAL GROUNDWATER SALINIZATION IN EAST DOVER, DELAWARE." In Joint 69th Annual Southeastern / 55th Annual Northeastern GSA Section Meeting - 2020. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020se-343132.

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Reports on the topic "East Dover"

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Assessment of natural attenuation of contamination from three source areas in the East Management Unit, Dover Air Force Base, Kent County, Delaware. US Geological Survey, 1998. http://dx.doi.org/10.3133/wri984153.

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