Disaster information: a bibliography
Exchange of notes between the government of U.K. and U.S.A. relating to the establishment of hurricane research stations in Jamaica and Grand Cayman
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ID: 147 Ti: Exchange of notes between the government of U.K. and U.S.A. relating to the establishment of hurricane research stations in Jamaica and Grand Cayman. Pub: London; Her Majesty's Stationery Office; 1960. 5. Lo: Jamaica, Ministry of Agriculture. ID: 148 Au: Turbott, I. G. Ti: Report on Hurricane Donna as it affected the territory of Antigua. Pub: Antigua; The Administrator of Antigua; 1960. Lo: UWI, Mona, Science Library.
Au: Versey, H. R. Ti: The hydrologic character of the white limestone formation of Jamaica. Pub: Mayaguez; University of Puerto Rico; 1960. 59-68. Co: Transactions of the Second Caribbean Geological Conference; Mayaguez, 4-9, Jan. 1959. Lo: UWI, Mona, Science Library. ID: 150 Au: Robinson, Edward; Versey, H. R; Williams, J. B. Ti: The Jamaica Earthquake of March 1, 1957. So: In:Transactions of the 2nd Caribbean Geological Conference. Mayaguez, University of Puerto Rico, 1960. 50-7. Co: Second Caribbean Geological Conference; Mayaguez, 4-9, Jan. 1959. Lo: UWI, Mona, Science Library. ID: 151 Ti: Before and after hurricane precautions to take. So: The Farmer; 64(7&8):200-1, Jul. – Aug. 1960. Lo: UWI, Mona, Science Library. ID: 152 Au: Skeete, Cecil C. Ti: A historical discription of the weather of the island of Barbados. Pub: sl; sn; 1961. Lo: UWI, Mona, Science Library.
Au: Jamaica. Geological Survey Department. Ti: Annual report of the Geological Survey Department for the finincial year 1959-60. Pub: Kingston; Geological Survey Department; 1961. 32. Lo: UWI, Mona, Science Library.
Au: Kirkpatrick, William. Ti: The Water Commission (Corporate Area) Kingston Ja. W.I. Pub: Kingston; Water Commission; 1961. 66. Lo: Jamaica, Jamaica Information Service; UWI, Mona, Science Library.
Au: Wernstedt, Frederick. Ti: World climatic data: Latin America and the Caribbean. Pub: sl; sn; 1961. Lo: UWI, Mona, Science Library.
Au: Robson, G. R. Ti: Earthquake series in St. Kitts - Nevis 1961-62. So: Nature; 195(4845): 972-4, 1962. Lo: Jamaica, Ministry of Agriculture; UWI, Mona, Science Library.
Au: Coastal water quality improvement project. Ti: Resource guide to coral reef educational material available in Jamaica Pub: Kingston; Jamaica; 1999. 271. Lo: UWI, Mona, Science Library.
Au: Williams, J. B. Ti: Earthquakes and their incidence and measurement in Jamaica. So: Information Bulletin of the Scientific Reaserch Council, Jamaica; 3(1-4):21-25, Jun. 1962- Mar. 1963. Lo: UWI, Mona, Science Library.
Au: Channon, J. A. Ti: The forecasting of hurricanes. So: Information Bulletin of the Scientific Reaserch Council, Jamaica; 3(1-4):1-5, Jun. 1962 - Mar. 1963. Lo: UWI, Mona, Science Library.
Au: Jamaica. Geological Survey Department. Ti: Synopsis of the geology of Jamaica. So: Kingston; Geological Survey Department; 1962. 72 Lo: Jamaica, National Library of Jamaica
Ti: Stopping hillside erosion at James Hill. So: The Farmer; 67(7-9):203-4, Jul. – Sept. 1962. Lo: UWI, Mona, Science Library. ID: 162 Au: Jamaica. Geological Survey Department. Ti: Annual report of the Geological Survey Department for the year ended 31st March, 1962. So: Kingston; Geological Survey Department; 1963. 22 Lo: UWI, Mona, Science Library.
Au: Geological Survey Department. Ti: Seismic unit. So: In: Geological Survey Department. Annual Report of the Geological Survey Department for the year ended 31st March, 1962. Kingston, Geological Survey Department, 1963. 22. Lo: UWI, Mona, Science Library.
Au: Cairn, Ernest E. Ti: Cyclone Hattie. Pub:Devon; Stockwell Ltd; 1963. 75. Lo: Jamaica, Ministry of Agriculture.
Ti: Hurricane damage. So: Caribbean Agriculture; 1(4): 1. 1963. Lo: UWI, Mona, Science Library. ID: 166 Ti: The Tobago hurricane and after. So: Journal of the Agricultural Society of Trinidad & Tobago; 63(3): 265-367, Sept. 1963. Lo: UWI, Mona, Science Library. ID: 167 Au: Jamaica. Scientific Resaerch Council Ti: The rainfall of Jamaica. Scientific Research Council Jamaica; November 1963. Lo: UWI, Mona, Science Library. ID: 168 Au: Nancoo, M. E. Ti: Hurricanes and flora. So: Bulletin of the Scientific Research Council, Jamaica; 4(3):45-9, Dec. 1963. Lo: UWI, Mona, Science Library.
Au: Jamaica.Geological Survey Department. Ti: Annual report of the Geological Survey Department for the year ended March 31st 1963. So: Kingston; Geological Survey Department; 1964. 17. Lo: UWI, Mona, Science Library.
Au: Williams, J. B. Ti: Harbour View Housing Scheme. So: In: Geological Survey Department. Annual Report of the Geological Survey Department for the year ended March 31st 1963. Kingston, Geological Survey Department, 1964. 15-6. Lo: UWI, Mona, Science Library.
Au: Williams, J. B. Ti: Hopewell land settlement St. Mary. So: In: Geological Survey Department., Annual Report of the Geological Survey Department for the year ended March 31st 1963. Kingston, Geological Survey Department, 1964. 17. Lo: UWI, Mona, Science Library.
Ti: Hurricane Flora: excerpts from Dunn & Miller. Hurricanes of the 20th century. Pub: Baton Rouge; L.S.U. Press; 1964. Lo: Jamaica, Office of Disaster Preparedness and Emergency Management. ID: 173 Au: Jamaica. Negril Area Environmental Protection Trust. Environmental Plan Task Force. Ti: Negril watershed environmental protection area plan. Pub: Negril; NAEPT; 1964. 86. Lo: Jamaica, Natural Resources Conservation Department.
Au: Robson, G. R. Ti: An earthquake catalogue for the Eastern Caribbean 1530-1960. So: Bulletin of the Seismological Society of America; 54(2), Apr. 1964. Lo: UWI, Mona, Science Library.
Au: Sykes, Lynn R; Ewing, Maurice. Ti: The seismicity of the Caribbean region. So: Journal of Geophysical Research; 70(20):5065-74, 15, Oct. 1965. Ab: The hypocenters of appoximately 500 Caribbean earthquakes were relocated using a digital computer. Since a large number of epicenters can now be located with an accuracy of about 10 km, the spatial distribution of earthquakes can be used in detailed investigations of the tectonics of deep-sea atrenches, fault zones and island arcs. A nearly continuous belt of shallow-focus seismicity can be traced from Central America to the Greater and Lesser Antilles and then to northeastern Venezuela. Intense sources of seismic activity are apparently associated with the El Pilar and Bocono fault zones. This study indicated a gap in the seismicity of northern South America between longitudes 64.5oW and 69oW. In addition to this area, several other segments of island arcs have acted as distinct tectonic units. These units are often bounded by major transverse features. About 30 percent of the events reported in this study were assigned focal depths greater than 70 km; earthquakes having depths as great as 200 km were detected. A zone of intermediate-depth earthquakes can be traced along the entire length of the Lesser Antilles. Most of the hypocenters in the Lesser Antilles are confined to a zone about 50 km wide which dips about 60oW. An intense source of intermediate earthquakes is located beneath the eastern end of Hispaniola. Much of the shallow-focus activity in the vicinity of the Puerto Rico trench is located beneath the south wall of the trench. Some activity was detected in the Puerto Rico trench itself, and several epicenters are associated with structural elements which strike WNW. Earthquake epicenters near the Virgin Islands indicate that the Anegada fault zone may be at least 400 km long. Lo: UWI, Mona, Science Library. ID: 176 Au: Robson, G. R. Ti: An introduction to earthquakes and earthquake risk in Jamaica. Pub: St. Augustine; University of the West Indies. Seismic Research Unit; 1965. Lo: UWI, Mona, Science Library.
Au: Hill, V. G. Ti: Factors affecting the strength and durability of stabilised earth (cinva ram) block structures in Jamaica. Pub: Kingston; Scientific Research Council; 1965. 24. (Technical Report, 2/65). Lo: Jamaica, National Library of Jamaica. ID: 178 Au: Andrew, E. M. Ti: Seismic surveys over river gravels in Jamaica, May - August 1964. Pub: London; Great Britain. Geophysical Division, Overseas Geological Surveys; 1965. 7. (Geophysical Reports, 28). Lo: Jamaica, National Library of Jamaica.
Ti: Hurricane precautions, advice to banana growers. So: The Farmer; 70(7-8): 207, Jul. – Aug. 1965. Lo: UWI, Mona, Science Library. ID: 180 Au: Monroe, Watson H. Ti: Formation of tropical karst topography by limestone solution and reprecipitation. So: Caribbean Journal of Science; 6(1-2):1-7, Mar. – Jun. 1966. Lo: UWI, Mona, Science Library.
Au: Hill, V. G; Taylor, W. A. Ti: A study of the effects of industrial waste on the oxygen values of the Rio Cobre. Pub:Kingston; Scientific Research Council; 1966. 13. (Scientific Research Council. Technical Report, 1/66). Ab: An investigation into the effects of pollution of the Rio Cobre by industrial efforts from the citrus processing plant, milk condensary, and the sugar factory was carried out over the period June 1962 to March 1966. The chemical oxygen demand (COD), biochemical oxygen (BOD) and dissolved oxygen (DO) content of the river water and the effluents were used as parameters of the state of pollution of the river and the polluting characteristics of the effluents. Lo: Jamaica, National Library of Jamaica; UWI, Mona, Science Library.
Au: Higuera-Gundy, Antonia; Brenner, Mark; Hodell, David A; Curtis, Jason H; Leyden, Barbara W; Binford, Michael. Ti: A 10300 C14 yr record of climate and vegetation change from Haiti. So: Quaternary Research; 52 :157-70, 1999. Ab: Pleistocene and Holecene vegetation dynamics in the American tropics are inferred largely from pollen in continental lake sediments. Maritime influences may have moderated climate and vegetation changes on Caribbean islands. Stable isotope (delta O-18) study of a 7.6m core from lake Miragoane, Haiti provided a high-resolution record of changing evaporation/precipitation (E/P) since 10300 C-14 yr B.P. The Miragoane pollen record documents climate influences and human impacts on vegetation in Hispaniola. The delta O-18 and pollen data near the base of the core indicate cool dry conditions before 10000 C-14 yr B.P. Lake Miragoane filled with water in the early Holocene as E/P declined the fresh water acquifer rose Despite increasing early Holocene moisture, shrubby, xeric vegetation persisted. Forest expanded 7000 C-14 yr B.P. in response to greater effective moisture and warming. The middle Holocene (7000-3200 C-14 yr B.P.) was characterized by high lake level and greater relative abundance of pollen from moist forest taxa. Climatic drying that began 3200 C-14 yr B.P. may have driven some mesophilic animal species to extinction. The pollen record of the last millennium reflects pre-Columbian (Taino) and European deforestation. Long-term, Holocene vegetation trends in southern Haiti are comparable to trends from continental, lowland circum-Caribbean sites, suggesting a common response to regional climate change. Lo: UWI, Mona, Science Library. ID: 183 Au: Robson, G. R. Ti: Action to be taken in the event of an earthquake or volcanic eruption in the West Indies. Pub: St. Augustine; University of the West Indies. Seismic Research Unit; 1966. 6. Lo: Jamaica, National Library of Jamaica.
Au: Martin-Kaye, P; Badcock, J. Ti: Geological background to soil conservation and land rehabilitation measures in Barbados, W.I. Pub: Kingston; Geological Survey Department; 1966. 131-5. Co: Transactions of the Third Caribbean Geological Conference; Kingston, 2-11, Apr. 1962. Lo: UWI, Mona, Science Library. ID: 185 Au: Perelli, Richard J. Ti: Geology and ore occurences at Mavis Bank, parish of St. Andrew, Jamaica. Pub: Kingston; Geological Survey Department; 1966. 122-3. Co: Transactions of the Third Caribbean Geological Conference; Kingston, 2-11, Apr. 1962. Lo: UWI, Mona, Science Library. ID: 186 Au: Reed, A. J. Ti: Geology of the Bog Walk quadrangle, Jamaica. Pub: Kingston; Geological Survey Department; 1966. 54. Lo: UWI, Mona, Science Library.
Au: Jamaica. Scientific Research Council. Ti: Good building practice prevents hurricane damage: a report on the effects of Hurricane Betsy. Pub:Kingston ; Scientific Research Council; 1966. 5. Ab: When Betsy, winds of which reached a velocity of 85 knots, struck Nassau in Sept. 1985, the damage to buildings was surprisingly little. Investigations disclosed that the rigid regulations adhered to in building construction, the distribution of the reinforcing material in the structures, the care taken in ensuring the adequacy of pins and drapes to wooden and concrete structures and the prompt and efficient manner in which the population reacted to hurricane warnings were responsible for the lack of destruction. The damage that did occur was caused mainly by occasional lack of attention to important details of construction, by falling trees and by the lifting of badly laid asphalt shingles from the roofs. The report includes recommendations which aim at improving building techniques and standard controls in Jamaica. Lo: UWI, Mona, Science Library. ID: 188 Au: Weaver, John D. Ti: Higher level erosion surfaces in the Caribbean. Pub: Kingston; Geological Survey Department; 1966. 10-2 Co: 3rd Caribbean Geological Conference; Kingston, 2-11, Apr. 1962. Lo: UWI, Mona, Science Library. ID: 189 Au: Trinidad & Tobago. Office of the Prime Minister. Ti: Tobago hurricane of 1847. Pub: Port of Spain; Government Printery; 1966. Lo: Jamaica, National Library of Jamaica.
Au: Robson, G. R. Ti: Earthquakes in Jamaica. So: Bulletin of the Scientific Research Council; 29-44, Sept. 1966. Lo: UWI, Mona, Science Library.
Au: Robson, G. R. Ti: Report and correspondence on the St. Kitts- Nevis earthquakes of 1961-1963. Pub: St. Augustine; University of the West Indies. Seismic Research Unit; 1967. Lo: Jamaica, National Library of Jamaica.
Au: Ireland, C. C. McArthur. Ti: Hurricanes. So: Jamaica Journal; 1(1), 1967. Lo: UWI, Mona, Science Library.
Au: Weyl, R. Ti: Volcanoes and volcanic rocks in Central America and the West Indies. So: Bulletin Volcanologique, Tome; 31: 3-12, 1967. Lo: Jamaica, Geological Survey Division.
Au: Smith, G. W. Ti: A nomogram for estimating - soil moisture deficits. Pub: Kingston; Scientific Research Council; 1967. 28-41. Co: U.W.I. Conference on Climatology & Related Fields; Kingston, Sept. 1966. Lo: UWI, Mona, Science Library. ID: 195 Au: Wint, J. McL. Ti: Hurricane precautions for tropical buildings. Pub: Kingston; Scientific Research Council; 1967. 91-102 Co: U.W.I. Conference on Climatology & Related Fields; Kingston, Sept. 1966. Lo: UWI, Mona, Science Library. ID: 196 Au: Helm, Thomas. Ti: Hurricanes; weather at its worst. Pub: New York; Dodd, Mead & Co.; 1967. Lo: UWI, Mona, Science Library.
Au: Robson, G. R; Barr, K. G. Ti: Report on investigation of Dominica tremors of 1959-60. Pub: St. Augustine; University of the West Indies. Seismic Research Unit; 1967. 17. Lo: Jamaica, National Library of Jamaica.
Au: Eyre, L. Alan. Ti: The concept of water surplus and water deficit and its usefulness in Caribbean climatology. Pub: Kingston; Scientific Research Council; 1967. 24-7. Co: U.W.I. Conference on Climatology & Related Fields; Kingston, September 1966. Lo: UWI, Mona, Science Library. ID: 199 Au: Simpson, R. W. Ti: The hydrological investigation of the Yallahs catchment. Pub: Kingston; Scientific Research Council; 1967. 64-8. Co: U.W.I. Conference on Climatology & Related Fields; Kingston, September 1966. Lo: UWI, Mona, Science Library. ID: 200 Au: Vickers, D. O. Ti: Very heavy and intense rainfall in Jamaica. Pub: Kingston; Scientific Research Council; 1967. 57-63. Co: U.W.I. Conference on Climatology and related fields; Kingston, 20-22 Sept. 1966. Lo: UWI, Mona, Science Library. ID: 201 Au: Marx, Robert F. Ti: The last day of Port Royal. So: Jamaica Journal; 1(1):16-20, Dec. 1967. Lo: UWI, Mona, Science Library.
Au: Shepherd, John B. Ti: Earthquake in Jamaica. So: Jamaica Journal; 2(1):36-40, Mar. 1968. Lo: UWI, Mona, Science Library.
Au: St. Lucia. Office of Disaster Preparedness. Ti: Disaster preparedness. So: Disaster Preparedness News; 1(1): 1999. Lo: St Lucia., Hunter J. Francois Library.
Au: Eyre, L. Alan. Ti: Precipitation from Hurricane Flora, 1963. So: Journal of Tropical Geography; 26: 29-36, 1968. Lo: UWI, Mona, Science Library.
Au: Potter, H. C. Ti: A preliminary account of the stratigraphy and structure of the eastern part of the Northern Range, Trinidad. Pub: Armina; Caribbean Printers; 1968. 15-20. Co: Transactions of the Fourth Caribbean Geological Conference; Port of Spain, 28, Mar. – 12, Apr. 1965. Lo: UWI, Mona, Science Library. ID: 206 Au: Burke, K; Coates, A. G; Robinson, Edward. Ti: Geology of the Benbow Inlier and surrounding areas, Jamaica. Pub: Arima; Caribbean Printers; 1968. 299-308. Co: Transactions of the Fourth Caribbean Geological Conference ; Port of Spain, 28, Mar.- 12, Apr. 1965. Lo: UWI, Mona, Science Library. ID: 207 Au: Millas, Jose Carlos. Ti: Hurricanes of the Caribbean & adjacent regions, 1492-1800. Pub: Miami; Academy of the Arts & Science of America; 1968. Lo: Jamaica, National Library of Jamaica.
Au: Kugler, H. G. Ti: Sedimentary volcanism. Pub: Armina; Caribbean Printers; 1968. 11-13. Co: Transactions of the Fourth Caribbean Geological Conference; Port of Spain, 28, Mar. – 12, Apr. 1965. Lo: UWI, Mona, Science Library. ID: 209 Au: Coates, A. G. Ti: The geology of the cretaceous central inlier around Arthurs Seat, Clarendon, Jamaica. Pub: Arima; Caribbean Printers; 1968. 309-15. Co: Fourth Caribbean Geological Conference; Port of Spain, 28, Mar. – 12, Apr. 1965. Lo: UWI, Mona, Science Library. ID: 210 Au: Baker, P. E. Ti: The geology of Mt. Misery Volcano, St. Kitts. So: In: Saunders, John B. ed. Transactions of the Fourth Caribbean Geological Conference. Arima, Caribbean Printers, 1968. 361-365. Co: Transactions of the Fourth Caribbean Geological Conference; Port-of-Spain, 28, Mar. – 12, Apr. 1965. Ab: Mt. Misery is the youngest of the four main volcanic centres on St. Kitts. It is a typical strato-volcano with a relatively steep central cone, rising to 3,792 ft. above sea level flanked by a gently sloping piedmont. There is a well preserved summit crater with traces of a somma rim around it. Associated with the volcano are four volcanic domes and two small explosion craters. Pleistocene limestone has been uplifted on the sides of the youngest dome, Brimstone Hill. Among the more recent products of the volcano are the Mansion pyroclastics which consist chiefly of greenish-gray andesitic lapilli, andesitic pumice and basaltic cinders: a few basaltic lavas intervene locally in the pyroclastic sequence. Although the maximum thickness of the pyroclastics is now only about 50 ft. the original thickness probably exceeded 130 ft. on the western side of the island. Investigations of thickness, grain size distribution and sorting indicate that they are pyroclastic-fall deposits erupted from the summit crater of Mt. Misery and distributed under the influence of a prevailing easterly wind. A small group of volcanic dusts termed the Steel Dust Series lie above the Mansion Series but are restricted to the lower western slopes of Mt. Misery. Mudflow deposits, some more recent than the Steel Dust Series, are extensively distributed on the piedmont. Isolated reports of eruptions in 1692 and 1843 are unsubstantiated but mild fumarolic activity persists to the present time, mainly in the crater of Mt. Misery. The bulk of the Mt. Misery rocks are of andesitic composition; basalts constitute less than 30 percent of the total and dacites are apparently absent. Most of the rocks are porphyritic and calcic plagioclase is the dominant phenocryst. The commonest rock-type is a two-pyroxene andesite in which hypersthene is usually slightly more abundant than clinopyroxene. Of the coarse-grained blocks ejected from Mt. Misery, the most abundant type is a hornblende gabbro but anorthite bearing blocks similar to those described from St. Vincent are also found. Lo: UWI, Mona, Science Library.
Au: Tomblin, Judith M. Ti: The geology of the Soufriere Volcanic Centre, St. Lucia. So: In: Saunders, John B. ed. Transactions of the Fourth Caribbean Geological Conference. Arima, Caribbean Printers, 1968. 367-76. Co: Fourth Caribbean Geological Conference; Port-of-Spain, 28, Mar. – 12, Apr. 1965. Ab: The Soufriere region of St. Lucia is the site of a volcanic caldera of Pleistocene age. Pre-caldera activity in the region involved firstly the emission of basalt lava flows, and subsequently the growth of a group of andesitic strato volcanoes around a centre to the north-east of the ultimate caldera. From these strato volcanoes, andesite pyroclasts were erupted both vertically and as pyroclast flows (glowing avalanches), in a phase of progressively more violent activity ending with caldera subsidence. Since caldera subsidence, intermittent eruptions have occurred, forming fifteen domes and seven craters within the caldera, and emitting pyroclasts, mainly as pumice flows, to form thick deposits within the caldera and beyond the caldera rim. The basalts of the Soufriere region are characterised by the predominance of augite among the mafic minerals, and contain between 51 percent of silic. In the andesites, hypersthene is often the only mafic phenocryst mineral. In the dacites, amphibole and bilatite are the principal mafic phenocrysts, and are accompanied by 5 percent to 15 percent of quartz phenocrysts. The andesites and dacites, which chemically form a continuous series with silica contents ranging from 59 percent to 66 percent, are believed to have been generated mainly by the partial fusion of local crustal material. Lo: UWI, Mona, Science Library. Yüklə 2,03 Mb. Dostları ilə paylaş:
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