Éditeur(s) : Leslie's Weekly Leslie's Weekly ( New York )
Résumé : Page 173 from Leslie's Weekly, Nov,. Article entitled "The Kingston earthquake at short range", by Francis E. Clark, Founder of the United Society of Christian Endeavor continues on verso.
Six illustrations: Plum Point Lighthouse, which was damaged by the earthquake and its ligth extinguished, causing the stranding of the steamship "Prinz Waldemar". -- Refugees each receiving the meagre food supply of two potatoes, a piece of bread, some brown sugar, and molasses. -- The American Consulate a mass of ruins - Vice-Counsul William H. Orrett standing in front of his demolished office. -- Hundreds of refugees in camp a the temporary market near the Parade ground. -- A crowd of homeless and hungry people waiting for the opening of the gate of the race-course relief station. -- Curious incident of the quake - Queen Victoria's statue, once facing the sea, turned completely around. -- Steamship "Prinz Waldemar," of the Hamburg-American Line, wrecked on the Jamaica coast because the Plum Point Light went out. -- Entrance to Up Park Camp, headquarters of the First West Indian Regiment, showing wreckage of gateways and buildings.
Kingston (Jamaica)

Droits : All rights reserved by the source institution.
2005-348-1

Éditeur(s) : Cassell Cassell ( London )
Résumé : The copyright notice inside the book states 1903. The book includes a photograph after the January 14, 1907 earthquake (Great Kingston Quake of 1907). Information on earthquakes in Jamaica: http://www.mona.uwi.edu/earthquake/equakedata.htm
Large format viewbook, with ill. and text derived by Dr. Brown's from his travel lecture with stereoptican views.
(Statement of Responsibility) by Jas. Johnston, M.D.
Jamaica
Jamaica

Droits : Published in 1903.
194228657
http://ufdc.ufl.edu/AA00011910/00001

Éditeur(s) : Great Britain : [s.n.] Great Britain : [s.n.]
Résumé : (Funding) Support for the development of the technical infrastructure and partner training provided by the United States Department of Education TICFIA program.
On January 14, 1907, a magnitude 6.5 earthquake shook Kingston, Jamaica. Extensive damage resulted from the earthquake and subsequent fire.
Kingston (Jamaica)
Jamaica

Droits : All rights reserved by the source institution.
2007-204-3

Éditeur(s) : Collier's Collier's ( [s.l.] )
Résumé : In Collier's (February 2, 1907), p. 13.
Article on verso: Why the canal by contract? : twelve millions in future commissions on a work already well begun / by Frederick Palmer. Concerns financing for construction of the Panama Canal.
Digital image, 2010,163 mb rgb tiff. 600 ppi
Prints. Box 8.
Kingston (Jamaica)

Droits : All rights reserved by the source institution.
1989-335-1

Éditeur(s) : National Library of Haiti National Library of Haiti
Haiti -- Port-au-Prince

Éditeur(s) : Impr. du Progrès Impr. du Progrès ( Cap-Haïtien, Haiti )
Résumé : Edited by Jean M. Lambert.
Haiti
Haiti
Cap-Haïtien

21215013

Éditeur(s) : New York : Underwood & Underwood, New York : Underwood & Underwood,
Résumé : (Funding) Support for the development of the technical infrastructure and partner training provided by the United States Department of Education TICFIA program.
On January 14, 1907, a magnitude 6.5 earthquake shook Kingston, Jamaica, causing extensive damage to buildings.
Kingston (Jamaica)
Jamaica

Droits : All rights reserved by the source institution.
1995-530-2
http://ufdc.ufl.edu/IR00000118/00001

Éditeur(s) : Chez Couturier Chez Couturier ( Paris )
Résumé : "Appové, ce 5 octobre 1770"--P. 4.
Haiti
Haïti
Haiti
Haïti
Haiti

819751677
ocn819751677
http://ufdc.ufl.edu/AA00021792/00001

Éditeur(s) : HAL CCSD American Geophysical Union
Résumé : International audience
Giant earthquake (moment magnitude M-w >= 8.5) forecasts for subduction zones have been empirically related to both tectonic stresses and geometrical irregularities along the subduction interface. Both of these controls have been suggested as able to tune the ability of rupture to propagate laterally and, in turn, exert an important control on giant earthquake generation. Here we test these hypotheses, and their combined influence, by compiling a dataset of trench fill thickness (a proxy for smoothing of subducting plate relief by sediment input into the subduction channel) and upper plate strain (a proxy for the tectonic stresses applied to the subduction interface) for 44 segments of the global subduction network. We statistically compare relationships between upper plate strain, trench sediment thickness and maximal earthquake magnitude. We find that the combination of both large trench fill (>= 1 km) and neutral upper plate strain explains spatial patterns of giant earthquake occurrence to a statistically significant degree. In fact, the concert of these two factors is more highly correlated with giant earthquake occurrence than either factor on its own. Less frequent giant earthquakes of lower magnitude are also possible at subduction zones with thinner trench fill and compressive upper plate strain. Extensional upper plate strain and trench fill < 0.5 km appear to be unfavorable conditions, as giant earthquakes have not been observed in these geodynamical environments during the last 111 years. Citation: Heuret, A., C. P. Conrad, F. Funiciello, S. Lallemand, and L. Sandri (2012), Relation between subduction megathrust earthquakes, trench sediment thickness and upper plate strain, Geophys. Res. Lett., 39, L05304, doi: 10.1029/2011GL050712.
ISSN: 0094-8276

hal-00745636
https://hal.archives-ouvertes.fr/hal-00745636
https://hal.archives-ouvertes.fr/hal-00745636/document
https://hal.archives-ouvertes.fr/hal-00745636/file/heuretGRL2012.pdf
DOI : 10.1029/2011GL050712

Éditeur(s) : New York : Judge Company, New York : Judge Company,
Résumé : (Funding) Support for the development of the technical infrastructure and partner training provided by the United States Department of Education TICFIA program.
Front page of Leslie's Illustrated Weekly, vol. CIV, no. 2682, p. 97 (January 31, 1907)
"Sketched for Leslie's Weekly by William Bengough."
Kingston (Jamaica)
Jamaica

Droits : All rights reserved by the source institution.
2005-268-1

Éditeur(s) : American book and Bible house American book and Bible house ( Philadelphia )
Résumé : (Statement of Responsibility) as told by eye-witnesses and by ... Samuel A. McAlister ... ed. and written by Charles Morris ...
Pelee, Mount (Martinique)
Saint Pierre (Martinique)
La Soufriere, Mount (St. Vincent)
Saint Vincent and the Grenadines

000588648
23441953
ADB7409

Éditeur(s) : Center for the Humanities and the Public Sphere, University of Florida Center for the Humanities and the Public Sphere, University of Florida ( Gainesville, FL )
Résumé : (Biographical) Dr. Louise Ivers is Chief of Mission for Partners In Health (PIH) in Haiti, an international non-profit organization that provides direct health care and social services to poor communities around the world, supported by research and advocacy. She is an Assistant Professor of Medicine at Harvard Medical School and an Associate Physician in the Division of Global Health Equity at Brigham and Women's Hospital (BWH). She completed her residency in Internal Medicine at Massachusetts General Hospital (MGH) and a fellowship in Infectious Diseases at the combined MGH/BWH program. Dr. Ivers also received a diploma in Tropical Medicine and Hygiene from the London School of Hygiene & Tropical Medicine and a Master of Public Health from the Harvard School of Public Health. Dr. Ivers implements health programs, and is interested in improving the delivery of healthcare in resource poor settings, the provision of care to the rural and urban poor, as well as patient-oriented investigation that offers solutions to barriers to healthcare. She balances her time between management of PIH Haiti, direct clinical service, and operational research. Dr. Ivers has contributed to published articles on HIV/AIDS, food insecurity, and the prevention of mother-to-child transmission of HIV. Current projects include investigating the impact of targeted food assistance to people with HIV infection in rural Haiti, the effectiveness of ARV therapies on viral suppression in community-based programs, and humanitarian assistance in response to the January 2010 earthquake. Dr. Ivers has served as a Technical Advisor to the WHO and also mentors Haitian and American physicians.
(Funding) Sponsored by the Caleb and Michele Grimes Fund in the CLAS Dean's Office and organized by the Center for the Humanities and the Public Sphere.

Droits : All rights reserved by the source institution.

Éditeur(s) : HAL CCSD American Geophysical Union
Résumé : International audience
We recover the Holocene earthquake history of seven seismogenic normal faults in the Fucino system, central Italy. We collected 800 samples from the well-preserved limestone scarps of the faults and modeled their 36Cl concentrations to derive their seismic exhumation history. We found that > 30 large earthquakes broke the faults in synchrony over the last 12 ka. The seven faults released strain at the same periods of time, 12-9 ka, 5-3 ka, and 1.5-1 ka. On all faults, the strain accumulation and release occurred in 3-6 ka supercycles, each included a 3-5 ka phase of slow (≤ 0.5-2 mm/yr) strain accumulation in relative quiescence, followed by a cluster of three to four large earthquakes or earthquake sequences that released most of the strain in < 1-2 ka. The large earthquakes repeated every 0.5 ± 0.3 ka during the paroxysmal phases and every 4.3 ± 0.9 ka between those phases. Earthquakes on the northern faults produced twice larger surface slips (~ 2 m) and had larger magnitudes (Mw 6.2-6.7) than those on the southern faults. On most faults, the relative strain level was found to control the amount of slip and the time of occurrence of the next large earthquake. Faults entered a phase of clustered activity once they had reached a specific relative strain threshold. The Tre Monti fault is identified as the most prone to break over the next century. Our data document earthquake synchrony and clustering at a broader space and time scale than has been reported to date.
ISSN: 0148-0227

hal-00903460
https://hal.archives-ouvertes.fr/hal-00903460
DOI : 10.1002/jgrb.50299

Éditeur(s) : HAL CCSD Seismological Society of America
Résumé : International audience
Abstract The continuous record of large surface-rupturing earthquakes along the Dead Sea fault brings unprecedented insights for paleoseismic and archaeoseismic research. In most recent studies, paleoseismic trenching documents the late Holocene faulting activity, while tectonic geomorphology addresses the long-term behavior (>10 ka), with a tendency to smooth the effect of individual earthquake rupture events (Mw >7). Here, we combine historical, archaeological, and paleoseismic investigations to build a consolidated catalog of destructive surface-rupturing earthquakes for the last 14 ka along the left-lateral Jordan Valley fault segment. The 120- km-long fault segment limited to the north and the south by major pull-apart basins (the Hula and the Dead Sea, respectively) is mapped in detail and shows five subsegments with narrow stepovers (width < 3 km). We conducted quantitative geomorphology along the fault, measured more than 20 offset drainages, excavated four trenches at two sites, and investigated archaeological sites with seismic damage in the Jordan Valley. Our results in paleoseismic trenching with 28 radiocarbon datings and the archaeoseismology at Tell Saydiyeh, supplemented with a rich historical seismic record, document 12 surface-rupturing events along the fault segment with a mean interval of ∼1160 yr and an average 5 mm=yr slip rate for the last 25 ka. The most complete part of the catalog indicates recurrence intervals that vary from 280 yr to 1500 yr, with a median value of 790 yr, and suggests an episodic behavior for the Jordan Valley fault. Our study allows a better constraint of the seismic cycle and related short-term variations (late Holocene) versus long-term behavior (Holocene and late Pleistocene) of a major continental transform fault.
ISSN: 0037-1106

hal-00747401
https://hal.archives-ouvertes.fr/hal-00747401
DOI : 10.1785/0120100097

Éditeur(s) : HAL CCSD Seismological Society of America
Résumé : With the assistance of the ASTER team (M. Arnold, G. Aumaître, D. Bourlès, and K. Keddadouche)
International audience
The Bulnay earthquake of 23 July 1905 (Mw 8.3–8.5), in north‐central Mongolia, is one of the world’s largest recorded intracontinental earthquakes and one of four great earthquakes that occurred in the region during the twentieth century. The 375 km long surface rupture of the left‐lateral, strike‐slip, N095°E‐trending Bulnay fault associated with this earthquake is remarkable for its pronounced expression across the landscape and for the size of features produced by previous earthquakes. Our field observations suggest that in many areas the width and geometry of the rupture zone is the result of repeated earthquakes; however, in those areas where it is possible to determine that the geomorphic features are the result of the 1905 surface rupture alone, the size of the features produced by this single earthquake are singular in comparison to most other historical strike‐slip surface ruptures worldwide. Along the 80 km stretch, between 97.18° E and 98.33° E, the fault zone is characterized by several meters width and the mean left‐lateral 1905 offset is 8.9±0.6  m with two measured cumulative offsets that are twice the 1905 slip. These observations suggest that the displacement produced during the penultimate event was similar to the 1905 slip. Morphotectonic analyses carried out at three sites along the eastern part of the Bulnay fault allow us to estimate a mean horizontal slip rate of 3.1±1.7  mm/yr over the Late Pleistocene–Holocene period. In parallel, paleoseismological investigations show evidence for two earthquakes prior to the 1905 event, with recurrence intervals of ∼2700–4000  yrs.
ISSN: 0037-1106

hal-01179837
https://hal.archives-ouvertes.fr/hal-01179837
https://hal.archives-ouvertes.fr/hal-01179837v2/document
https://hal.archives-ouvertes.fr/hal-01179837/file/rizza2015.pdf
DOI : 10.1785/0120140119

Éditeur(s) : HAL CCSD
Résumé : poster
International audience
Locations for earthquake recorded in the Lesser Antilles subduction zone are processed separately by regional observatories, NEIC and ISC. There is no earthquake location catalog available compiling all available phase arrival data. We propose a new best complete earthquake catalog by merging all available phase arrival data for better constrains on earthquake locations. ISC provides the phase arrival data of 29243 earthquakes (magnitude range from 1.4 to 6.4) recorded by PRSN (Porto Rico), SRC (British West Indies), and from FUNVISIS (Venezuela). We add phases data from IPGP observatories for 68718 earthquakes from magnitudes 0.1 to 7.5 (OVSG, Guadeloupe, recorded 53226 earthquakes since 1981, and OVSM, Martinique, recorded 29931 earthquakes since 1972). IPGP also provides the accelerometer waveform data of the GIS-RAP network. We achieved automatic picking on the GIS-RAP data using the Component Energy Correlation Method. The CECM provides high precision phase detection, a realistic estimation of picking error and realistic weights that can be used with manual pick weights. The CECM add an average of 3 P-waves and 2 S-waves arrivals to 3846 earthquakes recorded by the GIS-RAP network since 2002. The final catalog contains 84979 earthquakes between 1972 and 2013, 24528 of which we compiled additional data. We achieve earthquake location using NonLinLoc, regional P and S waves data and a set of one dimensional velocity models. We produce improved locations for 22974 earthquakes (better residuals, on equal or larger arrival dataset) and improved duration magnitudes for 6258 earthquakes (using duration data and improved locations). A subset of best constrained 15626 hypocenters (with more than 8 phases and an average RMS of 0.48_0.77s) could be used for structural analysis and earthquake local tomography. Relative locations are to be applied in order to image active faulting. We aim to understand coupling in the seismogenic zone as well as triggering mechanisms of intermediate depth seismicity like fluid migration beneath the volcanic arc.
Geophysical Research Abstracts
Vienne, Austria

hal-01059207
https://hal-brgm.archives-ouvertes.fr/hal-01059207

Éditeur(s) : HAL CCSD Oxford University Press (OUP)
Résumé : International audience
We carried out morphotectonic studies along the left-lateral strike-slip Bogd Fault, the principal structure involved in the Gobi-Altay earthquake of 1957 December 4 (published magnitudes range from 7.8 to 8.3). The Bogd Fault is 260 km long and can be subdivided into five main geometric segments, based on variation in strike direction. West to East these segments are, respectively: the West Ih Bogd (WIB), The North Ih Bogd (NIB), the West Ih Bogd (WIB), the West Baga Bogd (WBB) and the East Baga Bogd (EBB) segments. Morphological analysis of offset streams, ridges and alluvial fans-particularly well preserved in the arid environment of the Gobi region-allows evaluation of late Quaternary slip rates along the different faults segments. In this paper, we measure slip rates over the past 200 ka at four sites distributed across the three western segments of the Bogd Fault. Our results show that the left-lateral slip rate is similar to 1 mm yr(-1) along the WIB and EIB segments and similar to 0.5 mm yr(-1) along the NIB segment. These variations are consistent with the restraining bend geometry of the Bogd Fault.;Our study also provides additional estimates of the horizontal offset associated with the 1957 earthquake along the western part of the Bogd rupture, complementing previously published studies. We show that the mean horizontal offset associated with the 1957 earthquake decreases progressively from 5.2 m in the west to 2.0 m in the east, reflecting the progressive change of kinematic style from pure left-lateral strike-slip faulting to left-lateral-reverse faulting. Along the three western segments, we measure cumulative displacements that are multiples of the 1957 coseismic offset, which may be consistent with a characteristic slip. Moreover, using these data, we re-estimate the moment magnitude of the Gobi-Altay earthquake at M-w 7.78-7.95.;Combining our slip rate estimates and the slip distribution per event we also determined a mean recurrence interval of similar to 2500-5200 yr for past earthquakes along the different segments of the western Bogd Fault. This suggests that the three western segments of the Bogd Fault and the Gurvan Bulag thrust fault (a reverse fault bounding the southern side of the Ih Bogd range that ruptured during the 1957 earthquake) have similar average recurrence times, and therefore may have ruptured together in previous earthquakes as they did in 1957. These results suggest that the western part of the Bogd Fault system, including the Gurvan Bulag thrust fault, usually behaves in a 'characteristic earthquake' mode.
ISSN: 0956-540X

hal-00639467
https://hal.archives-ouvertes.fr/hal-00639467
https://hal.archives-ouvertes.fr/hal-00639467v2/document
https://hal.archives-ouvertes.fr/hal-00639467/file/rizzaGJI2011.pdf
DOI : 10.1111/j.1365-246X.2011.05075.x

Résumé : (Bibliography) Includes bibliographical references.
Title from PDF title screen (viewed on February 23, 2011).
Paper version available for sale by the Supt. of Docs., U.S. G.P.O.
Haiti
Haiti
Haiti
Haiti
Haiti

703448560
ocn703448560
http://ufdc.ufl.edu/AA00021599/00001

Éditeur(s) : [s.n., [s.n., ( [s.l. : )
Résumé : Two illustrations: The ruins of Kingston's principal hotel, the Myrtle Bank, the stopping-place of many of Jamaica's American and English visitors. -- The west wing of the Myrtle Bank Hotel, viewed from the court-yard.
Kingston (Jamaica)

Droits : All rights reserved by the source institution.
2005-268-2

Éditeur(s) : National Library of Haiti National Library of Haiti
Haiti -- Port-au-Prince