(Table 1) Sr-isotope values of representative sediment samples from ODP sites at the Costa Rica margin

Two sealed borehole hydrologic observatories (CORKs) were installed in two active hydrogeochemical systems at the Costa Rica subduction zone to investigate the relationship between tectonics, fluid flow, and fluid composition. The observatories were deployed during Ocean Drilling Program (ODP) Leg 205 at Site 1253, ~ 0.2 km seaward of the trench, in the upper igneous basement, and at Site 1255, ~ 0.5 km landward of the trench, in the décollement. Downhole instrumentation was designed to monitor formation fluid flow rates, composition, pressure, and temperature. The two-year records collected by this interdisciplinary effort constitute the first co-registered hydrological, chemical, and physical dataset from a subduction zone, providing critical information on the average and transient state of the subduction thrust and upper igneous basement. The continuous records at ODP Site 1253 show that the uppermost igneous basement is highly permeable hosting an average fluid flow rate of 0.3 m/yr, and indicate that the fluid sampled in the basement is a mixture between seawater (~ 50%) and a subduction zone fluid originating within the forearc (~ 50%). These results suggest that the uppermost basement serves as an efficient pathway for fluid expelled from the forearc that should be considered in models of subduction zone hydrogeology and deformation. Three transients in fluid flow rates were observed along the décollement at ODP Site 1255, two of which coincided with stepwise increases in formation pressure. These two transients are the result of aseismic slip dislocations that propagated up-dip from the seismogenic zone over the course of ~ 2 weeks terminating before reaching ODP Site 1255 and the trench. The nature and temporal behavior of strain and the associated hydrological response during these slow slip events may be an analog for the response of the seaward part of the subduction prism during or soon after large subduction zone earthquakes.

Grain size distribution analysis of prominent beds on Southern Central Chilean seamounts

Gravity cores obtained from isolated seamounts located within, and rising up to 300 m from the sediment-filled Peru-Chile Trench off Southern Central Chile (36°S-39°S) contain numerous turbidite layers which are much coarser than the hemipelagic background sedimentation. The mineralogical composition of some of the beds indicates a mixed origin from various source terrains while the faunal assemblage of benthic foraminifera in one of the turbidite layers shows a mixed origin from upper shelfal to middle-lower bathyal depths which could indicate a multi-source origin and therefore indicate an earthquake triggering of the causing turbidity currents. The bathymetric setting and the grain size distribution of the sampled layers, together with swath echosounder and sediment echosounder data which monitor the distribution of turbidites on the elevated Nazca Plate allow some estimates on the flow direction, flow velocity and height of the causing turbidity currents. We discuss two alternative models of deposition, both of which imply high (175-450 m) turbidity currents and we suggest a channelized transport process as the general mode of turbidite deposition. Whether these turbidites are suspension fallout products of thick turbiditic flows or bedload deposits from sheet-like turbidity currents overwhelming elevated structures cannot be decided upon using our sedimentological data, but the specific morphology of the seamounts rather argues for the first option. Oxygen isotope stratigraphy of one of the cores indicates that the turbiditic sequences were deposited during the last Glacial period and during the following transition period and turbiditic deposition stopped during the Holocene. This climatic coupling seems to be dominant, while the occurrence of megathrust earthquakes provides a trigger mechanism. This seismic triggering takes effect only during times of very high sediment supply to the shelf and slope.

Plan de reconstrucción 1971-1973 de las provincias de Coquimbo, Aconcagua, Santiago, Valparaíso y O'Higgins, afectados por el sismo del 8 de julio de 1971.

Mode of access: Internet.

Auxilios a los damnificados por el terremoto de Cuilapa

Mode of access: Internet.

Guatemala earthquake : hearing before the Subcommittee on Western Hemisphere Affairs and Subcommittee on Foreign Assistance of the Committee on Foreign Relations, United States Senate, Ninety-fourth Congress, second session ... February 16, 1976.

Mode of access: Internet.

Abatement of seismic hazards to lifelines : action plan /

BSSC Program on Improved Seismic Safety Provisions.

Indien, Das Schwer-Heimgesuchte Reich : Das Buch enthält eine vollständige Beschreibung der Pest, Teurung und des Erdbebens von 1896-97 ; Einschliesslich einer genauen Beschreibung der Linderungs-Arbeit durch die "Home and Foreign Relief Commission.' [!] /

"Verschönert mit vielen Abbildungen, welche die wirklichen Begebenheiten in Verbindung mit der Hungersnot, der Pest, dem Erdbeben und der Linderungsarbeit darstellen."

Seismicity of the earth,

"Works to which reference is made": p. 118-125.

Views of prominent places in Charleston, South Carolina, U.S.A., illustrating the effects of the earthquake shock, August 31st, 1886, and a sketch of the occurrence ...

Disbound Original Held in Oak Street Library Facility.

The tsunami of the Alaskan earthquake, 1964: engineering evaluation /

"May 1968."

Geological-seismological evaluation of earthquake hazards at Franklin Falls Damsite, New Hampshire /

Abstract.

Earthquake information bulletin /

Mode of access: Internet.

Verhandlungen der vom 11. bis 13. April 1901 zu Strassburg abgehaltenen ersten Internationalen Seismologischen Konferenz,

Mode of access: Internet.

Technical report, characterization of ground motions during the Northridge earthquake of January 17, 1994 /

"Program to reduce the earthquake hazards of steel moment frame structures"--Cover.

Earthquake history of the United States ...

This publication replaces Special publication 149, Earthquake history of the United States exclusive of the Pacific region, 1928, and Special publication 191, Destructive and near-destructive earthquakes in California and western Nevada, 1934. cf. pt. II, p. 1.