952 resultados para Seismological Society of America.


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Papers and dicussion in English, French or German; the original paper being accompanied by abstract or translation in the other two languages. The German and French contributions to the discussion have an English translation in parallel columns.

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List of members for the years 1914-20 are included in v. 1-7, after which they are continued in the year book of the Society, begun in 1922.

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No. 1, 4 originally published 1908, 1910 respectively, are reprints, 1914.

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Title from caption.

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Edition limited: v. 1, pt. 1, v. 2-5, 300 copies printed; v. 6-7, no. 1-2, 500 copies; v. 7, no. 3-4-v. 9, 400 copies.

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Place of publication varies: <1975- >, College Park, Md.; <1991>- , Lanham, MD.

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1911 called v. 4 to correspond with the 4th year of the society; previous publications were bound in 2 vols. to which no special numbers were given. The first comprised Bulletins 1-18, 1908-1909, and the 2d Bulletins 19-31, 1910.

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Mode of access: Internet.

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On 26 January 1531, a strong-magnitude earthquake heavily impacted Lisbon downtown. Immediately after the earthquake, the eyewitnesses reported large waves in the Tagus estuary, mainly north of the city and along the northern bank of the river. Descriptions include large impacts on ships anchored in the estuary and even morphological changes in the riverbed. We present a synthesis of the available information concerning both the earthquake and the water disturbance as a basis for the discussion of the probable tectonic source and the magnitude of the associated river oscillations. We hypothesize that the initial disturbance of the water can be attributed to the coseismic deformation of the estuary riverbed, and we use a nonlinear shallow water model to simulate the tsunami propagation and inundation. We show that the Vila Franca de Xira fault is the most probable source of the 1531 event. The largest inundation effects of the model correlate well with the historical descriptions: the impact is relevant in the inner Tagus estuary, but inundation in downtown Lisbon is small.

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Over the past decade, scientists have been called to participate more actively in public education and outreach (E&O). This is particularly true in fields of significant societal impact, such as earthquake science. Local earthquake risk culture plays a role in the way that the public engages in educational efforts. In this article, we describe an adapted E&O program for earthquake science and risk. The program is tailored for a region of slow tectonic deformation, where large earthquakes are extreme events that occur with long return periods. The adapted program has two main goals: (1) to increase the awareness and preparedness of the population to earthquake and related risks (tsunami, liquefaction, fires, etc.), and (2) to increase the quality of earthquake science education, so as to attract talented students to geosciences. Our integrated program relies on activities tuned for different population groups who have different interests and abilities, namely young children, teenagers, young adults, and professionals.

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Mode of access: Internet.