نتایج جستجو برای: taftan volcano
تعداد نتایج: 7445 فیلتر نتایج به سال:
We present a full-wave analysis method on the transmission of a Gaussian light pulse through a spherical invisibility cloak with causal dispersions. The spatial energy distribution of the Gaussian light pulse is distorted after the transmission. A volcano-shaped spatial time-delay distribution of the transmitted light pulse is demonstrated as a concrete example in our physical model. Both the t...
The 4.3-Mb genome of Lutibaculum baratangense strain AMV1(T), isolated from a soil sample collected from a mud volcano in Andamans, India, is reported. The draft genome of strain Lutibaculum baratangense AMV1(T) consists of 4,300,776 bp with a G+C content of 66.93 mol% and 4,198 predicted coding regions, including 56 RNAs.
A contribution presents a view about the current landscape of the central part of the Nízký Jeseník Mountains. This region was afflicted not only by the activity of volcanoes, but also by the activity of human. The construction of the Slezská Harta Water Reservoir was the last huge change in the landscape.
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Voight, B., 1990. The 1985 Nevado del Ruiz volcano catastrophe: ana tomy and retrospection. J. Volcanol. Geotherm. Res., 44:
A number of electric and magnetic signals have been observed on La Fournaise volcano, attributed to electrokinetic effects. A simple model is proposed here to check this hypothesis. The volcano is idealized as a 2d heterogeneous structure composed of a fractured zone located between two porous zones through which meteoritic waters flow downwards; flow occurs predominantly in the fractured zone ...
Kı̄lauea volcano is the largest stationary source of SO2 pollution in the United States of America. Moreover, the SO2 that the volcano emits eventually forms particulate matter, another major pollutant. We use this exogenous ∗We thank Jill Miyamura of Hawai‘i Health Information Corporation for the data. Chaning Jang and Jonathan Sweeney provided expert research assistance. We also thank particip...
Significant anomalous changes in the ultra low frequency range (approximately 0.01 Hz) were observed in both geoelectric and geomagnetic fields before the major volcano-seismic activity in the Izu Island region, Japan. The spectral intensity of the geoelectric potential difference between some electrodes on Niijima Island and the third principal component of geomagnetic field variations at an a...
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