990 resultados para Bowdoin College Grant West
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We present detailed paleomagnetic and rock magnetic results of rock samples recovered during Leg 173. The Leg 173 cores display a multicomponent magnetization nature. Variations in magnetic properties correlate with changes in lithology that result from differences in the abundance and size of magnetic minerals. The combined investigation suggests that the magnetic properties of the "fresher" peridotite samples from Site 1070 are controlled mainly by titanomagnetite, with a strong Verwey transition in the vicinity of 110 K, and with field- and frequency-dependent susceptibility curves that resemble those of titanomagnetites. These results are in excellent agreement with thermomagnetic characteristics where titanomagnetites with Curie temperature ~580°C were identified from the "fresher" peridotites. In contrast to the magnetic properties observed from the "fresher" peridotites, the low-temperature curves for the "altered" peridotites did not show any Verwey transition. Thermomagnetic analysis using the high-temperature vibrating sample magnetometer also failed to show evidence for titanomagnetites. The remanent magnetization is carried by a thermally unstable mineral that breaks down at ~420°C, probably maghemite. The field- and frequency-dependent relationships are also directly opposite to those in the reversal zone, with no signs of titanomagnetite characteristics. Altogether, these rock magnetic data seem to be sensitive indicators of alteration and support the contention that maghemite is responsible for the magnetic signatures displayed in the altered peridotites of the upper section. The magnetic minerals of the basement rocks from Sites 1068, 1069, and 1070 are of variable particle size but fall within the pseudo-single-domain size range (0.2-14 µm). The average natural remanent magnetization (NRM) intensity of recovered serpenitinized peridotite is typically on the order of 20 mA/m for samples from Site 1068, but ~120 mA/m for samples from Site 1070. The much stronger magnetization intensity of Site 1070 is apparently in excellent agreement with the observed magnetic anomaly high. Nearly half of the NRM intensity remained after 400°C demagnetization, suggesting that the remanence can contribute significantly to the marine magnetic anomaly.
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Originally West Professor's house on North University. Became Homeopathic Hospital. Wing added in rear of building in 1879. School of Dentistry 1875-1877. Psychological Lab 1903-1914. Building razed in 1914. On verso: Homeopathic Dept. from 1875-1877. In another hand: School & Dental School (Dr. M. Ward's corrections 3-25-35)
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Pompeii (deserted settlement), Italy
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"The Association [of American colleges] organized in the spring of 1937 a study known as the Library project. 'Teaching with books' is the outcome of this Library project ... made possible by a grant from the Carnegie corporation."--Foreword.
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Mode of access: Internet.
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Names of persons and places are fictitious.
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1887/88-1889/90 published in Charleston; 1890/91-1898/99, in Fairmont.
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Analyses of the War in Afghanistan frequently mention the declining or shaky domestic support for the conflict in the United States and among several U.S. allies. This paper dates the beginning of this decline back to the resurgence of the Taliban in 2005-06 and suggests that the deteriorating course of the war on the ground in Afghanistan itself along with mounting casualties is the key reason behind this drop in domestic support for the war.
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Bibliographies included in Appendix (p. [365]-387)
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Mode of access: Internet.
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"Based on mimeographed pupil's trial edition" published in 1930 in two volumes.
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Mode of access: Internet.
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Toyohara Kunichika and Utagawa Kunisada III; 1 ft. 2 49/64 in.x 2 ft. 5 49/64 in.; woodcut (triptych), ink and color on paper
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Originally published: Kansas City, Mo., Ramsey, Millet & Hudson, 1874.
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A.E. Shipley, chairman.