975 resultados para 116-718
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The state of consolidation of outer Bengal Fan deposits is closely related to their depositional history. Early Pleistocene sediments are underconsolidated, i.e., fabric strength is lower than under equilibrium with the present overburden stress, at depths greater than 60-80 mbsf. This may be due to rapid accumulation (>15-20 cm/k.y.) and overlying low-permeability (<10**-7 cm/s) deposits. The underlying Pliocene sediments are overconsolidated, i.e., fabric strength is higher than in equilibrium with the present overburden stress; at Sites 717 and 719 the sediments are slightly overconsolidated, whereas at Site 718 the overconsolidation is significant. Overconsolidation is explained by erosion that occurred during the early Pleistocene for which a stratigraphic gap was recorded in the drilled cores. The eroded section is estimated to be in the range of 10-40 m at Sites 717 and 719, respectively, and 130-150 m at Site 718. Below 250-300 mbsf the most sediments are normally consolidated. The amount of erosion seems to be related to block rotation and uplift due to intraplate deformation.
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"The tune comparative list. One hundred and sixteen melodies of white people paired with same number of Negro-sung variants": p. [145]-227.
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Mode of access: Internet.
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"Pursuant to the requirement of 105 ILCS 5/ IE-130 and IF-130 of the Illinois School Code, enclosed is the School Finance Authority's Annual Report for the Round Lake Area Schools -- District 116 and Hazel Crest School District 152.5 along with copies of the audited financial statements for fiscal year ending June 30, 2003."--Memorandum.
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Continued in "Lettre aux soi-disans membres du conseil général d'administration de l'Ordre du Temple."
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"16 December 1970."
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"June 1984."
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Includes index.