974 resultados para Constantine, VII Porphyrogenitus, Emperor of the East, 905-959.


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owing to the loss of the volume containing the entries for that period."--Pref.

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v. 1. Arabian nights' entertainments [from the French version of A. Galland] New Arabian nights [from the French version of D. Chavis and J. Cazotte]--v. 2. Continuation of the New Arabian nights. Persian tales [from the translation of F. Pétis de la Croix] Persian tales of Inatulla of Delhi [tr. by A. Dow] Oriental tales [by A. C. P., comte de Caylus] The history of Nourjahad [by Mrs. Frances Sheridan] Additional tales from the Arabian nights.--v. 3. Mogul tales [by T. S. Gueulette] Turkish tales [from the translation of F. Pétis de la Croix] Tartarian tales; Chinese tales [by T. S. Gueulette] Tales of the genii [by J. Ridley] The history of Abdalla, the son of Hanif [by J. P. Bignon]

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Mode of access: Internet.

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Audit report on Mental Health Disability Services of the East Central Region (MHDS-ECR) for the year ended June 30, 2015

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Bathymetric data from a Hydrosweep multibeam sonar survey of a 720 km long tectonic corridor on the east flank of the southern EPR at 14 degrees 14'S covered about 25,000 km(2) of zero-age to 8.5 m.y. old crust (magnetic anomaly 4A). In this corridor we document a strong correlation of robust along flowline changes in abyssal hill morphology and seamount size distribution with spreading rate changes deduced from our magnetic data. Indeed, we find that both rms height of abyssal hills and abundance and height of seamounts increase significantly as spreading rate changes from similar to 75 mm/yr to over 85 mm/yr (half rate). Moreover, we identified 46 seamounts taller than 100 m. Previous studies on the southern EPR reported a larger density of seamounts, organized primarily in chains. Our investigation, however, revealed seamounts not associated with major chains, leading us to the conclusion that different forms of off-axis volcanism occur along the spreading center.

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Faults form quickly, geologically speaking, with sharp, crisp step-like profiles. Logic dictates that erosion wears away this "sharpness" or angularity creating more rounded features. As erosion occurs, debris accumulates at the base of the scarp slope. The stable end point of this process is when the scarp slope approaches an ideal sigmoid shape. This theory of fault end process, in combination with a new method developed in this report for fault profile delineation, has the potential to enable observation and categorization of fault profiles over large, diverse swaths of fault formation-- in remote areas such as the Southern Kenyan Rift Valley. This up-to date method uses remote sensing data and the digitizer tool in Global Mapper to create shape files of fault segments. This method can provide further evidence to support the notion that sigmoidal- shaped profiles represent a natural endpoint of the erosional process of fault scarps. Over time, faults of many different ages would exist in this similar shape over a wide region. However, keeping in mind that other processes can be at work on scarps-- most notably drainage patterns, when anomalies in profiles are observed, reactivation in some form possibly has occurred.

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... And the probability of its success considered. To which is added a brief sketch of the present state of Egypt; an historical account of Alexandria; the two harbours of that city accurately delineated, its former splendor and present state contrasted; with some remarks on its local importance should it become the mart of the East: together with a few particulars relating to the navigation of the Red Sea. By the editor of the History of Peter III. and Catharine II. of Russia.