Table of Contents

  • HUTAOSA

    cross-reference

    See ATOSSA.

  • HUTH, GEORG

    Michael Knüppel

    (1867-1906) German Indologist, Tibetologist, Tugusologist, Mongolist, and the founder of Tibetology as a field of research at German universities.

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  • HUTUXŠ

    cross-reference

    and HUTUXŠBED, artisans as a class and the chief of artisans in Sasanian society. See CLASS SYSTEM ii.

  • HUVIŠKA

    A. D. H. Bivar

    ruler of the Great Kushan lineage, successor of Kaniška I the Great, known chiefly from inscriptions and from a prolific coinage. He reigned from at least the year 28 to 60 of the Kaniška Era, equivalent to 154-86 CE.

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  • HUZWĀREŠ

    D. Durkin-Meisterernst

    a term describing the use of Semitic word masks in Middle Persian texts, written in the official orthography of the Sasanian state and surviving in Zoroastrian texts, and a small number of inscriptions, and letters.

  • HVARCIERA

    cross-reference

    See XWARČIHR.

  • HYDARNES

    Rüdiger Schmitt

    (Gk. Hydárnēs), rendering of the Old Persian male name Vidṛna held by several historical persons of the Achaemenid period.

  • HYDE, THOMAS

    A. V. Williams

    (1636-1703), D.D., English orientalist, Professor of Arabic and Hebrew in the University of Oxford, the first scholar to attempt to write a comprehensive description of the religion of Zoroaster.

  • HYDERABAD

    Gavin Hambly, Deborah Hutton

    (Ḥaydarābād), city in the Deccan of India, the former capital of the Nizams (Neẓāms) of Hyderabad (ca. 1724-1948) and at present the state capital of Andhra Pradesh in southern India. It had a three and a half century history as one of the major Muslim states and as a center of Indo-Persian culture in the subcontinent.

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  • HYDROLOGY

    Multiple Authors

    i. Iranian plateau. ĀB. ii. Southwestern Persia. iii. Afghanistan. From a hydrological perspective, southwestern Persia must be considered as part of the Persian Gulf drainage region. Extending over an area of more than 350,000 km², its main drainage area covers the central and southwestern Zagros mountain areas with their extremely complex geomorphology.

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