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16 results

Chronicum Scotorum
  • A Chronicle of Irish Affairs, from the Earliest Times to AD 1135
  • Edited and translated by William M. Hennessy
  • Published online:
    05 October 2013
    Print publication:
    15 November 2012
    First published in:
    1866
  • This chronicle, first published in 1866, is a transcription and translation of a manuscript that gives an account of the earliest-known period of Ireland's history until 1135, describing the leaders and tribes of the Scoti, as the Romans called the inhabitants of the island. Forming part of the Rolls Series of publications of manuscripts concerning the history of Great Britain and Ireland during the Middle Ages, this work was edited and translated by William Hennessy (c.1829–89), a linguist who was interested in the preservation of the Irish language. His extensive introduction to the text examines the complicated history of the manuscript's previous versions, and his essay has been considered a valuable source for historians. The text has transcriptions of the manuscript in its original Irish and provides corresponding English translations, as well as a glossary.

  • Abundance and distribution of uranium and thorium in the northern units of the Leinster granite, Ireland

  • P. J. O'Connor, J. Hennessy, P. M. Bruck, C. T. Williams
  • Journal:
    Geological Magazine / Volume 119 / Issue 6 / November 1982
    Published online by Cambridge University Press:
    01 May 2009, pp. 581-592

  • Abundance data, determined by epithermal neutron activation analysis, are reported for radioelements in the northern units of the Leinster granite. Compared to similar data for silicic igneous rocks and British Caledonian granites, the Leinster granite shows normal U and K contents but is low in Th. Inter-element correlations and fission-track results suggest that most Th and up to 40% of the U is bound in resistate accessory phases (zircon, sphene, apatite), but that the bulk of U is associated with late-stage alteration products and is located at interstitial labile sites within the host-rock matrix. Mobilization of U located at such sites in the Leinster granite by hydrothermal leaching could lead to redeposition and enrichment in marginal sediments of Old Red Sandstone or younger age.