International Journal of Astrophysics and Space Science

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New Interpretation for Libyan Desert Glass Formation

Received: 15 September 2013    Accepted:     Published: 20 October 2013
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Abstract

Ever since the discovery of Libyan Desert Glass in the southwest corner of the Great Sand Sea near the Libyan border, its source of formation has become the subject of controversy that still has not been resolve. This paper introduces a general description of Libyan Desert Glass. It presents briefly different theories explaining its formation. This paper introduces also new interpretation for Libyan Desert Glass formation. This interpretation suggests a meteorite impact mechanism. In this paper, the study of meteorite impact mechanism of BP and Oasis craters was carried out for the first time using a simple model. Calculations have shown that change in temperature for the target materials (sand) because of meteorite impact could explain the formation mechanism of Libyan Desert Glass that took place about 29 million years ago.

DOI 10.11648/j.ijass.20130104.13
Published in International Journal of Astrophysics and Space Science (Volume 1, Issue 4, October 2013)
Page(s) 23-28
Creative Commons

This is an Open Access article, distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution and reproduction in any medium or format, provided the original work is properly cited.

Copyright

Copyright © The Author(s), 2024. Published by Science Publishing Group

Keywords

Materials Characteristics, Meteorite, Meteorite Impact Mechanism, Shock Wave, Geochemical Principles, Technology of Earth Mapping, Astrophysics, Space Science, NASA

References
[1] Christian Koeberl., Proceeding of the " Silica ’96 " Meeting, 1997, pp 121- 158
[2] Barnes V. E. and Underwood J. R. JR., " New Investigations of the strewn field of Libyan Desert Glass and its Petrography"., Earth Planetary Science Letters, 30, 1976, pp 117-122
[3] Bagnold R. A., " A further journey through the Libyan Desert"., The Geographical Journal (London), 82, 2, 1933, 103-129
[4] Bagnold R. A., Myers O. H., Peel R. F. and Winkler H. A., " An expedition to the Gilf Kebir and Uweinat". The Geographical Journal (London), 93, 4, 1939, pp 281-313
[5] Clayton P.A. and Spencer L.J., " Silica glass from the Libyan Desert"., Min. Mag., 23, 1934, pp 501-508.
[6] Weeks, Underwood, and Giegengack, ‘Libyan Desert Glass: A Review’, J. Noncrystalline Solid, v.67, 593 (1984).
[7] Seebaugh and Strauss, ‘Libyan Desert Glass: Remnants of an Impact Melt Sheet’, Lunar and Planetary Science 15th Conference, 1377 (1984).
[8] Begosew Abate et. al., "BP and Oasis impact structures, LIBYA: Preliminary Petrographic and Geochemical Studies, and Relation to Libyan Desert Glass"., Lunar and Planetary Science XXVIII, 1997, Abstract: 1620.pdf
[9] Storzer D and G.A. Wagner, Meteoritics 12, 1977, pp 368
[10] http://www.b14643.de/Sahara/LDG/
[11] The Libyan Desert Geography., Libyan Desert Glass, http://www.fjexpeditions.com
[12] https://www.google.com.ly/#q=LIBYAN+DESERT+ GLASS
[13] http://www.bibliotecapleyades.net/ancientatomicwar/esp_ancient_atomic_04d.htm
[14] John W. Olsen and James R. Underwood http://www.saudiaramcoworld.com/issue/197905/desert.glass-an.enigma.htm
[15] Christian Koeberl., Wolf Uwe Reimold., and Jeff Plescia., "BP and Oasis Impact Structures, Libya: Remote Sensing and Field Studies", Impact Tectonics, 6, Springer, 2005, pp. 161–190
[16] Stephen A. Nelson, Meteorites, Impacts, & Mass Extinction, http://www.tulane.edu/~sanelson/Natural_Disasters/impacts.htm
[17] Ben A. van der Pluijm., "How to Build a Habitable Planet"., Geological Sciences, 1998. www.umich.edu/~gs265/meteor.htm
Author Information
  • Department of Physics, University of Benghazi, P.O.Box 9480, Benghazi, Libya

  • Department of Physics, University of Benghazi, P.O.Box 9480, Benghazi, Libya

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    Samir Ahmed Hamouda, Fatma Milad Elsharif. (2013). New Interpretation for Libyan Desert Glass Formation. International Journal of Astrophysics and Space Science, 1(4), 23-28. https://doi.org/10.11648/j.ijass.20130104.13

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    ACS Style

    Samir Ahmed Hamouda; Fatma Milad Elsharif. New Interpretation for Libyan Desert Glass Formation. Int. J. Astrophys. Space Sci. 2013, 1(4), 23-28. doi: 10.11648/j.ijass.20130104.13

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    AMA Style

    Samir Ahmed Hamouda, Fatma Milad Elsharif. New Interpretation for Libyan Desert Glass Formation. Int J Astrophys Space Sci. 2013;1(4):23-28. doi: 10.11648/j.ijass.20130104.13

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  • @article{10.11648/j.ijass.20130104.13,
      author = {Samir Ahmed Hamouda and Fatma Milad Elsharif},
      title = {New Interpretation for Libyan Desert Glass Formation},
      journal = {International Journal of Astrophysics and Space Science},
      volume = {1},
      number = {4},
      pages = {23-28},
      doi = {10.11648/j.ijass.20130104.13},
      url = {https://doi.org/10.11648/j.ijass.20130104.13},
      eprint = {https://download.sciencepg.com/pdf/10.11648.j.ijass.20130104.13},
      abstract = {Ever since the discovery of Libyan Desert Glass in the southwest corner of the Great Sand Sea near the Libyan border, its source of formation has become the subject of controversy that still has not been resolve. This paper introduces a general description of Libyan Desert Glass. It presents briefly different theories explaining its formation. This paper introduces also new interpretation for Libyan Desert Glass formation. This interpretation suggests a meteorite impact mechanism. In this paper, the study of meteorite impact mechanism of BP and Oasis craters was carried out for the first time using a simple model. Calculations have shown that change in temperature for the target materials (sand) because of meteorite impact could explain the formation mechanism of Libyan Desert Glass that took place about 29 million years ago.},
     year = {2013}
    }
    

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    AB  - Ever since the discovery of Libyan Desert Glass in the southwest corner of the Great Sand Sea near the Libyan border, its source of formation has become the subject of controversy that still has not been resolve. This paper introduces a general description of Libyan Desert Glass. It presents briefly different theories explaining its formation. This paper introduces also new interpretation for Libyan Desert Glass formation. This interpretation suggests a meteorite impact mechanism. In this paper, the study of meteorite impact mechanism of BP and Oasis craters was carried out for the first time using a simple model. Calculations have shown that change in temperature for the target materials (sand) because of meteorite impact could explain the formation mechanism of Libyan Desert Glass that took place about 29 million years ago.
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