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The Demand On Tuff Reduced

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  • The Demand On Tuff Reduced

    THE DEMAND ON TUFF REDUCED

    ARMENPRESS
    27 June, 2012
    YEREVAN

    YEREVAN, JUNE 27, ARMENPRESS: The decline in tuff production has been
    registered in Armenia. During 2012 January-April overall 8 thousand
    524,3 tons of tuff has been produced , 193, 3 of which in April. Th 50,
    8 % decline is recorded when we draw a parallel with the same period
    of the previous year. Industry department of the Ministry of Economy
    informed Armenpress that decline, making over 34, 6 % has been seen
    in outer facing slabs production as well.

    Armenpress reporter had a briefing with the several major company
    representatives to determine the reasons of the production reduce.

    Shirak province, Artik town based "Karastgh "company director Oleg
    Gabrielyan verified the decline in the production of tuff and grounded
    it with the reduction of interest from abroad towards Armenian tuff .

    " A few years ago there was a great demand especially by Russian
    companies,they have not still recovered after the crisis, reportedly
    the marketability of our tuff has reduced" Gabrielyan came forth with.

    To the reporter's question on the export of tuff to Europe " Karastgh"
    representative was quoted as saying , there is a lack of information
    in European countries towards Armenian tuff, they are not familiar
    with this type of building materials, and therefore there is no
    appropriate order.

    Tuff is a type of rock consisting of consolidated volcanic ash ejected
    from vents during a volcanic eruption. Tuff is sometimes called tufa,
    particularly when used as construction material, although tufa also
    refers to a quite different rock. Rock that contains greater than 50%
    tuff is considered tuffaceous.

    This volcanic origin stone widely applied in Armenia has five types-
    , Ani (yellow, orange), Artik (pink, purple), Yerevan (black, red),
    Byurakan (pink, black spots, dark gray, black spots ) and felsitic
    type (figured).Due to the porous quality it retains the cold in winter
    season and hot in summer times.

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