The deposits of the useful minerals & rocks; their origin, form, and content . lying un-conformably upon Carboniferous beds. It is only the southern outliersof this belt which, on both sides of the frontier as well as in Galicia, areore-bearing. At Tarnowitz, the Tarnowitz syncline ^\ith a north-south strike andsome 20 km. wide, branches from the main belt. To this in turn isattached the Beuthen syncline some 7 km. wide, which, between Mikult-schiitz, Miechowitz, and Dombrowka, strikes sometimes east and some-times south-east. This latter syncline, illustrated in Fig. 152, extends overBeuthen,
The deposits of the useful minerals & rocks; their origin, form, and content . lying un-conformably upon Carboniferous beds. It is only the southern outliersof this belt which, on both sides of the frontier as well as in Galicia, areore-bearing. At Tarnowitz, the Tarnowitz syncline ^\ith a north-south strike andsome 20 km. wide, branches from the main belt. To this in turn isattached the Beuthen syncline some 7 km. wide, which, between Mikult-schiitz, Miechowitz, and Dombrowka, strikes sometimes east and some-times south-east. This latter syncline, illustrated in Fig. 152, extends overBeuthen, across the frontier to Czeladz, Bendzin, and as far as Klimontowin Russian Poland, when after a short break it continues to Dlugosczyn andSzakowa, situated in the synclinal subsidence of Chrzanow and Trzebinia, inGalicia. To the north, between Ptakowitz and Stollarzowitz, an anticlinallift of the older beds exposes two secondary synclines, the Trockenberg tothe north and the Miechowitz to the south. According to Beyschlag and VOL. II p jn cL too (D Q. 7 (0 CD o ^ r CD JC o. Komgshutte Beulnen ffTTTfTl rrm nrm (hem fr^^^ Border Anficline Sijnclme Up ffof/teoetidei Bufirerffrot/fi group group Deulich Pietor
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Keywords: ., bookcentury1900, bookdecade1910, booksubjectminesandmineralresou
