8~MMARY
The article is a continuation of the di.si:uB&ion held
in
,,Przegl~d Geologiczny", and 'begun once inthe papers on both the age and magnitude of the Young Tertiary tectonic activity in the Sudetes, and
the age of the so-called ice-dammed lake clays. In the papers No No 11 and 12, issued in 1968, microfioristic and geologic studies were anllilysed, as well as geomorphlc development and tectonic activity in the Sudetic aTaa were di6CIUssed in the light of·
the studies considered.
The present article is a .reply
to
Prof.Dr.
H. Tels-seyre's article printed in this .issue on the genesis and age of the Sudetlc varved clays.PE3IOME
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