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The Thrace depression
is limited to the south by the Rhodope Mountains, and to the north by the
Sredna Gora Mountains. Neogene and Quaternary deposits fill the depression.
These deposits cover older, mainly Paleogene, sedimentary and volcanic
rocks. The thickness of the young deposits riches several hundred meters
in central part of the depression. The sedimentation during Neogene and
Quaternary time is controlled by WNW–ESE and E–W striking faults. |