The first one is a tectonic depression in the Coast Range connected to Valdivia by Cruces River and the second is the continuation of the Intermediate Depression that re-opens south of M�fil.
12.
The Sian Lowland is a tectonic depression along the foothills of the Carpathian Mountains filled in by Miocene strata ( up to thick ) covered with Tarnohorod ) dissected by the valleys of rivers, such as the Tanew River, the Liubachivka River, the Shklo River, and the Vyshnia River.
