Mountain Building and Tectonic Deformations
This section covers orogenic processes and resulting deformations. Deformacje tektoniczne encompasses both continuous and discontinuous structural changes.
Definition: Orogenesis refers to the series of tectonic processes resulting in mountain chain formation.
Example: The Alpine orogeny created mountain ranges including the Himalayas, Cordilleras, and Alps.
Highlight: Three major orogenic periods shaped today's mountain ranges: Caledonian, Hercynian, and Alpine.
Vocabulary: Anticlines and synclines are types of continuous deformations where rock layers fold upward and downward respectively.






































