page_title: Main Dolomite
hierarchical_section_title: Main Dolomite
caption_attribution_description: Hauptdolomit Kaltenbachwildnis, Upper Austria, Austria
context_page_description: Main Dolomite is a lithostratigraphic unit in the Alps of Europe. Formation was defined by K.W. Gümbel in 1857.
  Middle to Late Triassic sedimentary record in the Alpine realm is characterized by presence of various masses of dolomitic rock formations. In the Northern Calcareous Alps the dolomitic mass of Ladinian - Norian age is divided by the Carnian sandstones and shales of Lunz Formation to the Ladinian - Carnian Wetterstein Dolomite and Norian Main Dolomite. The Main Dolomite reaches higher thickness than underlying dolomites in Alps, therefore it is considered as more important "Main".
context_section_description: Main Dolomite (German: Hauptdolomit, Hungarian: Fődolomit, Italian: Dolomia Principale) is a lithostratigraphic unit in the Alps of Europe. Formation was defined by K.W. Gümbel in 1857.
  Middle to Late Triassic sedimentary record in the Alpine realm is characterized by presence of various masses of dolomitic rock formations. In the Northern Calcareous Alps the dolomitic mass of Ladinian - Norian age is divided by the Carnian sandstones and shales of Lunz Formation to the Ladinian - Carnian Wetterstein Dolomite and Norian Main Dolomite. The Main Dolomite reaches higher thickness than underlying dolomites in Alps, therefore it is considered as more important "Main".
caption: Main dolomite of the Langbathscholle, Kaltenbachwildnis, Austria
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