Laramide orogeny

Target entity: Laramide orogeny
Context triple: [Alaska Range, orogeny, Laramide orogeny]

• A. Cordilleran orogeny
  The Cordilleran orogeny was a long-lasting mountain-building event along western North America that created much of the modern Cordillera, including ranges such as the Rockies and the Peninsular Ranges.
• B. Cascadian orogeny
  The Cascadian orogeny is the long-lasting mountain-building episode responsible for forming the Cascade Range through subduction-related tectonic activity along western North America.
• C. Alpine orogeny
  The Alpine orogeny is a major mountain-building event that created the Alps and other ranges across southern Europe and parts of Asia through the collision of tectonic plates during the Cenozoic Era.
• D. Acadian orogeny
  The Acadian orogeny was a major Middle Paleozoic mountain-building event that significantly shaped the northern Appalachian Mountains through the collision of ancient landmasses.
• E. Appalachian orogeny
  The Appalachian orogeny was a series of ancient mountain-building events that formed the Appalachian Mountains through the collision of tectonic plates during the Paleozoic Era.
• F. None of above. chosen
• G. Unsure - the case is ambiguous/there is not enough information to decide.

Target entity: Laramide orogeny
Target entity description: The Laramide orogeny was a major mountain-building event that occurred in western North America from the Late Cretaceous to early Paleogene, responsible for uplifting ranges such as the Rocky Mountains and parts of Alaska.

• A. Cordilleran orogeny
  The Cordilleran orogeny was a long-lasting mountain-building event along western North America that created much of the modern Cordillera, including ranges such as the Rockies and the Peninsular Ranges.
• B. Cascadian orogeny
  The Cascadian orogeny is the long-lasting mountain-building episode responsible for forming the Cascade Range through subduction-related tectonic activity along western North America.
• C. Alpine orogeny
  The Alpine orogeny is a major mountain-building event that created the Alps and other ranges across southern Europe and parts of Asia through the collision of tectonic plates during the Cenozoic Era.
• D. Acadian orogeny
  The Acadian orogeny was a major Middle Paleozoic mountain-building event that significantly shaped the northern Appalachian Mountains through the collision of ancient landmasses.
• E. Appalachian orogeny
  The Appalachian orogeny was a series of ancient mountain-building events that formed the Appalachian Mountains through the collision of tectonic plates during the Paleozoic Era.
• F. None of above. chosen