Sierra Nevada orogeny

Target entity: Sierra Nevada orogeny
Context triple: [Carson Range, orogeny, Sierra Nevada 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. Laramide orogeny
  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.
• C. 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.
• D. 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.
• E. Sierra Nevada batholith
  The Sierra Nevada batholith is a massive granitic rock formation underlying much of California’s Sierra Nevada range, formed by ancient magma intrusions during Mesozoic subduction along the western edge of North America.
• F. None of above. chosen
• G. Unsure - the case is ambiguous/there is not enough information to decide.

Target entity: Sierra Nevada orogeny
Target entity description: The Sierra Nevada orogeny is a major mountain-building event that formed the Sierra Nevada range in the western United States through prolonged subduction, magmatism, and crustal uplift.

• 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. Laramide orogeny
  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.
• C. 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.
• D. 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.
• E. Sierra Nevada batholith
  The Sierra Nevada batholith is a massive granitic rock formation underlying much of California’s Sierra Nevada range, formed by ancient magma intrusions during Mesozoic subduction along the western edge of North America.
• F. None of above. chosen