Triple

Given a phrase, classify it is english named entity (e.g., persons, organizations, works of art) in Latin script, or not (e.g., literals, dates, URLs, verbose phrases). For disambiguation, the statement where the phrase occurs as object is also given. Please return a JSON object with `phrase` (string, the phrase being analyzed) and `is_ne` (boolean, indicating whether the phrase is a Named Entity).

Phrase: Mesozoic–Cenozoic orogeny | Statement: [British Mountains, geologicalAge, Mesozoic–Cenozoic orogeny]

Target entity: Mesozoic–Cenozoic orogeny
Context triple: [British Mountains, geologicalAge, Mesozoic–Cenozoic orogeny]

• A. Marathon orogeny
  The Marathon orogeny was a late Paleozoic mountain-building event in what is now western Texas, associated with the collision of continental plates during the assembly of the supercontinent Pangaea.
• B. Variscan orogeny
  The Variscan orogeny was a major late Paleozoic mountain-building event in Europe, broadly contemporaneous with the Appalachian orogeny, that resulted from the collision of continental plates during the assembly of the supercontinent Pangaea.
• C. 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.
• D. Cadomian orogeny
  The Cadomian orogeny was a late Neoproterozoic mountain-building event that shaped parts of what are now western Europe, contributing to the assembly of the supercontinent Pannotia.
• E. Damara orogeny
  The Damara orogeny was a major Neoproterozoic–early Paleozoic mountain-building event in present-day Namibia associated with the assembly of the Gondwana supercontinent.
• F. None of above. chosen
• G. Unsure - the case is ambiguous/there is not enough information to decide.

Generate a one-sentence description of the target entity. 
You are given a context triple in the form (subject, predicate, object), where the object is the target entity. 
# Instructions
Use the triple to infer relevant information about the entity. Describe the entity based on what is most defining, well-known. 
Avoid repeating the information from the triple, unless really essential.
# Response Format
Return only the sentence: "Description: [one-sentence description of the target entity]"

Entity: Mesozoic–Cenozoic orogeny
Triple: [British Mountains, geologicalAge, Mesozoic–Cenozoic orogeny]

The Mesozoic–Cenozoic orogeny is a long-lasting mountain-building episode spanning from the Mesozoic into the Cenozoic era that shaped many of the modern mountain ranges and tectonic features observed today.

Target entity: Mesozoic–Cenozoic orogeny
Target entity description: The Mesozoic–Cenozoic orogeny is a long-lasting mountain-building episode spanning from the Mesozoic into the Cenozoic era that shaped many of the modern mountain ranges and tectonic features observed today.

• A. Marathon orogeny
  The Marathon orogeny was a late Paleozoic mountain-building event in what is now western Texas, associated with the collision of continental plates during the assembly of the supercontinent Pangaea.
• B. Variscan orogeny
  The Variscan orogeny was a major late Paleozoic mountain-building event in Europe, broadly contemporaneous with the Appalachian orogeny, that resulted from the collision of continental plates during the assembly of the supercontinent Pangaea.
• C. Cordilleran orogeny chosen
  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.
• D. Cadomian orogeny
  The Cadomian orogeny was a late Neoproterozoic mountain-building event that shaped parts of what are now western Europe, contributing to the assembly of the supercontinent Pannotia.
• E. Damara orogeny
  The Damara orogeny was a major Neoproterozoic–early Paleozoic mountain-building event in present-day Namibia associated with the assembly of the Gondwana supercontinent.
• F. None of above.