What is the Central Atlantic magmatic province (CAMP)?
Q: What is the Central Atlantic magmatic province (CAMP)?
A: The Central Atlantic magmatic province (CAMP) is the Earth's largest continental large igneous province, which resulted from a massive volcanic outburst that occurred at the end of the Triassic period.
Q: What is the area covered by the CAMP?
A: The CAMP has an area of approximately 11 million km2.
Q: What type of rock is the CAMP composed of?
A: The CAMP is mostly made up of basalt.
Q: When did the CAMP form?
A: The CAMP formed before the breakup of Pangaea in the Mesozoic Era.
Q: What is the legacy of the CAMP?
A: The legacy of the CAMP is a vast area of basaltic dikes, sills, and lavas around the present central North Atlantic Ocean, created as a result of the subsequent breakup of Pangaea.
Q: What event may have been caused by the CAMP?
A: The CAMP may have caused the end-Triassic extinction event.
Q: What is the significance of the CAMP?
A: The CAMP is significant because of its size and impact on Earth's history, contributing to the formation of the Atlantic Ocean and a legacy of basaltic features in the central North Atlantic Ocean region.
