north american
The Pacific Plate is subducting beneath the South American Plate to form the Andes mountain range, not the San Andreas mountain range. The San Andreas Fault is a transform boundary between the Pacific Plate and the North American Plate in California.
The South American Plate and the Nazca Plate are responsible for the creation of the Andes mountain ranges. The Nazca Plate is subducting beneath the South American Plate, causing the formation of the Andes through tectonic activity and volcanic processes.
The Andes mountain range forms near a subduction zone where the Nazca Plate is subducting beneath the South American Plate. This subduction process has resulted in the uplift of the Andes mountains over millions of years.
Examples of convergent boundaries include the Himalayan mountain range (where the Indian Plate is colliding with the Eurasian Plate), the Andes mountain range (where the South American Plate is subducting under the Nazca Plate), and the Mariana Trench (where the Pacific Plate is subducting beneath the Mariana Plate).
The Andes mountain range is a result of convergent plate boundary formation, where the South American Plate is subducting beneath the Nazca Plate. This collision has led to the uplift and formation of the Andes mountains through various geological processes over millions of years.
north american
north american
north american
north american
The Pacific Plate is subducting beneath the South American Plate to form the Andes mountain range, not the San Andreas mountain range. The San Andreas Fault is a transform boundary between the Pacific Plate and the North American Plate in California.
The South American Plate and the Nazca Plate are responsible for the creation of the Andes mountain ranges. The Nazca Plate is subducting beneath the South American Plate, causing the formation of the Andes through tectonic activity and volcanic processes.
The Andes mountain range forms near a subduction zone where the Nazca Plate is subducting beneath the South American Plate. This subduction process has resulted in the uplift of the Andes mountains over millions of years.
The Andes mountain range is being formed by the convergence of the Nazca and South American plates. This process involves the oceanic Nazca Plate subducting beneath the South American Plate, leading to the uplift of the Andes mountains.
Examples of convergent boundaries include the Himalayan mountain range (where the Indian Plate is colliding with the Eurasian Plate), the Andes mountain range (where the South American Plate is subducting under the Nazca Plate), and the Mariana Trench (where the Pacific Plate is subducting beneath the Mariana Plate).
The Andes mountain range is a result of convergent plate boundary formation, where the South American Plate is subducting beneath the Nazca Plate. This collision has led to the uplift and formation of the Andes mountains through various geological processes over millions of years.
The South American Plate and the Nazca Plate are the two plates that converge to form the Andes mountain range. The Nazca Plate is subducting beneath the South American Plate, leading to the uplift of the Andes through volcanic activity and compression.
The Nazca Plate is subducting beneath the South American Plate along the Peru-Chile Trench. This subduction zone is responsible for the formation of the Andes Mountains and the occurrence of frequent earthquakes in the region.