Central American Cordillera

The American Cordillera and the Continental Divide: A Geographical Backbone Shaping the Americas

The Continental Divide of the Americas is a geographic feature that divides watersheds draining into the Pacific Ocean from those flowing into the Atlantic. It stretches from North America's northernmost point to South America's southernmost tip. It is connected to the creation and evolution of the American Cordillera, a vast chain of mountain ranges forming the western backbone of the continent.

The Central America Volcanic Arc: A Geological Marvel

The Central America Volcanic Arc, also known as the Central Volcanic Range, is a mesmerizing chain of volcanic formations spanning from Guatemala to northern Panama. These volcanic formations range from major stratovolcanoes to lava domes and cinder cones. The volcanic arc unfolds parallel to the Pacific coastline of the Central American Isthmus, offering insight into the dynamic forces shaping the region.

The Sierra Madre de Chiapas: A Vital Natural Divide

The Sierra Madre de Chiapas is an impressive mountain range that extends parallel to the Pacific coast in southern Mexico and northern Central America. As the southernmost extension of the Sierra Madre Mountain System, this range is a significant geographical and ecological landmark. Spanning multiple countries, the Sierra Madre de Chiapas is known for its diverse ecosystems, volcanic activity, and role in the region's hydrology.

The Sierra Madre: Mexico's Magnificent Mountain Kingdom

Stretching majestically across Mexico, the Sierra Madre mountain system forms an awe-inspiring backbone that encloses the central Mexican Plateau. This vast and intricate network of ranges, part of the mighty American Cordillera, extends in a broad northwest-southeast arc, encompassing a kaleidoscope of landscapes, ecosystems, and cultural heritage that have shaped the essence of Mexico.

The Trans-Mexican Volcanic Belt: Unveiling Mexico's Geological Marvels

The Trans-Mexican Volcanic Belt, alternatively known as the Cordillera Neo-Volcánica, stands as a geological masterpiece stretching from the Pacific Ocean to the Gulf of Mexico in south-central Mexico. Encompassing an active volcanic arc, this volcanic belt narrates a tale of the dynamic interplay between tectonic plates that has unfolded over millions of years.