Yucatán Peninsula


The Yucatán Peninsula is a large landform located in southeastern Mexico, extending into Belize and Guatemala, and is characterized by its low relief and composition primarily of porous limestone. This unique geological makeup influences its hydrology and supports a distinctive ecosystem, separating the Gulf of Mexico from the Caribbean Sea.

⭐ In the context of the Yucatán Peninsula, its geological composition significantly impacts its characteristics. What is the primary material that constitutes the majority of the peninsula’s landmass?


⭐ Core Definition: Yucatán Peninsula

The Yucatán Peninsula (/ˌjkəˈtɑːn, -ˈtæn/ YOO-kə-TA(H)N, UK also /ˌjʊk-/ YUU-; Spanish: Península de Yucatán [peˈninsula ðe ʝukaˈtan]) is a large peninsula in southeast Mexico and adjacent portions of Belize and Guatemala. The peninsula extends towards the northeast, separating the Gulf of Mexico to the north and west of the peninsula from the Caribbean Sea to the east. The Yucatán Channel, between the northeastern corner of the peninsula and Cuba, connects the two bodies of water.

The peninsula is approximately 181,000 km (70,000 sq mi) in area. It has low relief and is almost entirely composed of porous limestone.

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HINT: The Yucatán Peninsula is almost entirely composed of porous limestone, which influences its low relief, hydrology, and overall geological characteristics. This composition is a defining feature of the region.

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