El Arco de Cabo San Lucas
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The arch of Cabo San Lucas is a distinctive
granitic A granitoid is a generic term for a diverse category of coarse-grained igneous rocks that consist predominantly of quartz, plagioclase, and alkali feldspar. Granitoids range from plagioclase-rich tonalites to alkali-rich syenites and from quartz- ...
rock formation at the southern tip of Cabo San Lucas, which is itself the extreme southern end of
Mexico Mexico (Spanish: México), officially the United Mexican States, is a country in the southern portion of North America. It is bordered to the north by the United States; to the south and west by the Pacific Ocean; to the southeast by Guatema ...
's Baja California Peninsula. The arch is locally known as "El Arco," which means "the arch" in Spanish, or "Land's End." It is here that the
Pacific Ocean The Pacific Ocean is the largest and deepest of Earth's five oceanic divisions. It extends from the Arctic Ocean in the north to the Southern Ocean (or, depending on definition, to Antarctica) in the south, and is bounded by the contin ...
becomes the
Gulf of California The Gulf of California ( es, Golfo de California), also known as the Sea of Cortés (''Mar de Cortés'') or Sea of Cortez, or less commonly as the Vermilion Sea (''Mar Bermejo''), is a marginal sea of the Pacific Ocean that separates the Baja C ...
. This area is widely used in hotel
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in the Los Cabos Corridor. This spot is a popular gathering area for sea lions and is frequented by tourists. It is three stories tall and was formed from natural
erosion Erosion is the action of surface processes (such as water flow or wind) that removes soil, rock, or dissolved material from one location on the Earth's crust, and then transports it to another location where it is deposited. Erosion is dis ...
. The Arch of Cabo San Lucas is adjacent to Lovers Beach on the Sea of Cortez side and Divorce Beach on the rougher Pacific Ocean side. The Arch is accessible by land if you approach it by placing yourself at the beach of the last hotel on the Pacific ( Finisterra ) You will have to climb some big rocks, once you do that, you will be at the very tip of the peninsula and a few steps from El arco. Basement rock in Los Cabos formed through intrusive igneous processes c. 115 million years ago, during the
Cretaceous The Cretaceous ( ) is a geological period that lasted from about 145 to 66 million years ago (Mya). It is the third and final period of the Mesozoic Era, as well as the longest. At around 79 million years, it is the longest geological period of ...
period.


References

Natural arches Rock formations of Mexico Landforms of Baja California Sur Cabo San Lucas Landmarks in Mexico {{BajaCaliforniaSur-geo-stub