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This article is about a peninsula in North America. For other uses, see Baja California (disambiguation) or California (disambiguation). The Baja California peninsula (Spanish: Península de Baja California, meaning Lower California peninsula) is a peninsula in western Mexico. It extends some 1250 km (775 miles) from Mexicali, Baja California, in the north to Cabo San Lucas, Baja California Sur, in the south, separating the Pacific Ocean from the Gulf of California (or "Sea of Cortés"). The total area of the Peninsula is 143,396 km2. The peninsula is connected to the mainland of Mexico by a strip of land that belongs to Sonora. There are four main desert areas on the peninsula: the San Felipe Desert, the Central Coast Desert, the Vizcaíno Desert and the Magdalena Plain Desert.
[edit] Geology
The Baja California peninsula was once a part of the North American Plate, the tectonic plate of which mainland Mexico remains a part. About 5 million years ago, the East Pacific Rise began cutting into the margin of the North American Plate, initiating the separation of the peninsula from it. Thereafter, the East Pacific Rise continued to propagate northward, up through what is now the Gulf of California. The propagating tip of the spreading center is now located somewhere in the Salton Sea basin. The Baja California peninsula is now part of the Pacific Plate and is moving with it away from the East Pacific Rise in a north northwestward direction. It is an ongoing example of a type of crustal block known as a terrane. Just up the coast from Santa Rosalia, Baja California Sur is a prominent area of volcanic activity. The arid climate of Baja California allows the dramatic volcanic features of the landscape to stand out clearly for the visitor. There are some points of dispute when it comes to stating specific detalis of Baja California's geologic history. However, there is a general agreement that the collision of the North American plate with the Pacific plate resulted in the creation of the mountains on Baja peninsula. The Pacific plate being thinner submerged under the North American thicker continental plate and formed a subduction zone resulting in the occurence of volcanoes. Currently, there are no active volcanoes on the Baja Peninsula. Upon the collision of the tectonic plates massive folds creased due to which the Pacific plate consisting of Baja and all land west of the San Andreas fault began to shift northwards and eventually tore the Baja peninsula off of the Mexican mainland. Naturally, this did not happen over night but over many millenniums. The Sea of Cortez was created when 5 million years ago when the process of opening was over and the sea filled it. The Sea of Cortez is over 600 miles long and more than 14,000 feet deep. Being positioned along the San Andreas Fault, it is seismically very active. Its long and narrow shape makes it produce one of the largest tidal ranges in the world with extreme water temperatures. can also vary by large extremes. Depending on the season and the location, the temperature can vary from a high of 91°F to a low of 47°F. At the point of creation, there was much water since that was the period when the last ice age ended and the sea level rose drastically due to the ice melting. The low areas were filled in while the previously connected higher lands became islands in the sea. In the middle of the Sea of Cortez is the San Andreas fault. Its northward migration continues to this day. It is 669 miles long and extends from the mouth of the Colorado River in the north up to the southern end at Cabo San Lucas. Sediments from the Colorado River filled in a large delta at the northern end of the peninsula. It is today known as the Imperial Valley. This shortened the Baja peninsula which was originally much longer. Today it is 800 miles long and it is one of the longest peninsulas in the world. It is also very narrow – approximately 70 miles. The narrowest part is 26 miles wide. In the future, it can be expected that Baja California and the part of upper California west of the San Andreas fault will detach the continent and transform into a very long island. [edit] HistorySee also: Origin of the name California In the minds of European explorers California existed as an idea before it was discovered. The earliest known mention of the idea of California was in the 1510 romance novel Las Sergas de Esplandián by Spanish author Garci Rodríguez de Montalvo. The book described the Island of California as being west of the Indies, "very close to the side of the Terrestrial Paradise; and it is peopled by black women, without any man among them, for they live in the manner of Amazons." Following Hernán Cortés conquest of Mexico, the lure of an earthly paradise as well as the search for the fabled Strait of Anián, helped motivate him to send several expeditions to the west coast of New Spain in the 1530s and early 1540s. The first expedition reached the Gulf of California and California, and proved the Island of California was in fact a peninsula. Nevertheless, the idea of the island persisted for well over a century and was included in many maps. The Spaniards gave the name "California" to the peninsula and to the lands north, including both Baja California and Alta California, the region that became parts of the present-day U.S. states of California, Nevada, and others. [edit] PartitionNew Spain's province of California was divided into Alta California and Baja California on May 19, 1773 near San Juan Bautista Creek by Fray Francisco Palóu. A marker is erected in the place where the dividing committee began the measurements for the province's partition. The marker is behind the Misión San Miguel Arcángel de la Frontera, near Ensenada, Baja California. Translated into English, the inscription on the marker reads:
[edit] TerritoryThe whole peninsula of Baja California was a Spanish, then Mexican territory from 1804 until 1931. [edit] Timeline
[edit] Political divisionsThe peninsula is divided into two parts:
[edit] Geographic featuresA series of mountain ranges runs the length of the peninsula, which are known as the Peninsular Ranges, and extend into Southern California.
[edit] EcoregionsThe peninsula is home to several distinct ecoregions. Most of the peninsula is deserts and xeric shrublands, although pine-oak forests are found in the mountains at the northern and southern ends of the peninsula. The southern tip of the peninsula, which was formerly an island, has many species with affinities to tropical Mexico.
[edit] See also[edit] Notes
[edit] References
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