The Serranía del Baudó is a coastal mountain range on the Pacific coast of Colombia . It is separated from the West Andes by the Atrato valley where the Atrato River flows and Quibdó is located. From the south the range extends from the Baudó River north and slightly west along the coast into Panama terminating at the Golfo de San Miguel. The range is called Serranía del Sapo when it is in Panama. Technically the landform extends south of the Baudó River down to Malaga Bay, but the area has been eroded into low hills and marshlands.
4-561: Baudo may refer to{ Places [ edit ] Baudó Mountains , a mountain range on the Pacific coast of Colombia Baudó River in Colombia People [ edit ] Pippo Baudo , Italian TV personality Serge Baudo , French conductor Animal species [ edit ] Baudó oropendola , bird species Baudo guan , bird species See also [ edit ] Boudot ,
8-532: A surname Topics referred to by the same term [REDACTED] This disambiguation page lists articles associated with the title Baudo . If an internal link led you here, you may wish to change the link to point directly to the intended article. Retrieved from " https://en.wikipedia.org/w/index.php?title=Baudo&oldid=1038069012 " Categories : Disambiguation pages Place name disambiguation pages Disambiguation pages with surname-holder lists Hidden categories: Short description
12-496: Is different from Wikidata All article disambiguation pages All disambiguation pages Baud%C3%B3 Mountains From Cabo Corrientes north to Punta Ardita and on into Panama the Baudó Mountains meet the ocean in steep cliffs, rising up to as high as 70 m (230 ft), with small indentations in the coast providing small pocket beaches , some sandy, but most are shingle or cobble. However, near river mouths
16-669: The coast has been eroded and there are wide sandy beaches, tidal flats and even mangrove swamps. The highest point, Alto de Buey, is 1,810 m (5,940 ft). Geologically, the Serranía del Baudó represents an extension of the Isthmus of Panama . The mountain range started forming in the Late Cretaceous and Paleocene from oceanic volcanics that were compacted as the Nazca Plate and later Malpelo Plate pushed westward into and under
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