2020
DOI: 10.3390/jmse8090669
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Cispatá Bay and Mestizos Evolution as Reconstructed from Old Documents and Maps (16th–20th Century)

Abstract: Historical cartography is increasingly being used for the study of coastal evolution, but less considered are coeval descriptive sources as well as exploration reports that accompany the construction of maps. Herein, these issues are considered when analyzing the chronological model of the Rio Sinú mouth and Cispatá bay evolution before the Tinajones delta formed (around 1942–1943) as it is established in the literature. This study is based on the examination of about 500 manuscripts or printed maps produced f… Show more

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Cited by 4 publications
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“…Cispatá Bay is located in the Colombian Caribbean Coast, enclosed in The Mestizos peninsula on the western side of the Morrosquillo Gulf (Figure 1), Cordoba department, between 09°25'12"-09°20'8"N and 75°47'37"-75°55'30"W [7,8]. The Bay is a Holocene depositional landform formed by Rio Sinú before its diversion occurred between 1937 and 1945, when the Tinajones delta started to grow [6].…”
Section: Area Of Studymentioning
confidence: 99%
“…Cispatá Bay is located in the Colombian Caribbean Coast, enclosed in The Mestizos peninsula on the western side of the Morrosquillo Gulf (Figure 1), Cordoba department, between 09°25'12"-09°20'8"N and 75°47'37"-75°55'30"W [7,8]. The Bay is a Holocene depositional landform formed by Rio Sinú before its diversion occurred between 1937 and 1945, when the Tinajones delta started to grow [6].…”
Section: Area Of Studymentioning
confidence: 99%