2016
Historic and ancient tsunamis uncovered on the Jalisco-Colima Pacific coast, the Mexican subduction zone
RAMÍREZ-HERRERA, María Teresa, María-Felicidad BÓGALO, Jan ČERNÝ, Avto GOGUITCHAICHVILI, Néstor CORONA et. al.Základní údaje
Originální název
Historic and ancient tsunamis uncovered on the Jalisco-Colima Pacific coast, the Mexican subduction zone
Autoři
RAMÍREZ-HERRERA, María Teresa (484 Mexiko), María-Felicidad BÓGALO (724 Španělsko), Jan ČERNÝ (203 Česká republika, garant, domácí), Avto GOGUITCHAICHVILI (268 Gruzie), Néstor CORONA (484 Mexiko), María Luisa MACHAIN (484 Mexiko), Arturo Carranza EDWARDS (484 Mexiko) a Susana SOSA (484 Mexiko)
Vydání
Geomorphology, Amsterdam, Elsevier, 2016, 0169-555X
Další údaje
Jazyk
angličtina
Typ výsledku
Článek v odborném periodiku
Obor
10500 1.5. Earth and related environmental sciences
Stát vydavatele
Nizozemské království
Utajení
není předmětem státního či obchodního tajemství
Odkazy
Impakt faktor
Impact factor: 2.958
Kód RIV
RIV/00216224:14310/16:00089892
Organizační jednotka
Přírodovědecká fakulta
UT WoS
000374199000008
Klíčová slova anglicky
Tsunami deposit; Mexican subduction; Earthquake; Magnetic properties
Příznaky
Mezinárodní význam, Recenzováno
Změněno: 21. 1. 2020 09:10, Mgr. Marie Šípková, DiS.
Anotace
V originále
Research on extreme wave events such as tsunamis using the geological record in areas of infrequent and or small magnitude earthquakes can aid in extending the long-term history and recurrence intervals of large events. This information is valuable for risk management and community preparedness in coastal areas. Here we investigate tsunami deposits on the Jalisco coast of Mexico that overlies the subducting Rivera Plate under the North American plate, an area due for a large thrust earthquake and potential tsunami. Here, we apply a full battery of rock-magnetic analyses that also include a detailed AMS study and other typically applied proxies in tsunami deposits research. We present evidence to demonstrate that anomalous sand units with sharp basal contacts at La Manzanilla, Tenacatita Bay, and El Tecuán shore sites on the Jalisco coast may be the products of tsunamis generated by known historical (Ms 8.2 earthquake of 3 June 1932) and other earlier tsunamigenic earthquakes. A sandy unit with a sharp basal contact, flame structures at the base, rip-up clasts at La Manzanilla, and four sand units with sharp basal contact overlying buried soils at El Tecuán, together with other proxies, such as magnetic properties and others, suggest tsunami deposits. 210Pb dating of sediments slightly above the upper sand layer indicate an age A.D. 1935 ± 11 at El Tecuán. Historical accounts of tsunami inundation at both sites provide further evidence that this is most probably the result of the 3 June 1932 tsunami. Hence this study may provide the first evidence of a tsunami triggered by this earthquake and also of three probable predecessors. Further evidence of at least three earlier tsunamis that occurred since the fifteenth century is also evident in the stratigraphy. These events may correspond to events listed in historical archives, namely the 1563, 1816, and/or the 1818 events.