SODOME ET GOMORRHE ET PLAQUES TECTONIQUES

L'auteur a réalisé une recherche géomorphologique sur les causes de la destruction des cités antiques de Sodome et Gomorrhe sur les rives de la Mer Morte. Ceci a été l'objet despuis l'antiquité de recherches et d'études bibliques qui ont été poursuivies de nos jours pars des études scientifiques. Une aproximation géomorphologique est proposée par l'auteur arguant des raisons tectoniques comme base de cette destruction et effacement des cités.

Mots clés:
Tectonique; failles de décrochement; Paléo-Climat

Authorship

Jean Pierre BERGOEING ^*(*)CORRESPONDING AUTHOR: Address: Universidad de Costa Rica - San Pedro Montes de Oca, San José, Costa Rica. Tel: (+00) 50686290712. E-mail: jegadana@gmail.com

Phd in Geography. Professor of the University of Costa Rica, San Jose, Costa Rica. CURRICULUM LATTES: https://www.researchgate.net/profile/Jean_BergoeingUniversity of Costa RicaCosta RicaSan Jose, Costa RicaPhd in Geography. Professor of the University of Costa Rica, San Jose, Costa Rica. CURRICULUM LATTES: https://www.researchgate.net/profile/Jean_Bergoeing

https://orcid.org/0000-0003-2079-6790

(*)CORRESPONDING AUTHOR: Address: Universidad de Costa Rica - San Pedro Montes de Oca, San José, Costa Rica. Tel: (+00) 50686290712. E-mail: jegadana@gmail.com

SCIMAGO INSTITUTIONS RANKINGS

Figures

Figures (4)

Thumbnail

Figure 1
African and Arabian tectonic plates colliding with the European plate, and forming a system of sliding tectonic faults. The Arabian plate slides North as the African plate makes it Southward. The Red Sea was formed during the Miocene and an important volcanism characterizes the western sector of the Arab Peninsula during the Pleistocene . In this figure lies the Dead Sea which is a tectonic depression product o landslides in opposite directions of the African and Arab plates. (BERGOEING, 2016BERGOEING, Jean Pierre. Geomorphology and volcanology of Costa Rica. New York: Elsevier Edit, 2017).

Thumbnail

Figure 2
Dead Sea tectonic area sector of the sliding African and Arabic plates, which has resulted in a tectonic depression occupied in part by the Dead Sea. (Tectonics and Geology of the Dead Sea. Https://woodshole.er.usgs.)

Thumbnail

Figure 3
Geological cut of the Dead Sea, located in a Miocene tectonic depression and resting on a base of granite and basalts on which more recent calcareous sedimentary rocks overlap. The Western bleed fault moves Southward while the eastern transforming fault is headed North. (Hernán Toledo, 2016TOLEDO, Hernán M. El Mar Muerto está Reviviendo ¿Se cumplirá pronto la Profecía? Breaking Israel News 2016..)

Thumbnail

Figure 4
Dead Sea, seen from Jordan. Waters are descending 1 meter per year. Photo: Kevin Connolly BBC. June 17th, 2016.

Figure 1 African and Arabian tectonic plates colliding with the European plate, and forming a system of sliding tectonic faults. The Arabian plate slides North as the African plate makes it Southward. The Red Sea was formed during the Miocene and an important volcanism characterizes the western sector of the Arab Peninsula during the Pleistocene . In this figure lies the Dead Sea which is a tectonic depression product o landslides in opposite directions of the African and Arab plates. (BERGOEING, 2016BERGOEING, Jean Pierre. Geomorphology and volcanology of Costa Rica. New York: Elsevier Edit, 2017).

Figure 2 Dead Sea tectonic area sector of the sliding African and Arabic plates, which has resulted in a tectonic depression occupied in part by the Dead Sea. (Tectonics and Geology of the Dead Sea. Https://woodshole.er.usgs.)

Figure 3 Geological cut of the Dead Sea, located in a Miocene tectonic depression and resting on a base of granite and basalts on which more recent calcareous sedimentary rocks overlap. The Western bleed fault moves Southward while the eastern transforming fault is headed North. (Hernán Toledo, 2016TOLEDO, Hernán M. El Mar Muerto está Reviviendo ¿Se cumplirá pronto la Profecía? Breaking Israel News 2016..)

Figure 4 Dead Sea, seen from Jordan. Waters are descending 1 meter per year. Photo: Kevin Connolly BBC. June 17th, 2016.

How to cite

copy

Universidade Federal do Ceará UFC - Campi do Pici, Bloco 911, 60440-900 Fortaleza, Ceará, Brasil, Tel.: (55 85) 3366 9855, Fax: (55 85) 3366 9864 - Fortaleza - CE - Brazil
E-mail: edantas@ufc.br

Acompanhe os números deste periódico no seu leitor de RSS

Versão para download de PDF

PDF

Inglês

Versões e tradução automática

Versão original do texto

English

Tradução automática

Google Translator
Microsoft Translator

Como citar

RIS

BIBTEX

Outros formatos de citação e exportação:

SciELO - Scientific Electronic Library Online
Rua Dr. Diogo de Faria, 1087 – 9º andar – Vila Clementino 04037-003 São Paulo/SP - Brasil
E-mail: scielo@scielo.org

Leia a Declaração de Acesso Aberto

Métricas

SODOME ET GOMORRHE ET PLAQUES TECTONIQUES

PlumX

Mensagem

[1] (*)CORRESPONDING AUTHOR: Address: Universidad de Costa Rica - San Pedro Montes de Oca, San José, Costa Rica. Tel: (+00) 50686290712. E-mail: jegadana@gmail.com