Messinian salinity crisis (Paleogeography 🦕)

The Messinian salinity crisis was an event in which the Mediterranean Sea went into a cycle of partial or nearly complete desiccation throughout the latter part of the Messinian age of the Miocene epoch, from 5.96 to 5.33 Ma. It ended with the Zanclean flood, when the Atlantic reclaimed the basin. Sediment samples from be...

https://en.wikipedia.org/wiki/Messinian_salinity_crisis

#MessinianSalinityCrisis #Messinian #Paleogeography #RegionalGeology

Messinian salinity crisis (Paleogeography 🦕)

The Messinian salinity crisis was an event in which the Mediterranean Sea went into a cycle of partial or nearly complete desiccation throughout the latter part of the Messinian age of the Miocene epoch, from 5.96 to 5.33 Ma. It ended with the Zanclean flood, when the Atlantic reclaimed the basin. Sediment samples from be...

https://en.wikipedia.org/wiki/Messinian_salinity_crisis

#MessinianSalinityCrisis #Messinian #Paleogeography #RegionalGeology

Messinian erosional crisis (Paleogeography 🦕)

The Messinian Erosional Crisis is a phase in the Messinian evolution of the central Mediterranean basin resulting from major drawdown of the Mediterranean seawater. As outlined in numerous studies, erosional events along the margins of the Mediterranean Basin during the Messinian timespan, before and during the evaporit...

https://en.wikipedia.org/wiki/Messinian_erosional_crisis

#MessinianErosionalCrisis #Messinian #Paleogeography #RegionalGeology

Messinian salinity crisis (Paleogeography 🦕)

The Messinian salinity crisis was an event in which the Mediterranean Sea went into a cycle of partial or nearly complete desiccation throughout the latter part of the Messinian age of the Miocene epoch, from 5.96 to 5.33 Ma. It ended with the Zanclean flood, when the Atlantic reclaimed the basin. Sediment samples from be...

https://en.wikipedia.org/wiki/Messinian_salinity_crisis

#MessinianSalinityCrisis #Messinian #Paleogeography #RegionalGeology

Betic corridor (Paleogeography 🦕)

The Betic Corridor, or North-Betic Strait, was a strait of water connecting the Mediterranean Sea with the Atlantic Ocean that once separated the Iberian plate from the Eurasian Plate through the Betic Cordillera. Its closure approximately 5.96 million years ago during the Messinian period of the Miocene epoch, precipitate...

https://en.wikipedia.org/wiki/Betic_corridor

#BeticCorridor #Messinian #BaeticSystem #Paleogeography #RegionalGeology #GeologyOfTheAlps

Messinian salinity crisis (Paleogeography 🦕)

The Messinian salinity crisis was a geological event during which the Mediterranean Sea went into a cycle of partial or nearly complete desiccation throughout the latter part of the Messinian age of the Miocene epoch, from 5.96 to 5.33 Ma. It ended with the Zanclean flood, when the Atlantic reclaimed the basin. Sediment sa...

https://en.wikipedia.org/wiki/Messinian_salinity_crisis

#MessinianSalinityCrisis #Messinian #Paleogeography #RegionalGeology

Messinian erosional crisis (Paleogeography 🦕)

The Messinian Erosional Crisis is a phase in the Messinian evolution of the central Mediterranean basin resulting from major drawdown of the Mediterranean seawater. As outlined in numerous studies, erosional events along the margins of the Mediterranean Basin during the Messinian timespan, before and during the evaporit...

https://en.wikipedia.org/wiki/Messinian_erosional_crisis

#MessinianErosionalCrisis #Messinian #Paleogeography #RegionalGeology