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Adriatic Plate

Index Adriatic Plate

The Adriatic or Apulian Plate is a small tectonic plate carrying primarily continental crust that broke away from the African plate along a large transform fault in the Cretaceous period. [1]

19 relations: Adriatic Sea, African Plate, Alpine orogeny, Continental collision, Continental crust, Cretaceous, Deformation (engineering), Eurasian Plate, Fault (geology), Italian Peninsula, Limestone, Mesozoic, Oceanic crust, Periadriatic Seam, Plate tectonics, Sedimentary rock, Slovenia, Southern Limestone Alps, Transform fault.

Adriatic Sea

The Adriatic Sea is a body of water separating the Italian Peninsula from the Balkan peninsula.

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African Plate

The African Plate is a major tectonic plate straddling the equator as well as the prime meridian.

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Alpine orogeny

The Alpine orogeny or Alpide orogeny is an orogenic phase in the Late Mesozoic (Eoalpine) and the current Cenozoic that has formed the mountain ranges of the Alpide belt.

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Continental collision

Continental collision is a phenomenon of the plate tectonics of Earth that occurs at convergent boundaries.

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Continental crust

Continental crust is the layer of igneous, sedimentary, and metamorphic rocks that forms the continents and the areas of shallow seabed close to their shores, known as continental shelves.

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Cretaceous

The Cretaceous is a geologic period and system that spans 79 million years from the end of the Jurassic Period million years ago (mya) to the beginning of the Paleogene Period mya.

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Deformation (engineering)

In materials science, deformation refers to any changes in the shape or size of an object due to-.

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Eurasian Plate

The Eurasian Plate is a tectonic plate which includes most of the continent of Eurasia (a landmass consisting of the traditional continents of Europe and Asia), with the notable exceptions of the Indian subcontinent, the Arabian subcontinent, and the area east of the Chersky Range in East Siberia.

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Fault (geology)

In geology, a fault is a planar fracture or discontinuity in a volume of rock, across which there has been significant displacement as a result of rock-mass movement.

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Italian Peninsula

The Italian Peninsula or Apennine Peninsula (Penisola italiana, Penisola appenninica) extends from the Po Valley in the north to the central Mediterranean Sea in the south.

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Limestone

Limestone is a sedimentary rock, composed mainly of skeletal fragments of marine organisms such as coral, forams and molluscs.

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Mesozoic

The Mesozoic Era is an interval of geological time from about.

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Oceanic crust

Oceanic crust is the uppermost layer of the oceanic portion of a tectonic plate.

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Periadriatic Seam

The Periadriatic Seam (or fault) is a distinct geologic fault in Southern Europe, running S-shaped about 1000 km from the Tyrrhenian Sea through the whole Southern Alps as far as Hungary.

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Plate tectonics

Plate tectonics (from the Late Latin tectonicus, from the τεκτονικός "pertaining to building") is a scientific theory describing the large-scale motion of seven large plates and the movements of a larger number of smaller plates of the Earth's lithosphere, since tectonic processes began on Earth between 3 and 3.5 billion years ago.

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Sedimentary rock

Sedimentary rocks are types of rock that are formed by the deposition and subsequent cementation of that material at the Earth's surface and within bodies of water.

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Slovenia

Slovenia (Slovenija), officially the Republic of Slovenia (Slovene:, abbr.: RS), is a country in southern Central Europe, located at the crossroads of main European cultural and trade routes.

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Southern Limestone Alps

The Southern Limestone Alps (Italian: Alpi Sud-orientali) are the ranges of the Eastern Alps south of the Central Eastern Alps mainly located in northern Italy and the adjacent lands of Austria and Slovenia.

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Transform fault

A transform fault or transform boundary is a plate boundary where the motion is predominantly horizontal.

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Redirects here:

Adriatic lithosphere, Adriatic plate, Apulian Plate, Apulian plate.

References

[1] https://en.wikipedia.org/wiki/Adriatic_Plate

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