All Topics  
Cimmerian Plate

 
Cimmerian Plate

   Email Print
   Bookmark   Link






 

Cimmerian Plate



 
 
The Cimmerian Plate is an ancient tectonic plate
Tectonic Plate

#REDIRECT Plate tectonics...
 that comprises parts of present-day Anatolia
Anatolia

Anatolia or Asia Minor is a region of Western Asia, comprising most of the modern Republic of Turkey. It is a geographic region bounded by the Black Sea to the north, the Caucasus to the northeast, the Aegean Sea to the west, the Mediterranean Sea to the south, and the Iranian plateau to the east and southeast....
, Iran
Iran

Iran , officially the Islamic Republic of Iran and formerly known internationally as Persian Empire until 1935, is a country in Central Eurasia, located on the northeastern shore of the Persian Gulf and the southern shore of the Caspian Sea....
, Afghanistan
Afghanistan

Afghanistan , officially the Islamic republic of Afghanistan, is a landlocked country that is located approximately in the center of Asia....
, Tibet
Tibet

Tibet is a Tibetan Plateau in Asia, north of the Himalayas, and the home to the indigenous Tibetan people and its related ethnic groups. With an average elevation of 4,900 metres , it is the highest region on Earth and has in recent decades increasingly been referred to as the "Roof of the World"....
, Indochina
Indochina

Indochina, or the Indochinese Peninsula, is a subregion in Southeast Asia. It lies roughly east of India, south of China.The word has French origins, Indochine, and was adopted when French colonizers in Vietnam began expanding their territory to bordering countries....
 and Malaya
Malay Peninsula

The Malay Peninsula or Thai-Malay Peninsula is a major peninsula located in Southeast Asia. It is also known as the Kra Peninsula and runs approximately north-south through the Kra Isthmus....
 regions. The Cimmerian Plate was formerly part of the ancient supercontinent
Supercontinent

In geology, a supercontinent is a landmass comprising more than one continental core, or craton. The assembly of cratons and terrane that form Eurasia qualifies as a supercontinent today....
 of Pangaea
Pangaea

Pangaea, Pang?a or Pangea was the supercontinent that existed during the Paleozoic and Mesozoic eras about 250 million years ago, before the component continents were separated into their current configuration....
. Pangaea was shaped like a vast "C", facing east, and inside of the "C" was the Paleo-Tethys Ocean
Paleo-Tethys Ocean

The Paleo-Tethys Ocean was an ancient Paleozoic ocean. It was located between the paleocontinent Gondwana and the so called Hunic terranes. These are divided into the European Hunic and Asiatic Hunic ....
.






Discussion
Ask a question about 'Cimmerian Plate'
Start a new discussion about 'Cimmerian Plate'
Answer questions from other users
Full Discussion Forum



Encyclopedia


290 Global
The Cimmerian Plate is an ancient tectonic plate
Tectonic Plate

#REDIRECT Plate tectonics...
 that comprises parts of present-day Anatolia
Anatolia

Anatolia or Asia Minor is a region of Western Asia, comprising most of the modern Republic of Turkey. It is a geographic region bounded by the Black Sea to the north, the Caucasus to the northeast, the Aegean Sea to the west, the Mediterranean Sea to the south, and the Iranian plateau to the east and southeast....
, Iran
Iran

Iran , officially the Islamic Republic of Iran and formerly known internationally as Persian Empire until 1935, is a country in Central Eurasia, located on the northeastern shore of the Persian Gulf and the southern shore of the Caspian Sea....
, Afghanistan
Afghanistan

Afghanistan , officially the Islamic republic of Afghanistan, is a landlocked country that is located approximately in the center of Asia....
, Tibet
Tibet

Tibet is a Tibetan Plateau in Asia, north of the Himalayas, and the home to the indigenous Tibetan people and its related ethnic groups. With an average elevation of 4,900 metres , it is the highest region on Earth and has in recent decades increasingly been referred to as the "Roof of the World"....
, Indochina
Indochina

Indochina, or the Indochinese Peninsula, is a subregion in Southeast Asia. It lies roughly east of India, south of China.The word has French origins, Indochine, and was adopted when French colonizers in Vietnam began expanding their territory to bordering countries....
 and Malaya
Malay Peninsula

The Malay Peninsula or Thai-Malay Peninsula is a major peninsula located in Southeast Asia. It is also known as the Kra Peninsula and runs approximately north-south through the Kra Isthmus....
 regions. The Cimmerian Plate was formerly part of the ancient supercontinent
Supercontinent

In geology, a supercontinent is a landmass comprising more than one continental core, or craton. The assembly of cratons and terrane that form Eurasia qualifies as a supercontinent today....
 of Pangaea
Pangaea

Pangaea, Pang?a or Pangea was the supercontinent that existed during the Paleozoic and Mesozoic eras about 250 million years ago, before the component continents were separated into their current configuration....
. Pangaea was shaped like a vast "C", facing east, and inside of the "C" was the Paleo-Tethys Ocean
Paleo-Tethys Ocean

The Paleo-Tethys Ocean was an ancient Paleozoic ocean. It was located between the paleocontinent Gondwana and the so called Hunic terranes. These are divided into the European Hunic and Asiatic Hunic ....
. Two microcontinents, which are part of present-day China
China

China is a Culture of China, an ancient civilization, and, depending on perspective, a national or multinational entity extending over a large area in East Asia....
, lay in the eastern expanse of the Paleo-Tethys Ocean
Paleo-Tethys Ocean

The Paleo-Tethys Ocean was an ancient Paleozoic ocean. It was located between the paleocontinent Gondwana and the so called Hunic terranes. These are divided into the European Hunic and Asiatic Hunic ....
. About 300 Mya
Mya (unit)

In astronomy, geology, and paleontology, mya or "m.y.a." is an abbreviation for "million years ago". Like the related unit bya, mya is traditionally written in lower case....
 (million years ago), a rift
Rift

In geology, a rift is a place where the Earth's Crust and lithosphere are being pulled apart and is an example of extensional tectonics.Typical rift features are a central linear downdropped geologic fault segment, called a graben, with parallel normal faulting and rift-flank uplifts on either side forming a rift valley, where the rift r...
 started opening from the east which split a long, thin arc off of the inside of the southern arm of the continent, which comprised present day Australia
Australia

Australia, officially the Commonwealth of Australia, is a country in the southern hemisphere comprising the Australia of the world's smallest continent, the major island of Tasmania, and numerous list of islands of Australia in the Indian Ocean and Pacific Oceans....
, Antarctica
Antarctica

Antarctica is Earth's southernmost continent, overlying the South Pole. It is situated in the Antarctica of the southern hemisphere, almost entirely south of the Antarctic Circle, and is surrounded by the Southern Ocean....
, India
India

India, officially the Republic of India , is a country in South Asia. It is the List of countries and outlying territories by total area country by geographical area, the List of countries by population country, and the most populous liberal democracy in the world....
, and Africa
Africa

Africa is the world's second-largest and second most-populous continent, after Asia. At about 30.2 million km? including adjacent islands, it covers 6% of the Earth's total surface area and 20.4% of the total land area....
-Arabia. The new micro-continent is called Cimmeria
Cimmeria (continent)

Cimmeria was an ancient continent that existed about 200 million years ago. It rifted north from Gondwana during the Late Carboniferous and collided against eastern Laurasia during the Late Triassic together with the Chinese continents....
. Behind this new micro-continent the rift formed a new ocean, the Tethys Ocean
Tethys Ocean

The Tethys Ocean was an ocean that existed between the continents of Gondwana and Laurasia during the Mesozoic era before the opening of the Indian Ocean....
. As the Tethys Ocean widened, it pushed the Cimmeria and the floor of the Paleo-Tethys Ocean
Paleo-Tethys Ocean

The Paleo-Tethys Ocean was an ancient Paleozoic ocean. It was located between the paleocontinent Gondwana and the so called Hunic terranes. These are divided into the European Hunic and Asiatic Hunic ....
 northward towards Laurasia
Laurasia

Laurasia was a supercontinent that most recently existed as a part of the split of the Pangaean supercontinent in the late Mesozoic era . It included most of the landmasses which make up today's continents of the northern hemisphere, chiefly Laurentia , Baltica, Siberia , Kazakhstania, and the North China Craton and East China Craton craton...
, the northeastern arm of Pangaea.

249 Global
As it moved north, the floor of the Paleo-Tethys subducted
Subduction

In geology, subduction is the process that takes place at convergent boundary by which one tectonic plate moves under another tectonic plate, sinking into the Earth's mantle, as the plates converge....
 under Laurasia and Cimmeria
Cimmeria (continent)

Cimmeria was an ancient continent that existed about 200 million years ago. It rifted north from Gondwana during the Late Carboniferous and collided against eastern Laurasia during the Late Triassic together with the Chinese continents....
 eventually collided with Laurasia, first at its western end c. 220 Ma, and Paleo-Tethys began to disappear altogether, closing from west to east. The collision of the continents raised mountains along the suture, called the Cimmerian orogeny
Cimmerian Orogeny

The Cimmerian Orogeny, is an orogeny that created mountain ranges that now lie in Central Asia. The orogeny is believed to have begun 200 - 150 million years ago , when the Cimmeria collided with the southern coast of Kazakhstania and North China and South China , closing the ancient Paleo-Tethys Ocean between them....
. On its eastern end, Cimmeria collided with the Chinese micro-continents c. 200 Ma, and the Cimmerian orogeny was extended along the entire northern boundary of the plate. Most of Paleo-Tethys disappeared by c.150 Ma. More mountains were raised as the northern edge of the China plates collided with eastern Laurasia. After it collided with Laurasia around 200 Ma (Early Jurassic
Early Jurassic

The Early Jurassic epoch is the earliest of three epochs of the Jurassic period. The Early Jurassic starts immediately after the Triassic-Jurassic extinction event and ends at the start of the Middle Jurassic ....
), the Tethyan Trench
Tethyan Trench

The Tethyan Trench was an ancient oceanic trench that existed in the northern part of the Tethys Ocean during the middle Mesozoic to early Cenozoic eras....
 formed on southern Cimmeria, subducting the Tethys Ocean
Tethys Ocean

The Tethys Ocean was an ocean that existed between the continents of Gondwana and Laurasia during the Mesozoic era before the opening of the Indian Ocean....
 which created island arcs and new mountain range
Mountain range

A mountain range is a chain of mountains bordered by highlands or separated from other mountains by mountain pass or valleys. Individual mountains within the same mountain range do not necessarily have the same geology, though they often do; they may be a mix of different orogeny, for example volcanoes, uplifted mountains or Fold mountains...
s in the area.

100 Global
The Tethys rift eventually extended westward to split Pangaea in two, and the growing Atlantic Ocean
Atlantic Ocean

The Atlantic Ocean is the second-largest of the world's oceanic divisions; with a total area of about 106.4 million square kilometres . It covers approximately one-fifth of the Earth's surface....
 separated the northern supercontinent of Laurasia from the southern supercontinent Gondwana. Around 150 Ma Gondwana also began to rift apart c. 150 Ma, and the continents of India and Africa-Arabia began to drift north towards Laurasia, of which Cimmeria
Cimmeria (continent)

Cimmeria was an ancient continent that existed about 200 million years ago. It rifted north from Gondwana during the Late Carboniferous and collided against eastern Laurasia during the Late Triassic together with the Chinese continents....
 now formed the southern coast. Africa-Arabia and India eventually collided with Asia c. 30 Ma, reuniting Cimmeria with its former Gondwanian neighbors and buckling and folding the former Cimmerian continent to form the Alps
Alps

The Alps is the name for one of the great mountain range systems of Europe, stretching from Austria and Slovenia in the east; through Italy, Switzerland, Liechtenstein and Germany; to France in the west....
, Caucasus
Caucasus

The Caucasus or Caucas is a geopolitical region located between Europe, Asia, and the Middle East. It is home to Europe's highest mountain ....
, Zagros Mountains
Zagros Mountains

The Zagros , are the largest mountain range in Iran and Iraq. They have a total length of 1 500 km from western Iran, on the border with Iraq to the southern parts of the Persian Gulf....
, Hindu Kush
Hindu Kush

The Hindu Kush is a mountain range located in eastern and central Afghanistan, northwestern Pakistan and northeastern India.The origin of the name Hindu Kush is disputed, despite its coinage apparently dating back no further than c.1330....
, and Himalaya (this is called the Alpine orogeny
Alpine orogeny

The Alpine orogeny is an orogeny phase in the Tertiary that formed the mountain ranges of the Alpide belt. These mountains include the Atlas Mountains, the Pyrenees, the Alps, the Dinaric Alps, the Pindus, the Carpathians, the Balkan Mountains, the Taurus Mountains, the Caucasus Mountains, the Alborz, the Zagros Mountains, the Hindu Kush, t...
).

See also

  • Geology of the Himalaya
    Geology of the Himalaya

    The geology of the Himalaya is a record of the most dramatic and visible creations of modern plate tectonic forces. The Himalayas, which stretch over 2400 km between the Namche Barwa syntaxis in Tibet and the Nanga Parbat syntaxis in Pakistan, are the result of an ongoing orogeny ? the result of a collision between two continenta...


External links

    • showing the expanding Tethys Ocean, the closure of Paleo-Tethys, and the movement of the Cimmerian Plate
    • showing the a narrow seaway of Paleo-Tethys Ocean, and beginnings of the Cimmerian Orogeny
      Cimmerian Orogeny

      The Cimmerian Orogeny, is an orogeny that created mountain ranges that now lie in Central Asia. The orogeny is believed to have begun 200 - 150 million years ago , when the Cimmeria collided with the southern coast of Kazakhstania and North China and South China , closing the ancient Paleo-Tethys Ocean between them....