Alpide Belt

Alpide belt
Alpine-Himalayan orogenic belt
Approximate extent of the Alpide orogenic system
Highest point
Peak	Mount Everest
Elevation	8,848.86 m (29,031.7 ft)
Dimensions
Length	15,000 km (9,300 mi) E–W in the west, N–S in the east
Naming
Etymology	Derived from Alps
Geography
Mesozoic oceanic platform	Southern Eurasia, northern Africa, central Asian subcontinent, southeast Asia
Geology
Formed by	compressive forces at aligned convergent plate boundaries
Orogeny	Alpine (in west), Himalayan (in east)
Mountain type	Folded mountain ranges

It includes, from west to east, the major ranges of the Atlas Mountains, the Alps, the Caucasus Mountains, Alborz, Hindu Kush, Karakoram, and the Himalayas. It is the second most seismically active region in the world, after the circum-Pacific belt (the Ring of Fire), with 17% of the world's largest earthquakes.

The belt is the result of Mesozoic-to-Cenozoic-to-recent closure of the Tethys Ocean and process of collision between the northward-moving African, Arabian, and Indian Plates with the Eurasian Plate. Each collision results in a convergent boundary, a topic covered in plate tectonics. The approximate alignment of so many convergent boundaries trending east to west, first noticed by the Austrian geologist Eduard Suess, suggests that once many plates were one plate, and the collision formed one subduction zone, which was oceanic, subducting the floor of Tethys.^{[citation needed]}

Suess called the single continent Gondwana, after some rock formations in India, then part of the supercontinent of Gondwana, which had earlier divided from another supercontinent, Laurasia, and was now pushing its way back. Eurasia descends from Laurasia, the Laurentia part having split away to the west as a consequence of the formation of the North Atlantic Ocean. As Tethys closed, Gondwana pushed up mountain ranges on the southern margin of Eurasia.

The Alpide belt is a concept from modern historical geology, the study in geologic time of the events that shaped the surface of the Earth. The topic began suddenly in the mid-19th century with the evolutionary biologists. The early historical geologists, such as Charles Darwin and Charles Lyell, arranged fossils and layers of sedimentary rock containing them into time periods, of which the framework remains.

The late 19th century was a period of synthesis, in which geologists attempted to combine all the detail into the big picture. The first of his type, Eduard Suess, used the term "comparative orography" to refer to his method of comparing mountain ranges, parallel to "comparative anatomy" and "comparative philology.

His work preceded plate tectonics and continental drift. This pre-tectonic phase lasted until about 1950, when the drift theory won the field just as suddenly as had the evolutionist. The concepts and language of the comparative graphists were kept with some modification, but were explained in new ways.

Suess's subsidence theory

The author of the concept of a trans-Eurasian zone of subsidence, which he called Tethys, was Eduard Suess. He knew it had been a subsidence because it expressed deposits of the Mesozoic, now indurated into layers and raised into highlands by compressional force. Suess had discovered the zone during his early work on the Alps. He spent the better part of his career following the zone in detail, which he assembled in one ongoing work, das Antlitz der Erde, "The Face of the Earth." Like a human face, the Earth's face has lineaments. Suess's topic was the definition and classification of the lineaments of this zone, which he traced from one end of Eurasia to the other, ending on the east with the Malay Peninsula.

Suess looked, as did all geologists, at the strata and content of sedimentary rock, deposited as sediment in the oceanic basins, indurated under the pressure of the depths, and raised later under horizontal pressure into folds of mountain chains. What he added to the field is the study of what he called the "trend-lines" or directions of mountains chains. These were to be discovered by examining their strikes, or intersections with the surface. He soon discovered what are known today as convergent plate borders, which are chains of mountains raised by the compression or subduction of one plate under another, but knowledge was not in such a state that he could recognize them as that. He concerned himself instead with the patterns.

• Cantabrian Mountains (incl. the Basque Mountains), Sistema Central, Sistema Ibérico, Pyrenees, Alps, Carpathians, Balkan Mountains (Balkanides), Rila-Rhodope massifs, Thracian Sea islands, Crimean Mountains – entirely in Europe
• Atlas and Rif Mountains in Northern Africa, Baetic System (Sierra Nevada and Balearic Islands), Apennine Mountains, Dinaric Alps, Pindus (Hellenides), and Mount Ida;
• Caucasus Mountains (on the limits between Asia and Europe), Kopet Mountains, Pamir, Alay Mountains, Tian Shan, Altai Mountains, Sayan Mountains;
• Pontic Mountains, Armenian Highlands, Alborz, Hindu Kush, Kunlun Mountains, Hengduan Mountains, Annamite Range, Titiwangsa Mountains, Barisan Mountains – entirely in Asia;
• Taurus Mountains, Troodos Mountains, Zagros Mountains, Makran Highland, Sulaiman Mountains, Karakoram, Himalayas, Transhimalaya, Patkai, Chin Hills, Arakan Mountains, Andaman and Nicobar Islands – entirely in Asia.

Indonesia lies between the Pacific Ring of Fire along the northeastern islands adjacent to and including New Guinea and the Alpide belt along the south and west from Sumatra, Java and the Lesser Sunda Islands (Bali, Flores, and Timor). The 2004 Indian Ocean earthquake just off the coast of Sumatra was located within the Alpide belt.

The word Alpide is a term first coined in German by Austrian geologist Eduard Suess in his 1883 magnum opus Das Antlitz der Erde and later popularized in English-language scientific literature by Turkish geologist and historian A. M. Celâl Şengör in a 1984 paper on the topic. The term adds the suffix -ides, derived from the Ancient Greek patronymic/familial suffix -ίδης (-ídēs), to the Alps, suggesting a "family" of related orogens. The term belt refers to the fact that the Alpides form a long, mostly unbroken chain of orogens running west to east along the southern edge of Eurasia.

If "Alpide" is taken in Kober's sense to mean the last and current of a collective group of contemporaneous ridges over the entire Tethyan region, then "Alpine orogeny" is used collectively of all the orogenies required to create the Alpides, a definition that is far from the original meanings of Alpide and Alpine, representing a specialized geologic usage.

• Geology of the Alps – The formation and structure of the European Alps