Göbekli Tepe and Holocene

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Difference between Göbekli Tepe and Holocene

Göbekli Tepe vs. Holocene

Göbekli Tepe, Turkish for "Potbelly Hill", is an archaeological site in the Southeastern Anatolia Region of Turkey, approximately northeast of the city of Şanlıurfa. The Holocene is the current geological epoch.

Jericho

Jericho (יְרִיחוֹ; أريحا) is a city in the Palestinian Territories and is located near the Jordan River in the West Bank.

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Natufian culture

The Epipaleolithic Natufian culture existed from around 12,500 to 9,500 BC in the Levant, a region in the Eastern Mediterranean.

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Neolithic

The Neolithic was a period in the development of human technology, beginning about 10,200 BC, according to the ASPRO chronology, in some parts of Western Asia, and later in other parts of the world and ending between 4500 and 2000 BC.

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Neolithic Revolution

The Neolithic Revolution, Neolithic Demographic Transition, Agricultural Revolution, or First Agricultural Revolution, was the wide-scale transition of many human cultures during the Neolithic period from a lifestyle of hunting and gathering to one of agriculture and settlement, making an increasingly larger population possible.

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Pleistocene

The Pleistocene (often colloquially referred to as the Ice Age) is the geological epoch which lasted from about 2,588,000 to 11,700 years ago, spanning the world's most recent period of repeated glaciations.

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Pre-Pottery Neolithic A

Pre-Pottery Neolithic A (PPNA) denotes the first stage in early Levantine and Anatolian Neolithic culture, dating BP.

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Pre-Pottery Neolithic B

Pre-Pottery Neolithic B (PPNB) is a Neolithic culture centered in upper Mesopotamia.

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Prehistory

Human prehistory is the period between the use of the first stone tools 3.3 million years ago by hominins and the invention of writing systems.

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Radiocarbon dating

Radiocarbon dating (also referred to as carbon dating or carbon-14 dating) is a method for determining the age of an object containing organic material by using the properties of radiocarbon, a radioactive isotope of carbon.

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Younger Dryas

The Younger Dryas (c. 12,900 to c. 11,700 years BP) was a return to glacial conditions which temporarily reversed the gradual climatic warming after the Last Glacial Maximum started receding around 20,000 BP.

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