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Tell Barri, northeastern Syria, from the west; this is 32 meters (105 feet) high, and its base covers 37 hectares (91 acres) Tel Be'er Sheva, Beersheva, Israel. In archaeology, a tell (from Arabic: تَلّ, tall, 'mound' or 'small hill') [1] is an artificial topographical feature, a mound [a] consisting of the accumulated and stratified debris of a succession of consecutive settlements at the ...
Temple Mount Sifting Project, The Masu'ot Lookout. The Temple Mount Sifting Project (TMSP; formerly known as the Temple Mount Salvage Operation) is an archaeological project begun in 2004 whose aim is the recovery and study of archaeological artifacts contained within debris which were removed from the Temple Mount in Jerusalem without proper archaeological care.
Note "out of phase" pipe intrusion left in for practical reasons Excavation in phase has reduced this site to the occupation level of a Romano-Celtic temple (56 Gresham Street, London) Phase is the most easily understood grouping for the layman as it implies a near contemporaneous Archaeological horizon representing "what you would see if you ...
Archaeologists have uncovered the remains of two more victims of the notoriously deadly Mount Vesuvius eruption that buried Pompeii in 79 A.D.
Monte Testaccio (Italian pronunciation: [ˈmonte teˈstattʃo]) [1] or Monte Testaceo, also known as Monte dei Cocci, is an artificial mound in Rome composed almost entirely of testae (Italian: cocci), fragments of broken ancient Roman pottery, nearly all discarded amphorae dating from the time of the Roman Empire, some of which were labelled with tituli picti.
Great Bath, Mohenjo-daro A water well in Lothal Water reservoir, with steps, at Dholavira, Gujarat, India. The ancient Indus Valley Civilization in the Indian subcontinent (located in present-day eastern-Pakistan and north-India) was prominent in infrastructure, hydraulic engineering, and had many water supply and sanitation devices that are the first known examples of their kind.
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The Younger Dryas impact hypothesis (YDIH) proposes that the onset of the Younger Dryas (YD) cool period at the end of the Last Glacial Period, around 12,900 years ago was the result of some kind of cosmic event with specific details varying between publications. [1]: