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An ash pit may sometimes be detected by the presence of white ash or swarms of insects hovering about. Nearly translucent smoke that quickly dissipates may be visible emanating from an ash pit when it is between the observer and the sun. Due to incomplete burning, an ash pit may also produce a smell of burning creosote or incomplete combustion.
Both human and animal skeletons were found in deep oval shaped pits, located either below the floors of the dwelling units or in its precincts. These pits were filled with ash, stones and potsherds. Some of the human skulls found here had trepanning (bored hole) marks. In many pits, bones of dogs and antlered deer were found along with human ...
Ash dump—An opening in a hearth to sweep ashes for later removal from the ash pit. [21] Back (fireback)—The inside, rear wall of the fireplace of masonry or metal that reflects heat into the room. [21] Brick trimmer—A brick arch supporting a hearth or shielding a joist in front of a fireplace. [21]
The fall of ash drifted downwind from the Bruneau-Jarbidge supervolcano eruption (in present-day Idaho), nearly 1,000 miles (1,600 km) west of the Ashfall site. A large number of very well preserved fossil Teleoceras (extinct hippo-like relatives of rhinos ), small three-toed and one-toed horses , camels , and birds have been excavated.
The Ash Pit is an inactive volcanic crater on the southern edge of the Kitsu Plateau in British Columbia, Canada. It is Holocene in age and may be the youngest feature of the Mount Edziza volcanic complex. It is within the Northern Cordilleran Volcanic Province and is part of the Pacific Ring of Fire, that includes over 160 active volcanoes.
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Amphicyonidae is an extinct family of terrestrial carnivorans belonging to the suborder Caniformia.They first appeared in North America in the middle Eocene (around 45 mya), spread to Europe by the late Eocene (35 mya), and further spread to Asia and Africa by the early Miocene (23 mya).
Neolithic ashmounds (sometimes termed as cinder mounds [1]) are man-made landscape features found in some parts of southern India (chiefly around Bellary) that have been dated to the Neolithic period (3000 to 1200 BC).