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Getting a portable lantern is the easiest way to ensure you won't be caught unprepared. Lanterns can cost you, but not today: Amazon has slashed prices up to 40% off top-rated Lighting Ever ...
Abyssal (or submarine) fans are formed from turbidity currents. These currents begin when a geologic activity pushes sediments over the edge of a continental shelf and down the continental slope, creating an underwater landslide. A dense slurry of muds and sands speeds towards the foot of the slope, until the current slows. The decreasing ...
The rattail Coryphaenoides armatus (abyssal grenadier) on the Davidson Seamount at a depth of 2,253 metres (7,392 ft). Deep-sea species exhibit lower changes of entropy and enthalpy compared to surface level organisms, since a high pressure and low temperature environment favors negative enthalpy changes and reduced dependence on entropy-driven ...
Fate/strange Fake is a Japanese light novel series in Type-Moon's Fate franchise, written by Ryōgo Narita and illustrated by Morii Shizuki. [1]It was originally placed on Narita's homepage under the title of "Fake/states night" on April 1, 2008, presented as a prologue and introduction for a role playing style game as an April Fool's prank.
Fulgora laternaria can reach a length of 85–90 millimetres (3.3–3.5 in), with a wingspan up to 100–150 millimetres (3.9–5.9 in). This insect has a protuberance at its head as long as 10–15 millimetres (0.39–0.59 in), looking like a peanut and showing false eyes to resemble that of a lizard or a serpent.
Paulding Light. The Paulding Light (also called the Lights of Paulding or the Dog Meadow Light) is a light that appears in a valley outside Paulding, Michigan.Reports of the light have appeared since the 1960s, with popular folklore providing such explanations as ghosts, geologic activity, or swamp gas.
The sediment distribution and deposition patterns of oozes inform scientists about prehistoric areas of the oceans that exhibited prime conditions for the growth of siliceous organisms. [9] Scientists examine paleo-ooze by taking cores of deep sea sediments. [9] Sediment layers in these cores reveal the deposition patterns of the ocean over time.
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