The Asgard have constant dependable sources of naquadah within their home systems in the galaxy of Ida. Most Asgard energy sources stem from naquadah fusion-reactors which power their formidable motherships and hyper-space drives. This energy is stored within a crystal lattice structure built into each Stargate. Neutrinos are not affected by the electromagnetic forces that act on electrons and thus able to pass through great distances and through matter without noticeable effect. In its refined state, a Stargate's naquadah only reacts with neutrinos – an electrically neutral particle – converting and storing energy as a large superconductor. ![]() Naquadah is a stable mineral, capable of many applications and uses, including the creation of weapons of mass destruction and the generation of seemingly limitless amounts of clean energy. The Ancients made the first practical application of the mineral with the creation of their network of interplanetary Stargates, constructed from refined naquadah ore, similar to quartz. Both the Ancients (who built the network of Stargates) and the Goa'uld (who exploit the network) used naquadah in the creation of their advanced technology. A Fossil Linear Zone of Weakness Beneath the Kasei Valles, Mars? 26th Lunar and Planetary Science Conference, Abstract #1351.Naquadah is the most prized mineral in the galaxy. "Amazonian Geologic History of the Echus Chasma and Kasei Valles System on Mars: New Data and Interpretations". "Noachian–Hesperian Geologic History of the Echus Chasma and Kasei Valles System on Mars: New Data and Interpretations" (PDF). (1978) Geomorphology: A Systematic Analysis of Late Cenozoic Landforms Prentice-Hall: Englewood Cliffs, NJ, p. American Geophysical Union, abstract #P11E-01.) New Insights about Mars from the Creation and Analysis of Mars Global Datasets. ^ Mars Orbital Laser Altimeter (MOLA) gridded dataset from JMars.^ a b c USGS Gazetter of Planetary Nomenclature.Layered bedrock is visible at the top of the escarpment in some medium and high resolution spacecraft images, but the scarp face is largely covered by talus aprons and dust. They probably consist of ancient impact breccias and volcanic materials. Two final episode of flooding from the Echus Chasma region to the south occurred in Kasei Valles during Amazonian times (3.6 Gya). ![]() (See outflow channels.) These floods occurred in Hesperian time between about 3.6 and 3.4 billion years ago (Gya).Īfter initial flooding, the northern Kasei valley was covered by extensive late Hesperian-aged basaltic lava flows from Tharsis. Thus, the proto-Nilokeras Scopulus was probably an east-west oriented fault scarp or fracture zone (or zone of weakness ) that was eroded and further downcut by at least one (and possibly two) episodes of early catastrophic flooding from the northern Tharsis region. Recent geologic mapping of the Kasei Valles region indicates that the west-to-east flow of the Kasei Valles floods followed the existing structural trend of rift valleys in southern Tempe Terra. ![]() Nilokeras Scopulus likely formed from a combination of faulting and erosion from flood waters that formed Kasei Valles. The term carries no implication of geologic origin. ![]() A scarp may be formed by tectonic, erosional, or depositional processes. In geomorphology, an escarpment (usually shortened to scarp) is any steep, abrupt slope or cliff along the margin of a plateau, terrace, or other topographic bench. Scopulus is the Latin term for "crag" or cliff. The International Astronomical Union (IAU) formally adopted the name Nilokeras Scopulus in 1976. (See List of Martian canals.) Scopulus is a descriptor term used in planetary geology for an irregular escarpment or cliff. Antoniadi in 1930 to a telescopic albedo feature and canal centered at lat. Nilokeras, which is Greek for "horn of the Nile," was the name given by astronomer E.
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