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, 2018 Digest of Papers Ninth IEEE Symposium on Mass Storage Systems, 1988. 'Storage Systems: Perspectives', 2003
The author describes the implementation of a library storage module (LSM) of the 4400 Automatic Cartridge System manufactured by StorageTek (STK). Each of the five LSMs contains approximately 6000 cartridges (1/2-in, 18-track) with a robot performing cartridge mounts and dismounts.
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The author describes the implementation of a library storage module (LSM) of the 4400 Automatic Cartridge System manufactured by StorageTek (STK). Each of the five LSMs contains approximately 6000 cartridges (1/2-in, 18-track) with a robot performing cartridge mounts and dismounts.
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Geology of the Cimarron Range, New Mexico
Geological Society of America Bulletin, 1943In north-central New Mexico the rugged Cimarron Range marks the eastern margin of the Southern Rocky Mountains, abruptly rising more than 5000 feet above the adjacent Great Plains. Structurally the range is a northward-plunging anticline with a core of pre-Cambrian crystalline rocks.
J. F. SMITH, L. L. RAY
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Black Rebels: The Cimarrons of Sixteenth-Century Panama
The Americas, 2007The strategic location of the Isthmus of Panama within the commercial network of the Spanish Empire and the need to defend it has greatly influenced historical writing on sixteenth-and seventeenth-century Panama. Most studies have emphasized military and economic history and with few exceptions, have shown little interest in other aspects of Panamanian
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Arizona State Prison Complex, Cimarron Unit
1996Abstract This one-hour disturbance by inmates at Cimarron Unit of the Arizona State Prison Complex at Tucson initially pitted inmates against inmates. It began as a fight over a cigarette lighter and escalated into a giant brawl. When prison officials intervened, inmates turned on them, and force had to be used to end the disturbance.
Bert Useem +2 more
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Accelerated Channel Erosion in the Cimarron Valley in Southwestern Kansas
The Journal of Geology, 1947The Cimarron River formerly had a narrow channel throughout its course from the Kansas-Colorado state line to the Kansas-Oklahoma state line. Accelerated erosion began in 1914 and has increased the average width of the channel to more than 1,000 feet. Overcultivation appears to have been the principal cause of the erosion.
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