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Library associations connect libraries and library workers at the local, national, and international level. Library associations often provide resources to their individual and institutional members that enable cooperation, exchange of information, education, research, and development.
The largest of the Northern Basin and Range subregions, the High Lava Plains covers 10,262 square miles (26,578 km 2) in Oregon and 5,740 square miles (14,867 km 2) in Nevada, featuring a variety of land uses, including rangeland, wildlife habitat, irrigated pastureland and cropland, historic gold and silver mines, and active opal mines and ...
Founded at a meeting in Estes Park, Colorado, by librarians from Colorado, Kansas, Nebraska, the Dakotas and Wyoming, the Mountain Plains Library Association was designed to facilitate regional American Library Association meetings. Within three days a temporary constitution had been drafted, Ralph T. Esterquist was elected president and Ruth V ...
The library board led by chairman Steve Sullivan expects to be presenting a plan on reviewing materials to ensure adherence to the community decadency ordinance by the Jan. 8 County Commission ...
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ULA has been a charter member of the American Library Association since 1913 and was a founding member of the Mountain Plains Library Association. [4] ULA advocated for the establishment of the Utah State Library in the 1950s; the library was established with state support, the last state library agency created in the United States up until ...
Extensive areas of nearly flat-lying lava flows throughout the Northern Cordilleran Volcanic Province can cover areas of at least 100 km 2 (39 sq mi) and are generally composed of highly-fluid basaltic lava. However, lava plains that pre-date the last glacial period have been eroded and overridden by glacial ice, affording a less distinctive ...
In 1992, Coffin and Eldholm initially defined the term "large igneous province" as representing a variety of mafic igneous provinces with areal extent greater than 100,000 km 2 that represented "massive crustal emplacements of predominantly mafic (magnesium- and iron-rich) extrusive and intrusive rock, and originated via processes other than 'normal' seafloor spreading."