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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.
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 ...
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 ...
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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Newberry lies 37 miles (60 km) east [9] of the major crest of the Cascade Range in the High Lava Plains region, [7] rising 3,500 feet (1,100 m) above its surroundings. [3] From north to south, the volcano runs for a length of 75 miles (121 km), with a width of 27 miles (43 km) [7] and a total volume of about 140 cubic miles (600 km 3). [9]
Boring Lava was erupted by vents in the volcanic field, [6] [74] and it has been exposed at elevated topographic levels in intact volcanic cones and dissected lava plains. There is likely more lava deposited under Quaternary sedimentary mantle throughout the region, [6] though activity was confined to a relatively concentrated area. [75]
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."