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At the high school level, school administrators cannot be involved in the booster club organization except approving activities held at the high school. At the collegiate level, the NCAA strictly regulates the activities of booster clubs and strictly defines what actions would cause a person to be considered an official booster of an athletic ...
The Ohio High School Athletic Association (OHSAA) is the governing body of athletic programs for junior and senior high schools in the state of Ohio.The OHSAA governs eligibility of student athletes, resolves disputes, organizes levels of competition by divisional separation of schools according to attendance population, and conducts state championship competitions in all the OHSAA-sanctioned ...
A foreland basin is a structural basin that develops adjacent and parallel to a mountain belt. Foreland basins form because the immense mass created by crustal thickening associated with the evolution of a mountain belt causes the lithosphere to bend, by a process known as lithospheric flexure .
The Alabama High School Athletic Association (AHSAA), based in Montgomery, is the governing body for interscholastic athletics and activities programs for public schools in Alabama. The AHSAA is a member National Federation of State High School Associations since 1924.
The Idaho High School Activities Association (IHSAA) oversees high school athletics and activities in the state of Idaho. Idaho high schools are classified in six categories, based on enrollment, for league competition and state playoffs and championships. The IHSAA recognizes twenty specific sports and activities. [1]
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The IHSA also has a 35-member Legislative Commission, [5] consisting of 21 high school principals, seven high school athletic directors elected from each of the seven state regions, and seven at-large members. The commission reviews amendment proposals to the IHSA Constitution and By-laws, and determines which are passed on to a vote of the ...
In geology, the name "molasse basin" is sometimes also used in a general sense for a synorogenic (formed contemporaneously with the orogen) foreland basin of the type north of the Alps. The basin is the type locality of molasse , a sedimentary sequence of conglomerates and sandstones , material that was removed from the developing mountain ...