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Between the two zones is the Missouri Gravity Low, or MGL, a mass of low density granite including the Missouri batholith up to 370 miles long and 60 miles wide, identified in gravity surveys. Igneous activity ended around 1.3 billion years ago, with the intrusion of numerous dikes and sills into newly crystallized rhyolite and granite.
Kansas City is a Late Carboniferous geologic group and formation having various significant alternating beds of limestone and shale known for forming high bluffs in Missouri, Kansas, and neighboring states. This formation was named for the bluffs within Kansas City, Missouri. [3] Primary group outcrops are in northwest Missouri.
The entrance originally was through a large sink-hole at the top of Roark Mountain, though now an easier entrance has been made. Marvel Cave has a large hall-like room about 350 ft (110 m) long and about 125 ft (38 m) wide with bluish-grey limestone walls, and a vaulted roof, rising from 100 to 295 ft (90 m).
A rural Ozarks scene. Phelps County, Missouri The Saint Francois Mountains, viewed here from Knob Lick Mountain, are the exposed geologic core of the Ozarks.. The Ozarks, also known as the Ozark Mountains, Ozark Highlands or Ozark Plateau, is a physiographic region in the U.S. states of Missouri, Arkansas, and Oklahoma, as well as a small area in the southeastern corner of Kansas. [1]
Geoprofessions is a term coined by the Geoprofessional Business Association to connote various technical disciplines that involve engineering, earth and environmental services applied to below-ground ("subsurface"), ground-surface, and ground-surface-connected conditions, structures, or formations.
Northwest Missouri State University (NW Missouri) is a public university in Maryville, Missouri, United States. It has an enrollment of 9,152 students. [ 4 ] Founded in 1905 as a teachers college, its campus is based on the design for Forest Park at the 1904 St. Louis World's Fair and is the official Missouri State Arboretum . [ 5 ]
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