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Geology of the Trans-Missouri River Tunnel project, Kansas City, Missouri

Conference · · Geological Society of America, Abstracts with Programs; (United States)
OSTI ID:5075094
 [1]
  1. Univ. of Missouri, Kansas City, MO (United States). Dept. of Geosciences
The geology of the Missouri River Valley at Kansas City is interpreted from the borehole and construction site data along the route of the Trans-Missouri River Tunnel, a 4.4 km long water tunnel constructed at a depth of 90--97.5 m below the floodplain of the Missouri River. The data from the site investigation is used to construct a detailed stratigraphic cross-section of the subsurface units to a depth of 120 m and extending in a north-south direction the length of the tunnel. The rock section is divided into 2 broad categories, (a) alluvium and (b) bedrock. The alluvium (Pleistocene-Holocene) fills the Missouri River Valley to a depth of 38 m along the tunnel route. An exception is a deep narrow channel near the center of the valley, the alluvium is 55 m thick and the lower several meters of the channel is filled with glacial till( ). The alluvium rests unconformably on Pennsylvanian bedrock consisting of thin strata arranged in cyclical sequences or cyclothems and belonging to the following groups in ascending order: Upper Cherokee, Marmaton and Lower Pleasanton. The test drill core data made it possible to conduct a detailed analysis of the subsurface stratigraphy. Of major importance is the stratigraphic position of a thick channel-fill deposit in the Labette Formation, Marmaton Group, a producing horizon in several small oil and gas fields in western Missouri and eastern Kansas. The 327.6 cm dia. bore for the essentially horizontal tunnel is constructed in predominately silty and sandy gray shale located stratigraphically near the Cherokee-Marmaton contact and in younger channel-fill deposits.
OSTI ID:
5075094
Report Number(s):
CONF-9303210--
Conference Information:
Journal Name: Geological Society of America, Abstracts with Programs; (United States) Journal Volume: 25:3
Country of Publication:
United States
Language:
English

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