Interstate 35 in Kansas direction. After passing through the Kansas suburbs of the Kansas City Metro Area, it then crosses the state line into Missouri and into Downtown Kansas City. The original plan for Interstate 35 was to follow US 50 from Newton, as well as US 81 and US 177 to the Oklahoma state line. But when Kansas Turnpike was created, a part of Interstate 35 was created south of Emporia. The Newton segment was declined, and there was another implication for US 50 that traveled north (which is known today). The segments from Olathe to Shawnee was created by 1962. The relocations
Geology of Kansas Southern granite-rhyolite province dating to 1.35 to 1.48 Ga. Geology of Kansas The Geology of Kansas encompasses the geologic history of the US state of Kansas and the present-day rock and soil that is exposed there. Rock that crops out in Kansas was formed during the Phanerozoic eon, which consists of three geologic eras: the Paleozoic, Mesozoic and Cenozoic. Paleozoic rocks at the surface in Kansas are primarily from the Mississippian, Pennsylvanian and Permian periods. The oldest rocks at the surface in Kansas are Mississippian rocks that consist of limestones, shale, dolomite, chert, sandstones and siltstones. The Mississippian consisted of