K-5 (Kansas highway) Road, it then follows Wolcott Drive towards Lansing. Inside the Lansing area, it turns onto 8th Street, then onto Muncie Drive in Leavenworth. K-5 then ends at 4th Street (US-73/K-7) in Leavenworth. K-5 mostly parallels the Missouri River for its entire run. The road's direction signs changed from west–east to north–south around 2010, although portions of it in Kansas City are still signed west–east. In 2015, The Kansas state legislature passed Statute 68-1038, which designation the portion of K-5 between US-73/K-7 to I-435, then from I-435 to US-69, and southward on US-69 to the Oklahoma border, as the Frontier Military
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