RAILROAD LOG #35b -- Albuquerque to Kansas City
Newton, Kansas to Topeka, Kansas
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701       NEWTON station, 414 N. Main Street.  Elevation approximately 1448.  This city was named after Newton, Massachusetts, by railroad investors from that area.  “Newton” is probably an Old English condensation of “New Town,” which was used often in the New England States to name newer communities.

            Like Halstead (see MP 691 above).  Newton also flourished on the old Turkey Red Wheat strain, which was brought to Kansas by Russian Mennonites.  Newton is now one of the largest Mennonite settlements in North America.  At Bethel College, in North Newton, an annual Mennonite festival is held.  The original Turkey Red Wheat is no longer raised, as better blends have since been patented.  Newton is the home of the Kauffman Museum, which depicts the early Mennonite settlements in this part of Kansas.

            Surficial geologic deposits around Newton are still primarily sand dune and alluvial deposits.

708      Pass through Walton.  The town was named after a Santa Fe stockholder and local businessman.

710      According to AAPG (1986), we are now leaving the area underlain by Quaternary-aged deposits and entering an area underlain by Pennsylvanian and Permian-aged sedimentary formations, and will be for the remainder of this log.  In this area, we are entering the outcrop area of the Lower Permian Sumner Group, composed primarily of limestones and shales.  Between here and Kansas City, we will be traveling downsection into areas of consecutively older sedimentary formations.

715       Enter MARION County.  This county was named by Samuel N. Wood, a State legislator from Ohio, after Lt. Colonel Francis Marion, the “Swamp Fox,” of Revolutionary War fame.

718       Peabody.  This area was settled by Mennonites, and was originally named Conesburg, after J.E. Cone of Wisconsin, a settler who helped locate the town site.  The name was later changed to Peabody, to honor F.H. Peabody of Boston, a banker and philanthropist who was also on the Santa Fe Railroad’s Board of Directors.

725      Pass through a small oil field, which produces from Silurian-aged sedimentary rocks.

729-730  Florence.  Florence was named after Florence Crawford, the daughter of Governor Samuel J. Crawford.  Florence went on to marry Arthur Capper, who later became another Kansas Governor.  Florence is the home of the Harvey House Museum, which is a restoration of an original Santa Fe Railroad “Harvey House” restaurant, which was moved from its original location due to flooding.  The museum contains historical exhibits, plus the original Harvey House dishes and furnishings.

731       The Cottonwood River is adjacent to the railroad on the right (eastbound).  The flood plain of the river is composed of Quaternary-aged alluvial deposits, but the hills on either side are composed of Lower Permian limestones and shales.

734.5    Enter CHASE County.  The county was named after Salmon Portland Chase of Ohio, who later became Chief Justice of the Supreme Court.  Chase was known as the “attorney general for fugitive slaves,” and was a champion of the anti-slavery movement.  Chase also helped found the Free-Soil Party in 1848.  He was elected to the U.S. Senate in 1848 as a Democrat, but he separated from the party in 1852 when it committed itself to slavery.  He was elected Governor of Ohio in 1855 as a Free-Soiler and in 1857 as a member of the newly formed Republican Party, which he helped to found. He was also President Abraham Lincoln’s Secretary of the Treasury.

735      South of the railroad (right if eastbound), across the river, is Cedar Point.  Lower Permian Sumner and Chase Group formations are exposed in the area.  North of the railroad is an exposure of the Wreford Limestone, the lowermost member of the Chase Group.

737      On the left (eastbound) is another exposure of Lower Permian limestones and shales.

739-740  The rock formations exposed on either side of the railroad consist of alternating cliffs and flatter areas.  The cliffs are composed of Lower Permian limestone beds, while the more gentle slopes are composed primarily of shales from the Lower Permian Chase Group.

741      Clements.  This town was formerly a prominent cattle shipping point.  The town was originally called Hunts Station, then Silver Creek, named by William C. Shaft of Michigan.  In 1882, the town was promoted by Joseph L. Crawford, and called Crawfordsville. In 1883, the town was finally renamed Clements in honor of H.G. Clements, an auditor for the Santa Fe Railroad.

748      Elmdale.  The town was named after the abundance of elm trees along the Cottonwood River.  It was originally named “Middle Creek.”  The stream known as Middle Creek is crossed on the east side of town.  It is a tributary of the Cottonwood River.

            In this area, there is a geologic structure known as a structural dome.  This is a subsurface feature, and not visible on the ground.  Such domes consist of sedimentary rock formations “updomed” into a dome shape.  Such features are often, but not always, good reservoirs for oil and gas.  Oil and gas has been explored for in this area, but nothing has been found in the immediate vicinity.

750.5    Neva, most likely named after the Neva River in Russia.

755       Strong City.  This town was originally named North Cottonwood Falls, after the city of Cottonwood falls to the south, named after the 2-ft falls on the Cottonwood River.  The name was then changed to Strong, to honor William Barstow Strong, the President of the Santa Fe Railway.  In 1951, the town was renamed Strong City.

            There are good exposures of the Lower Permian Sumner and Chase Groups on either side of the railroad.  We are now in the Flint Hills Region of Kansas, and Strong City is known as the “Heart of the Flint Hills.”  A few miles south of Strong City is Cottonwood Falls, which was founded in the 1850’s as an agricultural and livestock center.  Cottonwood Falls is the county seat of Chase County, and the French Renaissance-style courthouse, built in 1873, was designed by the same person who designed the State Capitol building in Topeka.

757       Quarries to the north of the railroad (left if eastbound) are cut into limestones of Lower Permian and Upper Pennsylvanian age.

763       Saffordville.  This town was named after Jacob Safford, who was from Vermont, and served as a Supreme Court justice in Kansas.  To the north can be seen shale ridges with limestone caps, from the Lower Permian Council Groves and Admire Groups.

765       Enter LYON County.  The county was named after General Nathaniel Lyon, of the Kansas army, who was killed in the Civil War.  The county seat of Lyon County is Emporia.

766       Just north of the railroad (left if eastbound) is the town of Plymouth, most likely named after Plymouth, Massachusetts, by settlers from New England.

769      The gentle slopes to the north (left if eastbound) are composed of shales from the Lower Permian Admire Group.  The flood plain along the Cottonwood River is still underlain by river alluvium of Quaternary age.

771       Merrick siding.  Pass beneath Interstate Highway 35.  Merrick was named after an Assistant Freight Manager of the Santa Fe Railroad.

773-775 Pass through Emporia.  Emporia was formerly a passenger stop on the route of the Southwest Chief, but the train no longer stops here.  The city is the Lyon County seat, and was founded in 1857 by the Emporia Town Company.  Emporia is best known as the home of journalist William Allen White, the “Sage of Emporia,” who published the Emporia Gazette from 1895 to 1944.  In 1922, White’s essay entitles “To An Anxious Friend” won a Pulitzer Prize.  White also wrote biographies of Presidents Woodrow Wilson and Calvin Coolidge.  Emporia State University is the home of the William Allen White Library.

            Emporia is also the home of the Lyon County Historical Museum, which documents the Pioneer settlement of Kansas.

778.5   Cross the Neosho River.  The Neosho rises to the north of here, and is 460 miles long.  It flows into the Arkansas River in Oklahoma.  The name Neosho means either “clear water” or “muddy water,” or possibly “river with potholes.”

            The bedrock exposed in the banks of the river are Upper Pennsylvanian strata, primarily the Willard Shale in this area.  We are continuing to travel down-section through the relatively flat-bedded Paleozoic sedimentary formations.

789.5    Reading. This town was named after the Reading Iron Works of Pennsylvania, the head of which was John McMann.  McMann made the largest individual purchase of land ever in Kansas in the 1860’s.

790       Enter OSAGE County.  The county was named after the Osage River and Indian tribe.  The Osage people became the wealthiest Native American tribe in the country after oil was discovered on their Midwestern tribal lands.

791.5    Cross the Marais de Cygne River, which flows into Melvern Lake a short distance southeast of here.  Marais de Cygnes is French for “marsh of the swans,” and the river was named after the multitude of swans which inhabited the area. We are now in the Melvena Wildlife Area.

796      Barclay.  The town is surrounded by Upper Pennsylvanian Wabaunsee Group sedimentary rocks.

798      Rocks exposed in this area are the Scranton Shale, Howard Limestone, and Severy Shale, which occur at the bottom of the Upper Pennsylvanian Wabaunsee Group.

801       Osage City.  Like the county, this city was also named after the Indian tribe.  The city is an agricultural and coal mining center.

804       Peterton.  We are still traversing the outcrop area of the Scranton, Howard, and Severy Formation members of the Upper Pennsylvanian Wabaunsee Group.

807      Cross Dragoon Creek.  There was formerly a town here named Dragoon, named after a soldier.

809      Burlingame.  The city was named after Massachusetts Senator Anson Burlingame, who negotiated the 1868 Burlingame Treaty, which made China a serious and secure trade partner with the United States.  In 1859, Burlingame came to the Topeka area as an Abolitionist. Burlingame, however, was founded by New Yorker Philip C. Schuyler.

            In 1863, the women of Burlingame erected a stone fort which defended them from Quantril’s raiders while most of the men from town were fighting on the Union side of the Civil War.  William C. Quantrill was a Confederate Captain, who, along with notorious outlaw Frank James, raided many towns in Kansas which were sympathetic to the Union cause.

            The type locality for the Burlingame Limestone member of the Wabaunsee Group is located just west of the railroad here.

811      The railroad route here is underlain by Willard Shale; however, the bluffs on either side are composed of various limestone and shale formations from the Wabaunsee Group.

             Note the presence of several coal mine dumps along the railroad.  The coal is mined from several Upper Pennsylvanian formations.

815      Scranton.  This small coal-mining town was named after Scranton, Pennsylvania, which is also a coal mining town.  The coal in Kansas is bituminous coal derived from relatively thin Pennsylvanian coal beds, which were deposited as part of numerous cyclothems (see MP 889 below).

818-819  Pass through Carbondale.  The town was originally named Fremont, after John Charles Fremont, the well-known “Pathfinder of the West.”  It was later named Carbondale, to reflect its coal industry.  The coal in the area, and the town, were promoted by T.J. Peters of the Santa Fe Railroad, and Carbondale was the first town to supply profitable freight (coal) to the railroad.

822.5    Enter SHAWNEE County, named after the Shawnee Indians.

823.5    Cross Wakarusa River.  In the banks of the river is the Topeka Limestone, which is the uppermost (youngest) member of the Upper Pennsylvanian Shawnee Group.  The Shawnee Group underlies the Wabaunsee group and the Scranton, Howard, and Severy Formations which we have been following for several miles now.

824       Wakarusa.  The town was founded in 1858 by two men named Mills and Smith, and was at first named Kingston in honor of Zenas King, one of the parties interested.  It is a popular summer camping place for Topeka residents, and a large camp is maintained throughout the season by the YWCA.  The town is a receiving and shipping point for a large and prosperous farming district.

828       Forbes Field Air Force Base, named after Major Daniel H. Forbes, Jr., is visible on the right (eastbound).  Major Forbes was killed during a test flight. Forbes Field is the home of the Combat Air Museum.  The museum features exhibits of 20th century military and other aircraft from the Spanish American War through the Space Shuttle program, including an EC-121 Super Constellation, F-11F Tiger, J-1 “Jenny” biplanes, and other aircraft.

829       Pauline.  This community is located on the former farm of W.A. Paul, and was then given a feminine name.

831       Pass beneath Interstate 470.  This location is the approximate southern limit of the great continental ice sheets of the Pleistocene Ice Age.  The earliest major ice advance during the Pleistocene Epoch is known as the Kansan glaciation, so named after the state you are currently in, since eastern Kansas is one of the very few places in which Kansan-aged glacial deposits are visible and are not covered by later glaciations.

            In the Topeka area, being at the southern edge of the glacial deposits, few glacial deposits are visible; therefore we will still be seeing Upper Pennsylvanian limestones and shales, and are now traveling downsection again, into the outcrop areas of older formations.

833      Passing through Highland Park, a suburban Topeka community.  Outcrops visible from the train are limestones and shales of the Upper Pennsylvanian Shawnee Group, consisting of Topeka Limestone and Calhoun Shale.

835.5    TOPEKA station, 500 S.E. Holliday Place.  Elevation approximately 886.  The origin of the name Topeka is uncertain; however, the most common theory is that it is a corrupted form of the French pomme de terre, which is a potato.  It is also thought that the name may have come from the phrase “To-poo-ka,” which means “a good place to dig potatoes.”

            Topeka is the state capital of Kansas.  The community was laid out in 1854 near the point where the Santa Fe Trail and Oregon Trail separated, and the city developed as a division center for the Atchison, Topeka, and Santa Fe Railroad.  In 1857, the city was incorporated, and the first mayor was Cyrus K. Holliday.  For several years it was the hub of conflict between the proslavery and antislavery factions in the Kansas Territory.  Topeka incorporated in 1857, became the temporary territorial capital in 1859, and was selected as the permanent state capital in 1861 when Kansas entered the Union.  Topeka is a commercial and manufacturing center situated in a fertile wheat- and cattle-raising area.  Major manufactures include processed food, printed materials, and rubber and metal products. Government operations, tourism, and the insurance industry are also important to the city’s economy.

            Topeka was the setting for the Landmark 1954 case Brown vs. Topeka Board of Education, which paved the way for school desegregation in the United States.

                Topeka is the home of the Menninger Foundation, the country’s leading institute for neuropsychiatry and psychiatric nursing.  Gage Park, renowned for its conservatory and miniature train, is located in Topeka, as is the Kansas Center for Historic Research and the Kansas Museum of History.