Payne County lies in north-central Oklahoma, with Stillwater forming the largest urban center in the west-central part of the county and Cushing anchoring the southeast. Between them are smaller communities, branching creeks, reservoirs, and rolling terrain that changes noticeably from the higher western and northern uplands to the lower river country in the east and southeast. The maps on this page combine county boundaries, roads, settlement locations, water features, and generalized elevation so those relationships can be compared without switching between unrelated sources.
The map files used here are also available as high-resolution JPG downloads in a single ZIP package below. A useful way to explore the county is to start with the general road and boundary map, then compare the settlement view with the terrain-and-water and elevation maps. That sequence shows where Stillwater, Cushing, Yale, Perkins, Glencoe, and Ripley sit, how Stillwater Creek and other tributaries cross the county, and why Lake Carl Blackwell, Cushing Lake, and the lower eastern valleys appear in different terrain settings.
Table of Contents
Stillwater provides the clearest reference point for roads and county orientation
Stillwater is the first place to use when orienting yourself on the general county map. The Oklahoma Historical Society and Payne County government identify Stillwater as the county seat, and the map shows a much larger built-up area there than around the county’s smaller towns. State Highway 51 runs east-west through the city, while State Highway 177 provides a strong north-south route toward Perkins. Those two corridors make Stillwater a practical reference point for locating nearly every other place shown on the county-wide map.
Moving east from Stillwater, the map passes Ingalls before reaching Yale, while Cushing lies farther south in the southeastern part of the county. Glencoe is set in the northern extension of the county, and Perkins and Ripley occupy separate positions along the southern half. Around Cushing, State Highway 33 is the prominent east-west route, with State Highways 18 and 108 also labeled nearby. Places outside the county, including Orlando, Mulhall, Lone Chimney, and Drumright, are shown around the edges and help explain how local roads continue beyond the boundary.
The outline is not a simple rectangle. Long straight sections appear on the west and south, but the northern and eastern sides step in and out, creating distinct projections around Glencoe and the eastern townships. That shape matters when reading place names near the edge of the county because a short straight-line distance can cross into Noble, Pawnee, Creek, Lincoln, or Logan County. The surrounding labels on the map provide enough context to see when a nearby town is actually outside Payne County.
Regional geography adds another layer to the road pattern. The Oklahoma Historical Society describes most of Payne County as rolling plains within the Sandstone Hills, with the western part extending into the Red Bed Plains. Those physiographic terms are easier to understand after looking at the elevation map later on: the west and north contain more short ridges and broken upland, while the eastern drainage corridors are generally lower. The road map therefore serves as a useful base for interpreting the water and terrain views rather than merely identifying highways.
Six highlighted cities reveal a dispersed settlement pattern
The city distribution map highlights six of the county’s larger incorporated places: Stillwater, Cushing, Perkins, Yale, Glencoe, and Ripley. Stillwater ranks first in the map’s city index and Cushing second, but the more useful information is their separation. Stillwater occupies the west-central area, Cushing the southeast, Perkins the south, Yale the east, Glencoe the north, and Ripley the south-central to southeastern side. The pattern is dispersed rather than concentrated along one continuous urban strip.
That distribution is important when a local address, newspaper story, genealogy record, or property description mentions Payne County without giving much additional context. A location near Yale or Cushing can be much closer to the eastern county line than to Stillwater, while Glencoe sits in a northern projection and follows a different set of roads. Perkins is close enough to Stillwater to appear part of the same broader north-south corridor on the map, yet it remains a separate city with its own position near the southern boundary.
The surrounding county names add useful orientation. Noble County appears to the northwest and north, Pawnee County to the northeast, Creek County to the east, and Lincoln and Logan counties to the south and west. These labels make the map more useful for understanding regional direction than a city-only chart would be. Stillwater is not simply “in central Oklahoma”; on this map it is clearly positioned between the western county boundary and the cluster of eastern communities that lead toward the Tulsa side of the state.
The city map should not be used as a driving-distance chart. It is designed to compare relative positions and the distribution of settlements. Actual travel depends on road alignment, river and creek crossings, construction, and the type of road available between two points. For trip planning, use the city map for orientation and confirm the route with current transportation information.
Stillwater Creek and smaller tributaries feed a broad eastern drainage system
The terrain-and-water map makes Payne County’s drainage pattern much clearer than the road map. Stillwater Creek crosses the middle of the county from the Lake Carl Blackwell area toward the east, with Little Stillwater Creek and many unnamed branches joining the system. The Oklahoma Historical Society identifies the Cimarron River as the county’s primary waterway and notes that much of the county drains through tributaries that include Stillwater Creek. Even where the largest river is not the most prominent label on the map, the branching tributaries show how water is collected across the county.
Lake Carl Blackwell is the largest named lake shown on the western side. Closer to Stillwater are Lake Boomer and Cedar Isle Lake, while Yost Reservoir appears north of the central area. Cushing Lake occupies the southeast, and Keystone Lake is labeled at the far eastern edge. The map also names Council Creek, Salt Creek, Euchre Creek, Wildhorse Creek, Long Branch, and Little Stillwater Creek. These features are useful for locating rural places that may be described by a creek or reservoir rather than by the nearest incorporated city.
The water network changes character across the county. In the west and north, many short tributaries cut through rolling upland and create a fine branching pattern. Toward the east and southeast, broader valleys and more strongly meandering channels become obvious. Comparing the water map with the elevation view explains this difference: the lower eastern terrain gives the larger drainage corridors more room to curve, while the western and northern uplands are divided by shorter, narrower valleys.
This map is a geographic reference, not a floodplain, navigation, parcel, or legal-boundary product. A blue line identifies a mapped water feature but does not establish property access, a regulatory flood zone, or the legal edge of a stream. Use current agency information for flood insurance, construction, land ownership, or water-access decisions. For ordinary geographic study, however, the map is useful for recognizing how lakes and tributaries relate to towns and terrain.
Higher western and northern ridges descend toward lower eastern valleys
The elevation map shows one of the strongest county-wide patterns. Browns and oranges are concentrated in much of the west and across parts of the north, where short ridges and closely spaced valleys give the surface a broken appearance. Greens become more common toward the east and southeast, especially along the broad winding drainage corridors. The transition is gradual rather than a single steep escarpment, but it is strong enough to make the eastern side look distinctly lower than the upland areas west of Stillwater.
The legend reports an actual elevation range of about 227 to 357 meters and a county mean near 285 meters. Those figures are appropriate for broad geographic comparison, not for surveying a property or determining construction grades. The surface is generalized to show county-scale relief. Anyone needing exact elevations for engineering, drainage design, building work, or legal documentation should use current USGS 3D Elevation Program data or a qualified survey.
Stillwater occupies an intermediate part of this terrain rather than the county’s highest or lowest ground. Relief becomes more pronounced west toward Lake Carl Blackwell and in the northern interior, while lower valleys extend toward Cushing and the eastern drainage network. The pattern helps explain why road alignments and settlement locations differ across the county. A road crossing the west may encounter frequent small valleys and ridges, whereas eastern routes often follow or cross broader drainage corridors.
The northern uplands deserve attention as well. South of Glencoe and along the upper part of the county, bands of higher terrain are cut by many small stream valleys. Farther east, the topography opens into lower, greener areas near the main drainage system. It is therefore more accurate to think of Payne County as a series of uplands and valleys that generally step downward toward the east than as a simple west-high, east-low slope.
Ingalls, Twin Mounds, and the Cimarron drainage add local detail to the terrain
County-specific landmarks make the terrain easier to interpret. The Oklahoma Historical Society identifies Twin Mounds, limestone-topped hills east of Ingalls, as one of Payne County’s notable landforms. Ingalls appears on the general map between Stillwater and Yale, and the elevation map shows that the central-eastern area is not simply a flat lowland. Instead, short ridges and valleys continue across the county even as the overall surface becomes lower toward the eastern drainage corridors.
The Cimarron River system provides the larger regional framework for many of those creeks. Stillwater Creek and smaller tributaries flow through a landscape of rolling plains before joining broader drainage valleys. Cushing, Yale, and the eastern rural areas sit closer to this lower network than Stillwater’s western side. When the road, water, and elevation maps are read together, the separation between the county’s urban centers makes more geographic sense: each sits within a different combination of roads, tributaries, and relief.
History also reflects those different local settings. Stillwater developed as the county seat and later as a major university community, while Cushing became nationally significant during the early twentieth-century oil boom. The two places are part of the same county but have different geographic surroundings. On the map, Stillwater is a broad west-central urban area tied to State Highways 51 and 177, whereas Cushing is a separate southeastern center near State Highway 33 and a denser network of eastern creeks and lower valleys.
Choosing the right Payne County map for a specific question
For city locations, county boundaries, and major highways, begin with the general map. It is the best choice for finding Stillwater, Cushing, Yale, Perkins, Glencoe, Ripley, and smaller places such as Ingalls and Mehan while also seeing the surrounding county context. If the main question is how the six highlighted cities are distributed, the city map removes much of the extra detail and makes their relative positions easier to compare.
For named lakes and creeks, use the terrain-and-water map. It brings Lake Carl Blackwell, Lake Boomer, Yost Reservoir, Cushing Lake, Stillwater Creek, Little Stillwater Creek, Council Creek, Salt Creek, and other water features into one view. If the question concerns hills, valleys, or the difference between the western uplands and eastern lowlands, add the elevation map. The four maps work best as complementary references rather than as competing versions of the same information.
The downloadable archive contains the original high-resolution JPG versions of all four maps, each at 3638 × 2572 pixels. Those files are easier to inspect at large scale or print than the smaller WebP images used in the article. They are intended for geographic reference and general map use, not as substitutes for legal boundary surveys, flood determinations, engineering-grade elevations, or live navigation.
Frequently Asked Questions
Which map is best for comparing Stillwater and Cushing?
The general county map is the best starting point because it shows both cities with the county outline and major roads. Stillwater occupies the west-central area around State Highways 51 and 177, while Cushing is farther southeast near State Highway 33. The city distribution map is useful as a second view because it also places Perkins, Yale, Glencoe, and Ripley in the same county-wide frame.
Can I find Lake Carl Blackwell and Stillwater Creek on the same map?
Yes. The terrain-and-water map shows Lake Carl Blackwell on the western side and Stillwater Creek extending from that area across the central part of the county. It also labels Lake Boomer, Cedar Isle Lake, Yost Reservoir, Cushing Lake, Little Stillwater Creek, Council Creek, and several other tributaries, making it the most detailed map for water features.
Are the 227–357 meter elevations precise enough for surveying or construction?
No. The elevation map is a generalized county-scale surface designed to compare relative highs and lows. It is useful for recognizing the higher western and northern uplands and the lower eastern drainage corridors, but it should not replace survey-grade measurements. For engineering, construction, or precise site elevation, use current USGS elevation data or a professional survey.
Map File Information
The original Payne County maps used in this article are packaged as high-resolution JPG files for printing, personal reference, and local geographic study. They are reference maps rather than survey or legal products.
- Included Files: general county map, city distribution map, terrain and water map, elevation map
- Printable Size: 3638 × 2572 px each
- File Type: JPG
Related Maps
Sources and references
- Payne County official website for county government information and local reference.
- Oklahoma Historical Society – Payne County for county history, terrain, the Cimarron River, and notable local features.
- U.S. Census Bureau – TIGER/Line Shapefiles for county boundary and geographic reference data.
- USGS – National Hydrography for official hydrography information and water-feature datasets.
- USGS – 3D Elevation Program for official elevation data and documentation.
Green Map creates custom-edited map images using open geographic data sources such as geoBoundaries, Natural Earth, OpenStreetMap, and government open data. These maps are edited visual materials, not raw data files, and are provided for education, documents, presentations, and graphic reference.
