Woods County lies in northwestern Oklahoma, where Alva anchors the northeastern part of the county and a broad transition in terrain runs from higher country in the west and northwest toward lower stream valleys in the east. The county map brings together major roads, towns, neighboring counties, and drainage features, while the water and elevation maps make the landscape easier to understand. The Salt Fork of the Arkansas River crosses the eastern side, the Cimarron River follows the southern part of the county, and numerous smaller creeks cut through the uplands between them.
The WebP maps on this page are designed for quick viewing, and the same four subjects are available as high-resolution JPG files in a downloadable ZIP archive. The JPG versions are better for printing or close inspection, while the page images make it easy to compare Alva, Waynoka, Freedom, Dacoma, and Capron with the road network, streams, and relief. These are general reference maps rather than legal boundary, parcel, flood-hazard, navigation, survey, or engineering products.
Table of Contents
Alva and U.S. 64 provide the clearest road reference in the northeast
Woods County sits against the Kansas line in northwestern Oklahoma. The Oklahoma Historical Society describes Harper and Woodward counties on the west, Major County on the south, Alfalfa County on the east, and the Kansas counties of Barber and Comanche along the north. That setting is easy to recognize on the county map because the boundary is not a simple rectangle. The western and southern edges bend noticeably, and the lower part of the outline follows the same general area where the Cimarron River becomes an important geographic reference.
Alva is the most useful place to start. It sits in the northeastern part of Woods County near U.S. 64, which runs east and west across this portion of the map. Other north-south and local routes meet the area around the county seat, so Alva works as a natural reference for locating the smaller communities. Waynoka lies well to the southwest, Freedom is near the western side, Dacoma is southeast of Alva, and Capron is to the northeast. Their separation makes the county feel more like a network of small rural centers than a single continuous urban area.
The western road pattern helps explain the county’s long shape. SH-34 and SH-50 appear in the west, while SH-14 gives Waynoka a clear north-south reference in the south-central part of the county. U.S. 281 is also shown near Waynoka, and additional state routes reach the eastern and southeastern edges. Instead of using these lines as turn-by-turn directions, it is more useful to treat them as a framework for understanding where the main communities sit relative to one another and to the county boundary.
The Oklahoma Department of Transportation publishes a much more detailed Woods County road map with federal, state, collector, and local roads. The map on this page deliberately keeps the view simpler. It is most useful when the question is whether Waynoka is southwest of Alva, how far Freedom sits toward the western bend of the county, or which side of the county Dacoma and Capron occupy. For exact routing, road conditions, or maintenance responsibility, the current ODOT material should be checked directly.
The Kansas border also matters when reading the landscape. Alva and Capron are close to the northern side of the county, while Freedom sits farther west in terrain influenced by the Gypsum Hills. The Oklahoma Historical Society notes that the Gypsum Hills of Barber County, Kansas, extend southward into western Woods County. That helps explain why the western half looks more dissected than the lower eastern valleys. The subtle shaded relief on the county map hints at this difference, but the elevation map later on makes it much easier to see.
City spacing from Alva shows how dispersed the county is
The city-connections map uses Alva as the hub and highlights Waynoka, Freedom, Dacoma, and Capron. The legend shows Waynoka about 19 miles from Alva, Freedom about 24 miles away, and Dacoma and Capron each about 10 miles away. These are direct, straight-line distances rather than driving distances. Actual trips are longer when roads curve, cross drainage features, or require a different route than the straight line drawn between two places.
Waynoka is the most prominent southern counterpart to Alva on this map. It lies southwest of the county seat near SH-14 and U.S. 281, with Avard shown between the two broader areas. A rail line also crosses the county on a diagonal, adding another layer to the transportation pattern. When the city map is compared with the water and elevation maps, Waynoka also appears closer to the Cimarron River side of the county and to lower valleys than the high country around the western and northwestern edge.
Freedom is the farthest of the highlighted communities from Alva in the city legend. Its position near the western bend of the county places it next to more rugged-looking terrain and a dense set of small stream valleys. The city map alone emphasizes distance and direction, but the relief map shows why this part of Woods County has a different visual character from the east. Freedom sits closer to the dissected uplands, where ridges and drainage lines repeat across the landscape.
Dacoma and Capron are both shown about 10 straight-line miles from Alva, yet they occupy different directions. Dacoma is southeast of the hub, while Capron is northeast. That difference matters because the surrounding roads, waterways, and neighboring counties are not the same. Capron is closer to the Kansas side of the county, whereas Dacoma points toward the eastern and southeastern drainage network and the Major County side of the map.
The numerical values printed with the city labels should be treated as reference information used in this map rather than as a substitute for the latest official population estimates. Anyone needing current population or incorporation data should consult the U.S. Census Bureau or local sources. The stronger purpose of this map is geographic: it shows how widely the principal communities are spread and why a single road corridor does not explain the whole county.
The Salt Fork and Cimarron River organize two major drainage areas
Water in Woods County does not drain toward a single river. The Oklahoma Historical Society describes the county as being drained by the Cimarron River, the Salt Fork of the Arkansas River, and their tributaries. The water-and-terrain map makes that division visible. The Salt Fork bends across the eastern and northeastern part of the county, while the Cimarron River follows the southern side and becomes a strong geographic reference near the lower boundary.
Several named tributaries feed the Salt Fork side of the system. Greenleaf Creek and Driftwood Creek appear in the northeast, Turkey Creek crosses the eastern interior, and Yellowstone Creek is visible farther north. Their channels do not run as simple straight lines. They meander through shallow valleys that are easier to see when the blue stream network is read together with the gray shaded relief beneath it.
The central and western uplands are cut by many smaller channels, including Anderson Creek and Sand Creek. These streams begin in higher ground and follow lower corridors between ridges. The density of drainage lines is especially noticeable west of the county center, where the terrain becomes more broken. This is one reason the water map adds information that is easy to miss on the road map: it shows the valleys that shape the land even where no major town or highway is present.
Farther south, the Cimarron River runs near the county boundary and provides an important landmark below Waynoka. Eagle Chief Creek crosses the southeastern portion of the map, and Avard Lake and McGill Lake are labeled nearby. Those features make the southern half more complex than a simple open plain. Small tributaries feed larger channels, local lakes occupy low points, and the county boundary bends through the same broad drainage landscape.
This water map is intended to show general hydrographic relationships, not flood zones or navigable channels. It does not indicate whether a small stream is perennial, whether private access is allowed, or what current water conditions may be. Flood-risk decisions require FEMA and local emergency-management sources, while detailed hydrography is available from the USGS National Hydrography program. Here, the value is in seeing how the Salt Fork, Cimarron River, and their tributaries divide and connect the county.
Elevation falls from the northwest uplands toward lower eastern valleys
The elevation legend shows an actual range of roughly 379 to 654 meters, with a mean near 480 meters. Browns and tans mark the higher parts of Woods County, while greens mark lower terrain. The strongest pattern is a broad area of high ground in the northwest and west, followed by generally lower elevations toward the east and southeast. The relief is locally scaled for this county, so the colors are best used to compare one part of Woods County with another rather than with a map that uses a different scale.
The northwest contains the darkest high-elevation colors and some of the most deeply cut relief. This is consistent with the extension of the Gypsum Hills into western Woods County described by the Oklahoma Historical Society. The high ground is not a smooth plateau. Numerous tributaries have carved narrow valleys into it, producing a repeated ridge-and-draw pattern that is especially clear when the elevation map is compared with the water map.
Alva’s northeastern surroundings are lower than the western uplands, and the terrain drops further along the Salt Fork and connected stream valleys. The southeastern corner also contains broad green areas, while the middle of the county acts as a transition zone between the higher west and lower east. This explains why roads that look simple on the boundary map still cross a landscape of frequent small rises and valleys.
The Waynoka and Cimarron River side of the county also contains local relief, even though it does not reach the highest elevations of the northwest. Low river corridors alternate with modest uplands north of the river, and isolated higher patches appear in the south-central interior. Woods County therefore has a clear west-to-east elevation trend without being uniformly sloped. The finer pattern is a patchwork of ridges, tributary valleys, and broader river lowlands.
Which map is most useful depends on the question. Use the county map for Alva, Waynoka, highways, boundaries, and neighboring counties; use the city-connections view when the spacing of the main communities matters most. The water map is better for the Salt Fork, Cimarron River, creeks, and lakes, while the elevation map makes the west-to-east relief change easiest to see. Viewing the water and elevation layers together is especially helpful because many of the blue channels follow the lower green valleys between higher ridges.
The elevation surface is a county-scale visualization, not survey-grade measurement. It should not be used to determine the exact elevation of a parcel, building pad, road grade, or drainage design. Those tasks require original elevation data, professional surveying, and applicable engineering standards. For general geographic orientation, classroom use, presentations, trip planning, or explaining why streams follow certain valleys, however, the four maps provide a useful set of complementary views.
Frequently Asked Questions
Which map is best for comparing Alva and Waynoka?
The county map and the city-connections map work well together. The county map shows Alva in the northeast and Waynoka to the southwest with U.S. 64, SH-14, U.S. 281, and other routes for context. The city-connections map simplifies the view and labels Waynoka at about 19 miles from Alva. That figure is a straight-line distance, not a road distance, so an actual driving route will usually be longer.
Where are the Salt Fork and Cimarron River in Woods County?
The Salt Fork of the Arkansas River winds through the eastern and northeastern side of the county, receiving several tributaries including Turkey Creek and other smaller channels. The Cimarron River follows the southern part of the county near the boundary below Waynoka. The water map is the clearest choice for comparing these two systems because it also labels tributaries and local lakes.
Why is the northwest brown while much of the east is green on the elevation map?
The colors represent relative elevation within Woods County. Browns and tans mark higher terrain, which is concentrated in the west and northwest, while greens mark lower valleys toward the east and southeast. The legend spans roughly 379 to 654 meters. These colors are useful for county-scale comparison, but they are not a substitute for survey measurements or engineering-grade elevation data.
Map File Information
The download package contains high-resolution JPG versions of the Woods County boundary and roads map, city-connections map, water-and-terrain map, and elevation map.
- File Type: JPG
Related Maps
Sources and references
County context and map interpretation were checked against the Oklahoma Historical Society Woods County entry, the Oklahoma Department of Transportation Woods County map, USGS National Hydrography, the USGS 3D Elevation Program, and U.S. Census Bureau TIGER/Line data.
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.
