Ellis County Oklahoma Map: Shattuck, Wolf Creek, and Canadian River Valleys

Ellis County sits on Oklahoma’s far western side, where small towns are widely spaced and the Canadian River bends along much of the southern boundary. Shattuck, Gage, and Fargo provide a useful west-to-east sequence in the northern half, while Arnett gives the center of the county a separate reference point. This page compares roads, settlements, waterways, and elevation, and the same map set is available as high-resolution JPG files in a downloadable ZIP archive.

The landscape is more varied than a simple flat-plains description suggests. Wolf Creek and its tributaries cut across the north and center, while the Canadian River and several southern creeks occupy lower corridors near the county edge. The elevation map adds another layer by showing broad uplands between those valleys. Reading the maps together makes the spacing of towns and roads easier to understand without turning the page into a technical GIS report.

Shattuck, Gage, Fargo, and Arnett form the main orientation points

Shattuck is the clearest western reference on the general county map. Gage lies east of it and Fargo is farther toward the eastern side of the northern half, while Arnett sits well to the south in the central part of the county. Those four places create a practical frame for locating the large rural spaces between them. Nearby labels outside the boundary, including Woodward and Fort Supply, also help place Ellis County within the broader western Oklahoma road network.

The route shields provide a second layer of orientation. Route 283 is visible in the western part of the county, route numbers 51 and 60 cross the Arnett area, and route 46 runs through the central section. Route 15 appears in the northwest and 412 is shown near the northern edge. The map is intended for geographic reference rather than live navigation, so construction, closures, and current driving directions should always be checked with an up-to-date road service.

The county outline changes character from north to south. Straight administrative segments dominate much of the northern and western edge, but the southern boundary becomes irregular where it follows the meandering Canadian River. A long eastern extension also keeps the county from looking like a simple rectangle. That outline makes much more sense after comparing the road map with the terrain-and-water map, where the river is shown as a physical feature rather than only as a boundary line.

The city map simplifies distance from Shattuck

The city-connections map uses Shattuck as the hub and highlights three other communities. The printed straight-line distances are about 8 miles to Gage, 11 miles to Arnett, and 17 miles to Fargo. These are direct distances measured between points, not driving mileage. Roads may curve around terrain or use different crossings, so the values are best used to compare relative spacing rather than to estimate travel time.

Shattuck and Gage form the closest pair among the highlighted places, while Fargo lies farther east and Arnett is separated to the south. That arrangement immediately shows why Ellis County does not read like a continuous urban corridor. The communities are distinct points within a large rural landscape, and substantial areas of open land and creek valleys lie between them. Pairing this simplified city view with the general map adds the road context without losing the clear sense of distance.

The numbers attached to the city labels should be treated as map-reference information rather than a live demographic table. Anyone who needs current population figures or a historical trend should use a current Census source. For classroom work, a regional introduction, or a presentation about settlement spacing, however, the city map is useful precisely because it reduces the visual detail and keeps the four principal reference points easy to find.

Wolf Creek organizes much of the northern drainage

Wolf Creek is the dominant named waterway across the northern and central part of the terrain-and-water map. It crosses a broad valley and receives numerous smaller tributaries from both sides. Twentyfive Mile Creek descends through the north-central area, Sixteenmile Creek approaches from the northeast, and Sand Creek is prominent farther north and east. Their courses show that the upper half of the county is divided by many valleys rather than forming one uninterrupted level surface.

The minor streams are important even when their names are not printed. Pale tributary lines branch repeatedly off the larger creeks and show how closely spaced the drainage cuts can be. On the elevation map, many of these same corridors appear as lower green fingers reaching into higher terrain. The comparison makes it easier to see why roads and towns occupy particular strips of ground instead of following a perfect grid across the county.

The Oklahoma Historical Society describes Wolf Creek as a major stream in Ellis County and notes that local drainage ultimately connects with both the Canadian and North Canadian river systems. That broader account fits the two very different water settings visible here: Wolf Creek and its northern tributaries within the county, and the Canadian River along the south. This map is not a flood-hazard, legal-channel, or navigation chart, so specialized water-management questions require the appropriate official product.

The Canadian River turns the southern edge into a river boundary

The Canadian River is the defining feature of the southern map edge. It bends sharply around the southwest and then continues eastward along the irregular county boundary. Unlike Wolf Creek, which lies within the county landscape, the Canadian River helps shape the county outline itself. That distinction explains why the southern border looks so different from the straighter administrative lines to the north and west.

Several smaller water features add detail to the southern half. Lake Lloyd Vincent is labeled in the southwest, Packsaddle Lake appears farther south, and Carltron Lake and Richards Lake are shown in the southeastern section. Hackberry Creek forms a pronounced drainage there, while Turkey Creek and South Turkey Creek cut smaller valleys nearby. The southern landscape is therefore a combination of the major river corridor and many tributary valleys rather than a single broad flat plain.

The Oklahoma Historical Society also links Lake Lloyd Vincent with the Ellis County Wildlife Management Area and describes the Packsaddle Wildlife Management Area along the Canadian River. The map does not attempt to draw every management boundary, but the water features provide useful geographic anchors for understanding where those landscapes lie. Visitors who need access rules, hunting regulations, or recreation information should consult the current managing-agency pages before a trip.

Elevation from about 566 to 786 meters separates uplands from valleys

The elevation map labels an actual county range of roughly 566 to 786 meters and a mean near 701 meters. Greens mark relatively lower ground, while yellow, tan, and brown identify higher terrain within the locally scaled map. Large areas of the west and northwest are elevated, while the major creek and river corridors stand out as lower green channels. The contrast is strong enough to show that county-scale relief exceeds 200 meters from the lowest to highest mapped areas.

Wolf Creek produces one of the most visible low corridors in the north and center. Twentyfive Mile Creek and Sixteenmile Creek create additional green branches, and small unnamed tributaries divide the surrounding uplands into many ridges. Along the southern edge, the Canadian River and Hackberry Creek are also clearly lower than adjacent terrain. Looking from the water map to the elevation map is an easy way to match named streams with the valleys they occupy.

The elevation surface is useful for county-scale comparison, not survey work. A 566-to-786-meter range can explain why one part of the county is a low river corridor and another is an upland, but it cannot establish the exact height of a house pad, road grade, field, or property corner. Engineering, drainage design, and parcel-level decisions require higher-resolution source data from programs such as the USGS 3D Elevation Program and, where appropriate, professional field surveying.

Great Plains geography here includes strong local relief

Ellis County lies along Oklahoma’s westernmost tier near the 100th meridian and the Texas line. The Oklahoma Historical Society places most of the county within the Great Plains physiographic region. That broad regional label is useful, but the maps show why it should not be interpreted as perfectly flat ground. Uplands, creek-cut ridges, and the deep Canadian River corridor create substantial local variation within the larger plains setting.

The higher western areas are especially obvious on the elevation map, where warm colors cover long stretches between tributary valleys. Those uplands are repeatedly cut by narrow lower corridors, so elevation can change over short distances near a creek. This matters when interpreting the road map: a route that looks straightforward in plan view may cross a landscape of ridges and drainage lines rather than a uniform open surface.

The Canadian River zone provides the strongest contrast. Low green terrain follows the sweeping southern bend, while higher colors rise on either side of the river corridor. Instead of summarizing the county as simply higher in one direction and lower in another, it is more accurate to think of several low drainage systems separated by broad uplands. Wolf Creek and the Canadian River are the two easiest examples to use when explaining that pattern.

Road and water maps become more useful when compared

A trip between Shattuck, Gage, and Fargo can be understood quickly on the city map, but the water map explains the terrain surrounding those direct-distance lines. Northern settlements sit among the Wolf Creek tributary network, and local routes must cross or skirt many small drainage corridors. The direct map distance is therefore a clean geographic comparison rather than a promise that the road between two places follows an equally straight line.

Arnett offers another good comparison. On the general map it appears near several numbered routes and works as a central orientation point. On the water and elevation maps, the surrounding area contains repeated small tributaries and alternating higher and lower ground. Moving between the views turns a simple road junction into a more complete picture of the landscape in which that junction sits.

The Canadian River boundary is even more revealing. One map shows the irregular county outline, the water map identifies the river and its neighboring tributaries, and the elevation map marks the same corridor as low ground. The three views explain administrative geography, drainage, and relief without requiring specialized software. This is one of the clearest examples of why multiple county maps can be more informative than a single all-purpose image.

Choose the Ellis County map that fits the question

Use the general county map when towns, roads, nearby places, and the full county outline need to be visible at once. It is the best starting view for locating Shattuck, Gage, Fargo, and Arnett and for seeing how the numbered routes cross the county. The city-connections map is better when the main question is settlement spacing, because it emphasizes Shattuck and the straight-line distances to the other highlighted communities.

Choose the terrain-and-water map for named creeks, the Canadian River, small lakes, and the relationship between drainage and valleys. Wolf Creek, Twentyfive Mile Creek, Sixteenmile Creek, Hackberry Creek, and the southern river corridor are much easier to compare there than on the road-focused map. It should be used as a regional water reference rather than a substitute for flood, property, or legal-boundary products.

The elevation map is the clearest choice for explaining relief. Its roughly 566-to-786-meter range highlights higher western and central uplands and lower stream corridors. Pairing it with the water map works well in a classroom or presentation because green valleys can be matched with the named waterways. The downloadable JPG files are suitable for printing and general reference, but live navigation, legal boundaries, flood hazards, and engineering decisions should use the relevant current official sources.

Frequently Asked Questions

Related Maps

• Beaver County Oklahoma Map
• Blaine County Oklahoma Map
• Bryan County Oklahoma Map

Sources and References

• Oklahoma Historical Society – Ellis County
• U.S. Census Bureau – TIGER/Line Shapefiles
• USGS – National Hydrography
• USGS – 3D Elevation Program