Shinall Mountain
Rising above the western edge of Little Rock, Shinall Mountain is the highest natural point in Pulaski County, Arkansas and one of the easternmost prominent summits of the Ouachita Mountains. Modern LiDAR measurements place its summit at approximately 1,069 feet (326 meters) above sea level.
Shinall Mountain is unusual among Arkansas peaks because wilderness is not what defines its summit. Instead, the mountaintop is crowned by a striking collection of radio, television, cellular, emergency-communications, and other transmission towers that can be seen from miles across the Little Rock metropolitan area.
The mountain also has an important geological story. Its slopes expose Pennsylvanian-age rocks of the Jackfork Formation, including shale, siltstone, and sandstone that were folded during the tectonic collision responsible for creating the Ouachitas. The mountain lies near the axis of the geologically important Shinall Mountain syncline.
And despite standing only a few miles south of the much more famous Pinnacle Mountain, Shinall is actually the higher of the two.
⚡ Fast Facts
| Feature | Details |
|---|---|
| Country | United States |
| State | Arkansas |
| County | Pulaski County |
| Mountain Range | Ouachita Mountains |
| Region | Eastern / Central Ouachita foothills |
| Elevation | Approximately 1,069 ft / 326 m |
| Traditional Elevation | 1,056–1,066 ft, depending on source |
| Prominence | Approximately 526 ft / 160 m |
| Isolation | Approximately 10.0 mi / 16.1 km |
| Nearest Higher Neighbor (NHN) | Moss Mountain |
| Coordinates | Approximately 34.7987° N, 92.4970° W |
| USGS Quadrangle | Pinnacle Mountain |
| County High Point | Highest natural point in Pulaski County |
| Geology | Primarily Jackfork Formation |
| Geological Structure | Shinall Mountain syncline |
| SOTA Reference | W5A/OA-015 |
| Major Modern Use | Television, radio, cellular and emergency communications |
| Public Summit Trail | None |
| Fun Fact | Shinall Mountain is higher than nearby Pinnacle Mountain even though Pinnacle looks much more dramatic |
🗺️ Where Is Shinall Mountain?
Shinall Mountain rises on the western edge of the Little Rock metropolitan area in Pulaski County.
Its summit coordinates are approximately 34.7987° N, 92.4970° W.
The mountain lies beside the Chenal Valley area of western Little Rock and approximately three miles south-southwest of Pinnacle Mountain.
Although Little Rock is generally associated with the Arkansas River and relatively low terrain, its western side reaches the rugged eastern foothills of the Ouachita Mountains.
Shinall Mountain is one of the most conspicuous of those foothills.
The summit can be recognized from many surrounding viewpoints by the extraordinary cluster of communication towers rising from its crest.
⛰️ How High Is Shinall Mountain?
You may encounter several different elevations for Shinall Mountain.
Older references commonly list the summit at 1,056 feet.
USGS-derived mapping sites sometimes place it around 1,066 feet, while ListsOfJohn uses 1,065 feet.
Peakbagger’s modern LiDAR measurement gives a more precise elevation of:
1,069.2 feet / 325.9 meters
For Mountain Field Guide, approximately 1,069 feet (326 meters) is therefore the best current figure.
The variation does not mean the mountain has changed height. Instead, it reflects improvements in elevation measurement.
Older topographic maps frequently estimated summit elevations from contour lines, spot elevations, or older surveys. Modern LiDAR can model the ground surface with much greater precision, even on forested mountains.
🏆 Highest Point in Pulaski County
Shinall Mountain is the highest natural point in Pulaski County.
That distinction can surprise visitors because nearby Pinnacle Mountain looks dramatically taller.
Pinnacle Mountain has a steep, sharply defined rocky profile and rises abruptly from the surrounding landscape. Shinall Mountain is broader and more rounded, making its actual height less obvious.
Modern measurements place Pinnacle Mountain at approximately 1,013 feet, meaning Shinall rises roughly 55–60 feet higher.
Pinnacle, however, has greater topographic prominence because its summit rises much more dramatically above its immediate surroundings.
The contrast provides a good example of why elevation, prominence, and visual relief are not the same thing.
📏 Prominence and Isolation
Peakbagger calculates Shinall Mountain’s topographic prominence at approximately 526 feet (160 meters).
Its key saddle lies at roughly 543 feet above sea level.
ListsOfJohn gives a similar prominence of approximately 520 feet.
The mountain also has about 10 miles of isolation, meaning a traveler must go roughly ten miles from the summit before encountering terrain that rises higher than Shinall.
That is substantial isolation for a mountain sitting directly beside a major metropolitan area.
🧭 Nearest Higher Neighbor: Moss Mountain
Modern peak data identifies Moss Mountain, west of Shinall Mountain in Saline County, as the nearest higher named summit.
PeakVisor places Moss Mountain at approximately 1,161 feet (354 meters) and roughly 10.1 miles west of Shinall.
ListsOfJohn uses a slightly more complicated parent system, associating Shinall Mountain with an unnamed 1,168-foot summit farther west in the same general Saline County mountain country.
For the Mountain Field Guide’s Nearest Higher Neighbor (NHN) field, Moss Mountain is the most useful named geographical reference.
This corrects an older identification of Crystal Mountain as Shinall’s NHN.
🪨 Don’t Confuse the Two Crystal Mountains
There is an especially important naming issue around Shinall Mountain.
A small Crystal Mountain in Pulaski County lies immediately adjacent to the Shinall Mountain ridge. ListsOfJohn places that summit at only about 945 feet.
That is not the same mountain as the much higher Crystal Mountain (Arkansas) in Saline County.
The Saline County Crystal Mountain reaches approximately 1,729 feet and lies much farther west in Ouachita National Forest.
The two should not be mixed when comparing elevations, nearby peaks, or Nearest Higher Neighbor data.
🏔️ Shinall Mountain and Pinnacle Mountain
Pinnacle Mountain lies only about three miles north-northeast of Shinall Mountain.
The two peaks could hardly look more different.
Pinnacle Mountain is a steep, rocky landmark with extensive boulder fields and a distinctive pointed profile.
Shinall Mountain is a broader forested ridge whose shape is much less dramatic.
Yet Shinall is higher.
Interestingly, Peakbagger identifies Shinall Mountain as Pinnacle Mountain’s Nearest Higher Neighbor.
Pinnacle has an elevation of roughly 1,013 feet and approximately 679 feet of prominence, while Shinall reaches about 1,069 feet but has only around 526 feet of prominence.
So Shinall wins on elevation, while Pinnacle wins on prominence.
🏔️ Part of the Ouachita Mountains
Shinall Mountain belongs to the eastern reaches of the Ouachita Mountains, one of the principal components of the U.S. Interior Highlands.
The Ouachitas extend across western and central Arkansas into southeastern Oklahoma.
Unlike many familiar North American ranges, most Ouachita ridges run approximately east to west.
They consist largely of folded and faulted sedimentary rocks deposited in ancient marine environments.
Farther west, the range becomes considerably higher and more rugged around mountains such as Rich Mountain, Black Fork Mountain, and other high ridges of western Arkansas.
Shinall stands near the eastern end of this great folded mountain system.
🪨 Geology of Shinall Mountain
Shinall Mountain provides an excellent glimpse into the geological architecture of the Ouachitas.
Arkansas geological publications identify the mountain with the Jackfork Formation, a thick sequence of Pennsylvanian-age sedimentary rocks.
Around Shinall Mountain, the formation includes:
- shale
- siltstone
- sandstone
- small quartz veins
- locally occurring quartz crystals
The rocks were originally deposited as sediment hundreds of millions of years ago.
They were later compressed, folded, fractured, and uplifted during the tectonic collision that created the Ouachita Mountains.
🌊 Rocks From an Ancient Ocean
The landscape surrounding modern Little Rock looked unimaginably different when the rocks of Shinall Mountain formed.
During the late Paleozoic Era, sediment accumulated within or along the margins of a deep marine basin.
Underwater currents transported sand, silt, and mud into the basin.
Repeated depositional events eventually built extremely thick layers of sediment.
Burial and pressure transformed those sediments into sandstone, siltstone, and shale.
The Jackfork Formation is particularly well known for deposits produced by sediment moving downslope through deep water, including submarine gravity flows and turbidity currents.
The rocks now standing hundreds of feet above Little Rock therefore began their geological history beneath an ancient sea.
↩️ The Shinall Mountain Syncline
Shinall Mountain has even lent its name to a geological structure: the Shinall Mountain syncline.
A syncline is a fold in rock layers in which the strata bend downward toward the center.
Arkansas Geological Survey field guides describe exposures of shale, siltstone, and sandstone from the middle Jackfork Formation near the axis of the Shinall Mountain syncline.
The surrounding rocks also contain evidence of intense deformation.
Layers have been tilted, fractured, sheared, and locally faulted.
Small quartz veins fill some fractures.
These structures preserve evidence of the tremendous tectonic stresses that acted on the region during formation of the Ouachita Mountains.
🌎 The Ouachita Orogeny
The mountain-building event responsible for the Ouachitas occurred during the late Paleozoic Era as the ancient continents that would become North America and parts of Gondwana converged.
An ocean basin between them gradually closed.
As continental masses approached one another, layers of marine sediment were compressed from the south.
They folded into anticlines and synclines and were pushed across one another along large thrust faults.
This episode is known as the Ouachita Orogeny.
It occurred as part of the enormous tectonic reorganization that ultimately helped assemble the supercontinent Pangaea.
The National Park Service estimates that the ancient Ouachitas may once have reached elevations of roughly 9,000 feet before hundreds of millions of years of weathering and erosion reduced them to their modern form.
🌿 Fossils on Shinall Mountain
Older geological descriptions of Shinall Mountain report plant fossils in dark or bluish-black shale along its slopes.
That fits the broader geology of the Jackfork Formation.
Arkansas geological descriptions note that some Jackfork siltstones contain coalified plant fragments, although fossils are generally much less conspicuous here than in famous fossil beds elsewhere in the state.
These remains help geologists reconstruct the environments surrounding the ancient sedimentary basin.
Any fossils encountered should be left in place unless collecting is clearly permitted by the landowner and applicable regulations.
Much of Shinall Mountain is not public recreational land.
💎 Quartz Veins
Shinall Mountain also contains small quartz veins.
The Arkansas Geological Survey has documented quartz-bearing fractures in sandstone around the Shinall Mountain syncline.
These veins formed when mineral-rich fluids moved through cracks within already-existing rock.
As conditions changed, silica precipitated from solution and crystallized as quartz.
The veins around Shinall are generally far less spectacular than the famous quartz deposits farther west in the Ouachita Mountains, particularly around Mount Ida and Montgomery County.
Nevertheless, they are another visible consequence of the fracturing and fluid circulation associated with the Ouachitas’ complicated geological history.
📡 The Mountain of Towers
For residents of Little Rock, Shinall Mountain may be most recognizable not for its rocks but for its communication towers.
The summit is one of the most important broadcasting locations in central Arkansas.
Television stations, FM radio stations, cellular systems, emergency communications networks, weather services, and amateur-radio operators have all used the mountain.
Its value is easy to understand.
Radio and television signals generally benefit from elevated transmitter locations with clear lines of sight across the surrounding terrain.
Central Arkansas is hilly enough that transmitting from lower sites can create signal obstructions.
Shinall Mountain’s combination of elevation and proximity to Little Rock made it an ideal broadcasting location.
📺 Television on Shinall Mountain
The mountain became important to television during the early years of broadcasting in Arkansas.
Television transmitter facilities were established on Shinall Mountain during the 1950s.
Historical accounts describe construction of a transmitter for KTHV on the mountain, and the summit eventually developed into a large antenna complex serving multiple Little Rock stations.
Modern broadcast infrastructure now dominates sections of the crest.
Some towers rise hundreds of feet above the mountain itself, making them far more visually conspicuous than the summit.
Their red warning lights are particularly visible after dark.
📻 Emergency and Amateur Radio
Shinall Mountain also has an important role in emergency communications.
The Central Arkansas Radio Emergency Network (CAREN) maintains its flagship repeater site on the mountain.
The organization traces its roots to the 1950s and supports public-service and emergency radio communications across central Arkansas.
Shinall’s elevation allows repeater systems to cover a much broader area than would be possible from lower ground.
The mountain is therefore not simply a commercial broadcasting location—it also contributes to communication systems used during emergencies and public-service operations.
📻 Summits on the Air
Shinall Mountain is recognized by the Summits on the Air (SOTA) amateur-radio program.
Its designation is:
W5A/OA-015
SOTA classifies the mountain as a one-point Arkansas summit.
The designation remains in active use, with amateur-radio operators continuing to report activations from Shinall Mountain.
However, a SOTA listing does not mean unrestricted public access is guaranteed.
Operators are responsible for reaching activation areas legally and respecting land ownership and access restrictions.
🛣️ Can You Drive Up Shinall Mountain?
Service roads extend high onto Shinall Mountain because of the extensive communications infrastructure.
Historical peakbagging reports describe driving a maintenance road toward the tower complex.
That should not be interpreted as confirmation that the summit road is currently open to recreational traffic.
Land ownership and access around Shinall Mountain are complicated, and the summit is not maintained as a public mountain park.
Tower compounds themselves are working infrastructure sites and may be fenced or restricted.
Visitors should never bypass gates, barriers, fences, or posted signs.
🥾 Can You Hike Shinall Mountain?
Shinall Mountain should not be presented as a conventional public hiking destination.
There is no established state-park trail leading recreational hikers to the county high point.
Some climbing areas on the Shinall/Chenal ridge have specifically been identified as private property, with climbers asked not to enter without permission.
Older summit reports may describe routes that appeared accessible at the time, but land ownership, gates, road access, and development can change.
Anyone interested specifically in reaching the summit should confirm current legal access rather than relying on historical trip reports.
⚠️ Respect Private Property
This is especially important at Shinall Mountain because its location within the rapidly developing western Little Rock area can create the impression that roads or undeveloped slopes are publicly accessible.
They may not be.
Do not:
- cross posted private property
- drive around locked gates
- enter fenced communications facilities
- climb towers
- trespass on utility roads
- assume an old hiking or climbing report reflects current access
The summit’s status as Pulaski County’s high point does not create a public right of access.
🥾 Better Public Hiking Nearby
Visitors who want to experience the mountain scenery of western Little Rock have excellent public alternatives.
The most obvious is Pinnacle Mountain, approximately three miles north of Shinall.
Pinnacle Mountain State Park provides developed trails, including steep routes to the summit as well as easier trails around the surrounding foothills and waterways.
Another nearby option is Rattlesnake Ridge Natural Area, which is open to the public and contains roughly six miles of hiking and mountain-biking trails.
Rattlesnake Ridge also provides views toward both Pinnacle Mountain and Shinall Mountain.
These destinations offer a much better choice for ordinary recreation than attempting to navigate restricted tower property on Shinall itself.
🌲 Forest and Vegetation
Despite the extensive development near its base and summit, large portions of Shinall Mountain remain forested.
The mountain lies within the Ouachita mixed pine-hardwood landscape.
Oak and hickory species are important components of the forest, along with shortleaf pine and other trees adapted to dry ridges.
Vegetation changes with slope direction and soil moisture.
Sunny, rocky slopes tend to be drier, while protected hollows and north-facing slopes retain more moisture.
The City of Little Rock’s long-range planning has recognized the Shinall Mountain ridgeline as an important open-space landscape, particularly because its steep slopes make extensive development difficult.
🦌 Wildlife
Shinall Mountain’s position on the edge of a growing metropolitan area creates an interesting transition between urban development and natural habitat.
White-tailed deer, raccoons, squirrels, foxes, coyotes, and numerous smaller mammals occur throughout the wooded hills of western Pulaski County.
The forest supports woodpeckers, hawks, owls, songbirds, and migratory species.
Reptiles and amphibians inhabit rocky slopes, forest litter, streams, and moist ravines.
Nearby protected lands such as Rattlesnake Ridge and Pinnacle Mountain State Park help preserve larger connected blocks of habitat within this rapidly growing part of central Arkansas.
🏘️ Shinall Mountain and Chenal Valley
The mountain’s name is closely connected with the Chenal Valley area of western Little Rock.
“Shinall” is widely described as a phonetic or Anglicized form of the French surname Chenault.
Members of the Chenault family settled near the mountain before the Civil War.
The related spelling Chenal later became associated with Chenal Valley and Chenal Parkway.
As a result, Shinall Mountain is sometimes incorrectly written as Chenal Mountain.
The similar spellings are not accidental, but Shinall Mountain is the established geographic name of the summit.
🏙️ A Mountain Beside a Growing City
Few significant Arkansas summits sit so close to a major urban area.
Western Little Rock has expanded dramatically toward and around the foothills during recent decades.
Residential neighborhoods, roads, commercial development, golf courses, and other infrastructure now occupy areas that were once largely rural.
Yet the steep slopes and ridge around Shinall Mountain remain one of western Little Rock’s dominant natural landforms.
The juxtaposition is striking.
From some viewpoints, the mountain appears as a green ridge rising directly behind modern neighborhoods, while enormous broadcasting towers extend hundreds of feet into the sky above it.
Shinall is therefore both a natural landmark and an unmistakable part of Little Rock’s modern skyline.
👀 Where Can You See Shinall Mountain?
Because the summit carries so many towers, Shinall Mountain is relatively easy to identify from surrounding high ground.
It can be seen particularly well from portions of western Little Rock and from trails on nearby ridges.
Rattlesnake Ridge Natural Area specifically provides views toward Shinall Mountain.
Pinnacle Mountain and its surrounding parkland also provide excellent geographic context for understanding the relationship between Shinall Mountain, the Arkansas River Valley, and the eastern Ouachitas.
The tower-covered skyline makes Shinall easier to distinguish than many similarly shaped forested ridges.
🌄 Shinall Mountain vs. Pinnacle Mountain
The comparison between Shinall and Pinnacle Mountain is one of the most interesting geographical quirks in central Arkansas.
| Feature | Shinall Mountain | Pinnacle Mountain |
|---|---|---|
| Approx. Elevation | 1,069 ft | 1,013 ft |
| Approx. Prominence | 526 ft | 679 ft |
| County | Pulaski | Pulaski |
| Public Summit Trail | No | Yes |
| Summit Character | Forested/tower complex | Rocky and exposed |
| County High Point | Yes | No |
| NHN Relationship | Higher mountain | Shinall is Pinnacle’s NHN |
Shinall is higher, but Pinnacle rises more dramatically from its surroundings.
That explains why the lower mountain often appears larger.
🍂 Best Time to Explore the Surrounding Area
Because the summit itself is not a conventional recreation destination, seasonal planning is most relevant to nearby public trails and viewpoints.
Autumn is particularly attractive. Cooler temperatures and colorful hardwood foliage make the eastern Ouachitas one of central Arkansas’s best seasonal landscapes.
Winter opens views through leafless trees and provides comfortable temperatures for steep hikes at Pinnacle Mountain.
Spring brings redbuds, dogwoods, wildflowers, and fresh green foliage.
Summer can be hot and humid, with ticks, mosquitoes, and strong afternoon thunderstorms. Early morning is generally the most comfortable time for strenuous hiking.
🌟 Why Shinall Mountain Is Interesting
Shinall Mountain is not a wilderness summit.
It is something arguably more unusual: an ancient mountain embedded in the modern metropolitan landscape.
Its 1,069-foot summit is the highest natural point in Pulaski County.
Its rocks preserve the remains of sediments deposited hundreds of millions of years ago.
The Shinall Mountain syncline records the folding that occurred during formation of the Ouachitas.
Its name preserves part of central Arkansas’s French settlement history.
Its slopes stand beside some of Little Rock’s newest development.
And its summit has become one of Arkansas’s most important broadcasting and communications locations.
Perhaps most intriguingly, Shinall Mountain quietly rises higher than Pinnacle Mountain, the dramatically shaped neighbor that receives almost all the attention.
For anyone exploring the geography of the Ouachita Mountains and central Arkansas, Shinall Mountain is a small summit with an unexpectedly large story.
❓ Frequently Asked Questions
Where is Shinall Mountain?
Shinall Mountain is in Pulaski County, Arkansas, on the western edge of the Little Rock metropolitan area near Chenal Valley.
How high is Shinall Mountain?
Modern LiDAR data places Shinall Mountain at approximately 1,069 feet (326 meters).
Older sources commonly report elevations between about 1,056 and 1,066 feet.
Is Shinall Mountain the highest point in Pulaski County?
Yes. Shinall Mountain is the highest natural point in Pulaski County.
Is Shinall Mountain higher than Pinnacle Mountain?
Yes. Shinall is roughly 55–60 feet higher than nearby Pinnacle Mountain.
Pinnacle Mountain has greater prominence and looks much steeper, however.
What is Shinall Mountain’s prominence?
Modern Peakbagger data gives Shinall Mountain approximately 526 feet of topographic prominence.
What is Shinall Mountain’s Nearest Higher Neighbor?
The nearest higher named summit is Moss Mountain, approximately ten miles west in Saline County.
Is Crystal Mountain the NHN of Shinall Mountain?
No. Modern peak data does not support the nearby Crystal Mountain as Shinall’s NHN.
There is also considerable potential for confusion because a small Crystal Mountain lies beside Shinall in Pulaski County, while the much higher Crystal Mountain (Arkansas) profiled separately by Mountain Field Guide is in Saline County.
Is Shinall Mountain part of the Ouachita Mountains?
Yes. Shinall Mountain lies in the eastern foothills of the Ouachita Mountains.
Can you hike to the summit?
There is no established public recreational summit trail.
Access around the tower complex and some surrounding climbing terrain involves private or restricted property, so visitors should obtain permission and obey all gates and posted signs.
Why are there so many towers on Shinall Mountain?
Its elevation and location beside Little Rock make the summit extremely useful for television, FM radio, cellular, emergency, weather, and amateur-radio communications.
What kind of rock is Shinall Mountain made from?
The mountain is associated primarily with the Jackfork Formation, consisting of Pennsylvanian-age sandstone, shale, and siltstone.
What is the Shinall Mountain syncline?
It is a folded geological structure in which layers of Jackfork rock bend downward toward the center. The feature records some of the deformation associated with formation of the Ouachita Mountains.
Where does the name Shinall come from?
The name is generally understood as a phonetic or Anglicized form of the French surname Chenault, associated with settlers who lived near the mountain.
🔗 Related Articles
- Pinnacle Mountain (Arkansas)
- Crystal Mountain (Arkansas)
- Ouachita Mountains
- Ouachita Pinnacle
- Smith Pinnacle
- Potato Hill Mountain
- Rich Mountain (Arkansas, Oklahoma)
- Mountain Ranges in the U.S.
📚 Sources
- Peakbagger — Shinall Mountain — Modern LiDAR elevation, prominence, isolation, coordinates, county high-point status, and USGS quadrangle.
- ListsOfJohn — Shinall Mountain — Elevation, prominence, saddle, isolation, parent data, and Pulaski County ranking.
- ListsOfJohn — Pulaski County Peaks — Comparison with Pinnacle Mountain, Bear Den Mountain, and the nearby Pulaski County Crystal Mountain.
- PeakVisor — Shinall Mountain — Nearest higher named summit, isolation, prominence, and regional mountain data.
- Arkansas Geological Survey — A Guidebook to the Geology of the Ouachita Mountains — Shinall Mountain syncline, Jackfork Formation, quartz veins, folding, and local geology.
- Arkansas Geological Survey — General Geology and Mineral Resources of the Ouachita Mountains — Jackfork Sandstone lithology, age, depositional history, and coalified plant fragments.
- Arkansas Geological Survey — Geology Resources — Ouachita Mountain geology, folding, faults, rock types, and east-west ridge structure.
- National Park Service — Collisional Mountain Ranges: Ouachita Mountains — Tectonic evolution and ancient scale of the Ouachita Mountains.
- Encyclopedia of Arkansas — Central Arkansas Radio Emergency Network — CAREN history and its flagship Shinall Mountain communications site.
- Encyclopedia of Arkansas — Cecil Lowery Suitt — Historical information about construction and operation of television transmitter facilities on Shinall Mountain.
- City of Little Rock — Land Use Plan — Chenal district planning, Shinall Mountain ridgeline, steep slopes, development, and open-space planning.
- Mountain Project — Shinall (Chenal) Mountain — Current private-property warning for climbing terrain on the Shinall/Chenal Mountain area.
- The Nature Conservancy — Rattlesnake Ridge Natural Area — Public hiking access, trails, and views toward Shinall and Pinnacle Mountains.
- On The Air — SOTA Alerts — Recent confirmation of Shinall Mountain’s active SOTA reference W5A/OA-015.
