Caves

 

 

Geology and Karst Physiography

Dry Creek and the adjacent Swago Creek basin occupy the northern boundary of the Greenbrier Karst region in southern Pocahontas County. Physiographically, the valley is a classic fluviokarst system—a landscape combining standard fluvial surface valleys with subterranean drainage networks developed within Mississippian-age Greenbrier Limestone.

 * Subterranean Piracy and "Dry" Valley Morphology: Dry Creek earned its name from significant stream sinking. While surface water flows through the hollow during heavy rain or spring thaw, most normal runoff sinks into swallets and fractures in the soluble limestone bedrock.

 * Overholt Blowing Cave Connection: Dye tracing and speleological mapping reveal that the underground drainage beneath Dry Creek Valley connects directly into the Overholt Blowing Cave system. The underground stream from Overholt Blowing Cave extends nearly to the head of the Dry Creek Valley, while portions of the upper valley's drainage are pirated eastward beneath surface ridges toward base-level discharge springs along the Greenbrier River.

 * Stratigraphic Controls: The drainage pathway is strongly shaped by the dipping carbonate strata (predominantly Union and Pickaway limestones) bounded by insoluble layers such as the Maccrady Shale below and clastic caprock formations above, which funnel surface water vertically through sinkholes and fissures into horizontal cave conduits.

Early Pioneer Settlement and Local History

The fertile limestone soil and timber of the Swago and Dry Creek drainages made them prime areas for late 18th- and early 19th-century homesteading following early exploration in the Greenbrier Valley.

 * The McNeel (McNeil) Settlement: The Swago and Dry Creek valleys were central to the expansion of the pioneer McNeel family. Jonathan McNeel (son of pioneer Thomas McNeel) established an active economic center at Swago Mill, operating grist milling, weaving, cloth fulling, and powder manufacturing. His wife, Phoebe Moore McNeel (daughter of Moses Moore), was an early frontier figure who survived regional border conflicts, including the 1780s Drinnan raid era.

 * Dry Creek Homesteads: Jonathan and Phoebe’s sons settled along the creek:

   * Moore McNeel married Martha McNair (and later Nancy Auldridge) and homesteaded near the mouth of Dry Creek.

   * John McNeel married Rebecca McNeel and settled further up Dry Creek. He served as a county court justice, local schoolmaster, prominent Methodist Episcopal leader, and early community medical practitioner who provided botanical and practical remedies across the Little Levels and Swago districts.

 * Agricultural & Timber Era: Throughout the 19th and early 20th centuries, Dry Creek transitioned from small-scale subsistence farms and water-powered gristmills to livestock grazing and selective logging, taking advantage of the Greenbrier Valley rail corridor after the Chesapeake and Ohio Railway built through nearby Buckeye and Marlinton at the turn of the century.

Regional Karst Hydrology & Structural Setting

The Swago Creek and Dry Creek karst drainage basins lie within the Appalachian Plateau Province along the western limb of the Browns Mountain Anticline. The subterranean hydrology is developed primarily within the Mississippian Greenbrier Group (limestones totaling 400–600 feet in thickness, notably the Union, Pickaway, Taggard, Patton, and Sinks Grove members), underlain by the impervious Maccrady Shale and capped by clastics of the Mauch Chunk Group.

The regional structure exhibits a gentle regional dip toward the northwest (roughly 2^\circ\text{ to }5^\circ). Groundwater movement is governed by a combination of strike-oriented conduits, downdip vadose canyons, and stratigraphic confinement along the Maccrady contact, discharging into trunk resurgences along the Greenbrier River base level.

Primary Cave Systems & Surveyed Conduits

The Swago–Dry Creek karst complex contains several extensive, multi-mile subterranean drainage conduits surveyed largely by the West Virginia Speleological Survey (WVSS) and the National Speleological Society (NSS).

 * Overholt Blowing Cave System:

   * Passage Extent: Extends over 4.5\text{ to }5\text{+ miles} of surveyed multi-level canyon and phreatic trunk passages.

   * Morphology & Flow: The cave's active master stream channel originates beneath the upland sinkhole plain and blind valleys of Dry Creek and upper Swago. It features a massive blowing entrance that discharges cold air due to barometric and thermal chimney effects linked to high-elevation surface swallets.

   * Stratigraphy: Conduits are developed through the massive Union and Pickaway limestones, cutting down to near-perched vadose streams resting near the lower Patton/Maccrady contact.

 * Friars Hole Cave System Connection (Hydrologic Margin):

   * While the main Friars Hole System lies primarily southwest along the Droop Mountain / Spring Creek divide, the extreme northern recharge and strike-oriented peripheral conduits intercept drainage divides shared with the Swago and Dry Creek subterranean headwaters.

 * Swago Pit / Cave Conduits:

   * Includes vertical insurgences and pit-caves (such as Swago False Bottom Pit and associated swallets) that drop 50\text{ to }150\text{ feet} vertically through upper cherty limestones into narrow vadose slots, capturing ephemeral runoff from non-carbonate ridge caps.

 * Carpenters Pit & Tub Cave Complex:

   * Subordinate tributary inputs along the lower flanks of the basin that feed direct conduit branches into the trunk flow network heading toward the Greenbrier River resurgence line.

Dye-Tracing & Subsurface Flow Paths

Fluorescein and optical brightener dye-tracing investigations conducted across the Swago–Dry Creek watershed have established critical subsurface capture routes that deviate significantly from surface topographic divides:

[Surface Infiltration: Dry Creek & Swago Swallets]

                         │

                         ▼

        [Vertical Vadose Shafts & Sinkholes]

                         │

                         ▼

      [Overholt Blowing Subterranean Master Stream]

                         │

                         ▼

       [Base-Level Resurgences on Greenbrier River]

 * Inter-Basin Piracy of Dry Creek: Dye injected into sinking surface streams in the upper Dry Creek valley confirms that water does not follow the dry surface stream bed during low-to-moderate flow. Instead, it is pirated sub-surface, traversing north-northeast through phreatic tubes into the Overholt Blowing master conduit.

 * Sub-Mauch Chunk Recharge: Runoff from the sandstones and shales of the Mauch Chunk caprock on adjacent ridges sinks immediately upon contacting the top of the Greenbrier Limestone (often via blind valleys and contact springs).

 * Terminal Resurgences: Subterranean waters route beneath surface ridges to discharge at major tubular spring outlets (such as the Overholt Resurgence / Greenbrier River springs near Buckeye/Marlinton) at river level (approx. 2,080\text{–}2,120\text{ feet} elevation), representing a total vertical hydrologic drop of 300\text{ to }600\text{ feet} from the high upland capture points.

The Greenbrier Group in southern Pocahontas County comprises roughly 400\text{ to }600\text{ feet} of middle-to-late Mississippian carbonates. Variations in chemical purity, bedding thickness, and insoluble clastic interbeds across its constituent members govern the cross-sectional geometry, vertical dropping, and horizontal branching of cave passages in the Swago and Dry Creek basins.

Stratigraphic Column and Passage Morphologies

Member / Formation	Lithological Character	Cave Passage Morphology in Swago Basin
Alderson / Greenville (Upper Transition)	Thin-bedded, argillaceous, fossiliferous limestone interbedded with calcareous shale.	Inception & Perching Horizons: Highly resistant to major void formation; retards rapid vertical dissolution. Sinking streams often run on top until finding major tectonic joints.
Union Limestone (~150–200 ft)	High-calcium, massive to thick-bedded, cross-bedded oolitic and bioclastic calcarenite (>90\%\text{ CaCO}_3).	Massive Phreatic Trunks & Large Rooms: Highly soluble. Hosts the largest tubular conduits, upper abandoned paleotrunks, high-arched elliptic passages, and large breakdown chambers in Overholt Blowing Cave.
Pickaway Limestone (~100–150 ft)	Medium-bedded, impure, silty/argillaceous limestone with distinctive "sheeted" or "ribbon" weathering and chert nodules.	Keyhole Passages & Vertical Shafts: Impure argillaceous parting forces vertical downcutting along joints rather than lateral widening. Forms narrow vadose canyon slots, fluted vertical pits, and entrenched stream beds beneath Union tubes.
Taggard Formation (~15–30 ft)	Clastic marker bed of red and greenish-gray shale, siltstone, and thin argillaceous limestone.	Hydraulic Perching & Step-Downs: Acts as a regional aquitard/aquiclude. Conduits flowing through the Union/Pickaway often level out into low crawls on top of the Taggard or breach it abruptly via vertical waterfalls and plunge pools.
Patton Limestone (~80–120 ft)	Dense, dark gray, thick-bedded micritic and sparitic calcilutite/calcarenite with sparse nodular chert.	Deep Active Stream Conduits: Highly competent rock that supports deeply incised vadose canyons and stable active streamways. Often forms the final lower level of trunk passages before reaching base level.
Sinks Grove / Hillsdale (~50–80 ft)	Dark, dense, cherty, dolomitic to siliceous limestone with heavy black chert nodules.	Restricted Conduit Geometries: Prominent insoluble chert ribbons protrude from passage walls. Passages are frequently irregular, low, and constrained by bedding joints.
Maccrady Shale (Basal Contact)	Impermeable, thick red and green mudstone/shale (Mississippian).	Basal Aquitard / Conduit Floor: Prevents further downward dissolution. Forces deep subterranean streams to track along the stratigraphic strike or dip toward the Greenbrier River resurgences.

Morphological Controls and Conduit Evolution

The interaction between these units creates the distinctive hybrid profiles observed in the Swago and Dry Creek networks:

• T-Shaped & Keyhole Profiles: A typical master conduit begins phreatically at the water table within the pure Union Limestone, dissolving broad, horizontal elliptical tubes. As regional base level drops, downcutting streams enter the siltier, joint-controlled Pickaway Limestone, incising a narrow, deep vadose trench into the floor of the original tube.
• Vertical Shaft Cascades: Sinking runoff captured at the surface drops straight down vertical pit features through the upper units until striking the Taggard Shale, where water travels horizontally along the shale contact before breaking through into the Patton Limestone.
• Basal Strike Runoff: Upon descending to the Maccrady Shale, water can no longer dissolve downward; it is forced into lateral, strike-oriented master conduits that convey large volumes of drainage northeastward to river-level resurgence springs.

Multiple complex rescues and incident responses have occurred in the Swago Creek and Dry Creek karst systems over decades of exploration, recorded primarily through the National Speleological Society (NSS) and the Eastern Region of the National Cave Rescue Commission (ER-NCRC).

Notable Swago Basin Rescues and Incidents

• Carpenter’s / Swago Pit Extraction:
  • One of the most demanding early rescues in the basin involved two severely injured cavers: one sustaining a depressed skull fracture from falling rock/gear, and another breaking both arms.
  • The rescue required regional grotto mobilization to rig haul systems, haul both litters up a vertical 120\text{-foot} entrance shaft, and transport them through approximately three-quarters of a mile of tight, high-relief passage to reach the surface.
• Carpenter Swago Cave Fall (April 2002):
  • A caver suffered a vertical fall resulting in traumatic injury within Carpenter Swago Cave, requiring an organized multi-agency response, underground stabilization, and technical rope hauling.
• Overholt Blowing Cave Flash Flooding & Entrapment Hazards:
  • Because Overholt Blowing Cave acts as a primary subterranean storm sewer for the sinking streams of Dry Creek, exploration teams have encountered rapid hydraulic surges. Several operations have involved locating and escorting stranded survey teams cut off by sumped or flooded low-airspace passages after unexpected surface storms.
• Nearby System Rescues (Cassell Cave & Friars Hole Margins):
  • Just across the topographic divides from Swago and Dry Creek, technical rescues—such as fall-related litter extractions in Cassell Cave (including major incidents in 2002) and deep-system search/extraction missions along the Friars Hole Cave boundaries—regularly draw on the specialized cave rescue call-down networks established across Pocahontas and Greenbrier counties.

Rescue Challenges Specific to the Basin

• Vertical Pit Riggings: Most swallets along Dry Creek and Swago drop through sheer vertical shafts (50\text{ to }150\text{ feet}) before reaching horizontal passages, 

 

Pocahontas County is situated in one of the most cave-dense karst regions in eastern North America, underlain heavily by Mississippian Greenbrier Limestone.

Major Cave Systems & Multi-Mile Networks

• Friars Hole Cave System — Straddles the Pocahontas–Greenbrier border on the western flank of Droop Mountain. At over 50 miles of surveyed passage, it is one of the longest cave systems in the United States and the second-longest in West Virginia. Major entrances and internal sectors associated with Pocahontas County include:
  • Snedegar's Cave (including Snedegar's Staircase, Snedegar's Saltpeter, and Snedegar's North)
  • Canadian Hole
  • Rubber Chicken Cave
  • Crookshank Pit
  • Toothpick Cave
  • Icebox Cave
• Cassell Cave System — Located on Back Allegheny Mountain, featuring more than 8 miles of surveyed, highly intricate passages.
• Cass Cave — Situated on Cheat Mountain near Cass; famous for the massive "Big Room" (800 ft long, 180 ft high) and the 139-foot underground waterfall (Lacy Suicide Falls).
• Carpenter-Swago Cave System — A connected karst drainage complex in the Swago Creek basin encompassing over 5.5 miles of mapped passage.
• Simmons Mingo / My Cave System — Straddles the Pocahontas–Randolph county border along the upper Elk River basin.

Swago Creek & Marlinton Karst Area

• Overholts Blowing Cave (One of the deepest and most notable spring resurgence caves in the county)
• Cave Creek Cave
• Tub Cave
• Barnes Pit
• Dry Creek Cave
• Hause Waterfall Cave
• Schoolcraft Cave

Back Allegheny, Cheat Mountain & Northern Basins

• Billy Clay Pit & Clay Pit #2 (Preserved by the Mid-Atlantic Karst Conservancy)
• Sharps Cave
• Wanless Cave
• Beverly Cave
• Ruckers Cave
• Warwick Cave
• Cloverlick Valley Solution Pits

Hillsboro, Little Levels & Southern Pocahontas

• Poor Farm Cave (Poorfarm Cave — significant for Pleistocene paleontological discoveries)
• Martha Cave (Martha's Cave)
• Salmon Cave
• Piddling Pit
• Shinaberry Cave
• Turkey Roost Cave
• Soup City Cave
• Clyde Cochrane Sink / Cave
• Sewell's Cave (Historic limestone shelter and cavern near Mill Point associated with early pioneer Stephen Sewell)
• Hills Creek Sinks (Subterranean drainage swallowing Hills Creek before resurging into the Greenbrier drainage)

(Most caves in Pocahontas County are on private land, within protected karst conservancy preserves like the WVCC/MAKC, or subject to access restrictions to protect bat habitats and preserve fragile karst hydrology.)

 

IMAGINARY STORY

 

The cold bit through Sarah’s coveralls, ignoring the layers of polypro beneath. It was the damp, static cold of fifty degrees that felt like freezing, typical for Pocahontas County in November, and entirely normal when you were two hundred feet underground.

She paused, wiping a smear of clay from her headlamp. Beside her, Marcus was meticulously brushing away loose debris from a pale protrusion embedded in the muddy floor of Poor Farm Cave.

“You see it?” he asked, his voice echoing flatly in the narrow, limestone-ribbed chamber.

“I see it,” Sarah replied, leaning closer. “Looks like a femur. Not human. Too thick.”

Poor Farm Cave wasn't exactly famous among recreational cavers. It lacked the massive, echoing rooms of Cass Cave or the endless, winding labyrinth of the Friars Hole system just down the road. Instead, Poor Farm was a tight, muddy, often wet slog. But for paleontologists, it was something else entirely. It was a natural trap—a limestone sink that, over thousands of years, had swallowed the unwary, the injured, and the dead.

Marcus switched to a smaller brush, revealing the distinctive curve of the bone. “Pleistocene, definitely. Given the strata, I’d bet money this is part of the megafauna deposit we were looking for.”

He was talking about the Late Pleistocene epoch, a time when the Little Levels of Pocahontas County—the broad, fertile valley just outside the cave entrance—was covered not in farmland, but in sub-boreal spruce and pine forests.

“Megalonyx?” Sarah suggested, referring to the giant ground sloth that once lumbered across North America. Thomas Jefferson had described one from a cave just over in Monroe County.

“Maybe,” Marcus said, “but look here.” He tapped a smaller, sharper fragment protruding near the femur. “That’s a tooth. A canine, I think.”

Sarah crouched lower, letting her headlamp illuminate the jagged shape. It was dark, stained by thousands of years of mineral absorption, and it was large.

“Dire wolf,” she breathed, the realization sending a thrill through her that momentarily banished the cold. Aenocyon dirus.

“Or a short-faced bear,” Marcus cautioned, always the skeptic. “We won't know for sure until we get it back to the lab at Morgantown and compare it with the Smithsonian's casts.”

For the next three days, they lived in a subterranean routine. They’d enter the cave shortly after dawn, navigate the slick, mud-coated descent past the “Corkscrew” formation, and spend hours in the cramped excavation trench.

They weren't the first to find bones in Poor Farm. Local legends always spoke of "monster bones" pulled from the sinkholes around Hillsboro. But this excavation was different. They were carefully documenting the stratigraphy, reading the layers of sediment like a book to understand the changing climate of the Appalachian mountains.

By the end of the week, they had uncovered not just a single animal, but a chaotic jumble of remains. It appeared a small pack of dire wolves—perhaps pursuing prey, perhaps seeking shelter from a sudden snowstorm—had fallen into the vertical shaft that once opened directly above the chamber.

They found the remains of their prey, too: the shattered pelvis of a flat-headed peccary, an extinct type of pig that roamed the ice age forests.

“It’s a snapshot,” Sarah said on their final day, as they carefully packed the stabilized fossils into padded crates for the difficult haul to the surface. “A bad day for a wolf pack, frozen in mud for twenty thousand years.”

Marcus nodded, securing a lid. “And a good day for us. This changes the known range of the dire wolf in the eastern mountains. They weren't just in the lowlands; they were hunting right up here on the plateau.”

 

 

The dire wolf (Aenocyon dirus) was a heavily built, apex hypercarnivore that roamed the Americas during the Late Pleistocene epoch before going extinct around 10,000 to 13,000 years ago.

Anatomy & Physical Build

• Body Structure: Roughly 5 feet (1.5 m) long from snout to tail tip, standing about 2.6 to 2.8 feet (80–85 cm) tall at the shoulder.
• Weight: Averaged 130–150 lbs (60–68 kg), with exceptionally large specimens reaching nearly 175–200 lbs—making it roughly 25% heavier on average than a modern gray wolf (Canis lupus).
• Skeletal Stature: Possessed shorter, thicker, and more robust limb bones relative to its body size. This gave the dire wolf a stockier frame built more for grappling and wrestling powerful megafauna than for long-distance pursuit endurance.
• Skull & Bite Force: The skull was broader, with heavily reinforced zygomatic arches (cheekbones) and a massive sagittal crest to anchor powerful jaw musculature. Its bite force was among the strongest of any known canine, capable of crushing through large mammal bones.
• Dentition: Larger, stouter teeth with thicker enamel and specialized carnassials compared to modern wolves, adapted to shear thick hide and pulverize bone.

Dire Wolf vs. Gray Wolf Comparison

Trait	Dire Wolf (Aenocyon dirus)	Gray Wolf (Canis lupus)
Build	Heavy, muscular, stocky	Lean, agile, built for pursuit
Average Weight	130–150+ lbs	80–110 lbs
Limbs	Shorter, robust, thicker bone density	Longer, leaner, optimized for endurance
Skull & Jaws	Broad, massive sagittal crest, bone-cracking bite	Narrower muzzle, slicing bite
Evolutionary Lineage	Distinct American lineage; sister to jackals/dholes	Eurasian origin; modern Canis

Evolutionary Insights

Recent genomic sequencing has revealed that the dire wolf was not a true wolf (Canis), but rather belonged to its own distinct genus (Aenocyon). Its lineage diverged from the ancestors of modern gray wolves, coyotes, and jackals over 5.7 million years ago in the Americas.

Its superficial resemblance to the gray wolf is a classic example of convergent evolution, where two distinct evolutionary lineages independently evolved similar body plans to fill the same ecological niche.

As they emerged from the cave entrance, the sudden warmth and bright sunlight of the late afternoon felt almost aggressive. Sarah looked out across the rolling farmland of the Little Levels, imagining it as it was: a harsher, wilder landscape, where giant sloths tore at the trees and dire wolves stalked through the snow, their bones waiting patiently in the dark belo

The extinction of the dire wolf (Aenocyon dirus) versus the survival of the gray wolf (Canis lupus) comes down to a classic evolutionary showdown: extreme specialization versus broad adaptability during a period of abrupt ecological collapse.

Specialization vs. Dietary Flexibility

• Megafaunal Dependence: Dire wolves were hypercarnivores specialized in ambushing and overpowering massive Pleistocene herbivores—such as bison, horses, camelids, and ground sloths.
• Collapse of the Food Web: During the Quaternary extinction event (~13,000–10,000 years ago), North America lost roughly 70% of its megafauna due to rapid climatic warming, shifting vegetation, and increasing human hunting pressure.
• The Gray Wolf’s Broad Diet: Gray wolves were dietary generalists. When large game vanished, gray wolves readily shifted their diets to smaller, faster prey (deer, elk, rabbits, rodents) and even scavenged vegetation or fish. The heavily built dire wolf could not sustain its high caloric requirements on small, elusive game.

Locomotion and Hunting Mechanics

• Grappling vs. Endurance: The dire wolf's skeleton featured shorter, denser limbs and a heavier torso, optimized for close-quarters grappling and wrestling large prey to the ground rather than running long distances.
• The Speed Deficit: As open woodlands transformed and megafauna disappeared, surviving prey species became smaller, faster, and more agile. The dire wolf lacked the cursorial endurance and speed required to chase down swift animals like pronghorn or white-tailed deer.

Genetic Isolation and Inability to Hybridize

• Deep Evolutionary Divergence: Ancient DNA studies show that dire wolves diverged from other canines over 5.7 million years ago, making them an isolated evolutionary lineage (Aenocyon) rather than close relatives of Canis lupus.
• No Genetic Rescue: While gray wolves, coyotes, and domestic dogs frequently hybridized across Eurasia and North America—swapping adaptive alleles that boosted immunity and survival—the dire wolf had been genetically isolated in the Americas for millions of years. It could not interbreed with invading Eurasian canids to adapt to new environmental pressures or pathogens.

Key Survival Factors

Factor	Dire Wolf (Aenocyon dirus)	Gray Wolf (Canis lupus)
Ecological Role	Hyper-specialized megafaunal predator	Versatile generalist predator & scavenger
Primary Prey	Large megafauna (horses, sloths, ancient bison)	Variable (mega-herbivores to rodents and fish)
Hunting Strategy	Short-burst ambushing & bone-crushing grappling	Long-distance pursuit & high-endurance coursing
Geographic Origin	Endemic American lineage (evolutionarily isolated)	Adaptable Eurasian migrant across Beringia
Outcome	Extinct (~10,000–12,000 years ago)	Surviving apex predator today

 

 

•  
• requiring technical counter-balance hauling systems for litter extrication.
• Hypothermia & Inundation: Water temperatures in the Greenbrier aquifer hover around 50^\circ\text{F to }52^\circ\text{F} (10^\circ\text{C to }11^\circ\text{C}). The rapid catchment of surface runoff from Mauch Chunk sandstone caps makes rapid inundation and severe hypothermia the primary operational risks during prolonged extractions.

The cold bit through Sarah’s coveralls, ignoring the 

The Kee and Armstrong Families

 

The Kee (Key) family of Pocahontas County traces its lineage to George Kee (1772–1863), a native of County Tyrone, Ireland, who arrived in America around 1780. After migrating through Pennsylvania and Pendleton County, he settled in the Little Levels and married Esther "Hetty" Buckley, establishing the family seat south of Marlinton at what became known as Kee Flats near Buckeye (where the original 1830s Kee log cabin stood, later preserved by the Pocahontas County Historical Society).

Key Family Lines & Intermarriages

• Buckley Connection
  • Esther "Hetty" Buckley (daughter of pioneer settler Joshua Buckley and Hannah Collins) married George Kee. The Buckley settlement along the Greenbrier River opposite Swago Creek firmly anchored the Kee family into early regional frontier history.
• McNeill (McNeil) Connection
  • Aaron Kee (son of John Kee and grandson of George Kee) married Mildred "Milly" McNeill, daughter of Jonathan McNeill and Angelina Adkisson of Buckeye. They maintained and farmed the original Kee family homestead.
• Poage Connection
  • Hester Kee (daughter of John Kee and Hester Gwin) married into the prominent Poage family of the Levels/Edray district twice: first to William Poage, and following his death, to Henry Poage.
• McKeever Connection
  • Alcinda Kee (daughter of John Kee) married George McKeever, connecting the family directly with the McKeever settlements along Swago Creek.
• Gwin Connection
  • John Kee (son of George Kee), a noted wagonmaker and farmer, married Hester Gwin, daughter of James Gwin, Sr. (of Highland County) and niece of Rebecca Stephenson/Gwin.
• Duncan Connection
  • Andrew Kee (son of George Kee), an expert marksman and hunter, married Mary Duncan (sister of Henry Duncan, originally from the Collierstown area of Rockbridge County, Virginia). Their homestead near Buckeye later passed to William A. Duncan.
• McCollam, Palser, & Moore Connections
  • William Kee (son of George Kee) married Ruth McCollam, settling on land later associated with Capt. J. R. Apperson.
  • Their son, Confederate veteran George M. Kee, married first Mary J. Palser and second Rachel Moore.
• Stevenson Connection
  • Joshua Kee (eldest son of George Kee), renowned locally as a master gunsmith, stonemason, and woodworker, married Rebecca Stevenson of Bath County and settled along the Greenbrier River just below Marlinton.

Primary Inter-Family Summary

Family Line	Primary Alliance / Marriage	Geographic Footprint
Buckley	George Kee \leftrightarrow Esther "Hetty" Buckley	Greenbrier River / Swago
McNeill	Aaron Kee \leftrightarrow Milly McNeill	Buckeye / Kee Flats
Poage	Hester Kee \leftrightarrow William Poage / Henry Poage	Edray District / Levels
McKeever	Alcinda Kee \leftrightarrow George McKeever	Swago Creek
Gwin	John Kee \leftrightarrow Hester Gwin	Kee Flats / Buckeye
Duncan	Andrew Kee \leftrightarrow Mary Duncan	Buckeye / Stony Creek
McCollam	William Kee \leftrightarrow Ruth McCollam	Buckeye / Marlinton
Moore / Palser	George M. Kee \leftrightarrow (1) Mary Palser / (2) Rachel Moore	Buckeye area
Stevenson	Joshua Kee \leftrightarrow Rebecca Stevenson	Lower Marlinton / Greenbrier

Joshua Buckley Kee (1807–1885) was the eldest son of pioneer George Kee and Esther Buckley. County records and local histories—particularly Rev. William T. Price’s Historical Sketches of Pocahontas County (1901)—highlight his craftsmanship, homestead, and family line.

Mechanical Skill & Gunsmithing Trade

• Master Craftsman: Joshua Kee was widely recognized across the region for his versatile mechanical aptitude, working proficiently in stone, iron, and wood in addition to managing his farm.
  
  
• Gunsmithing Specialty: His primary craft was gunsmithing, an essential trade in 19th-century Pocahontas County when hunting and frontier defense remained central to daily sustenance and commerce.
  
  
• Community Role: Local historical accounts note that his firearms craftsmanship was considered exceptional and provided a vital service to hunters and settlers throughout the Greenbrier Valley.
  
  

Homestead & Estate

• Location: Rather than remaining on the main Kee Flats plateau where his father settled, Joshua established his own farm and shop on the east bank of the Greenbrier River, approximately one mile below Marlinton (between Marlinton and Buckeye).
  
  
• Operations: His property functioned as both a productive river-bottom farm and a specialized metal and woodworking shop where he forged rifle components, repaired agricultural tools, and handled specialized local metalwork.
  
  

Marriage & Descendants

• Marriage: Joshua married Rebecca Stevenson of Bath County, Virginia.
  
  
• Children:
  
  
  • Esther Kee
    
    
  • Rachel Kee
    
    
• Lineage Note: Tragically, both daughters passed away around the time they reached adulthood, leaving no surviving direct descendants from Joshua B. Kee's immediate branch.
  
  

Consequently, subsequent generations carrying the Kee surname in Pocahontas County descend primarily through Joshua's brothers—notably William Kee (who married Ruth McCollam) and Andrew Kee (who married Mary Duncan)—as well as through his sister Hannah Kee, who married Timothy Clunen and established extensive lines in the Buckeye and Swago Creek areas.

The Armstrong family of Pocahontas County and the surrounding Allegheny Highlands traces its lineage to the Scotch-Irish migrations of the early to mid-18th century. Originating in the Scottish Borderlands and Ulster (Northern Ireland), the family entered North America primarily through ports in Pennsylvania and Delaware before following the Great Wagon Road south into the Shenandoah Valley (Old Augusta County, Virginia) and westward over the Allegheny crest.

Pioneer Settlement & Regional Lineage

As frontier settlements expanded across Augusta, Bath, and Greenbrier counties in the mid-1700s, several Armstrong branches established homesteads along the headwaters of the Jackson River, Bullpasture, Cowpasture, and the Upper Greenbrier River basin:

• Archibald Armstrong & Early Land Claims: By the 1750s and 1760s, Archibald Armstrong acquired frontier tracts on the Jackson River and Muddy Run, near the boundaries of present-day Bath, Highland, and Pocahontas counties. These early tracts adjoined settlements of the pioneer Ewing, Moore, and Jamison families.
• Robert, Thomas, and William Armstrong Lines: Parallel branches established footholds along the Jackson River and the Bullpasture Valley (Highland County), with branches gradually moving west into Pocahontas County across the gaps of Allegheny Mountain and Back Creek Mountain.
• Pocahontas County Settlements: Over the late 18th and 19th centuries, Armstrong descendants settled throughout Pocahontas County, notably in the Huntersville, Knapp's Creek, Buckeye, Edray, Marlinton, and Little Levels districts.

Key Family Alliances & Marriages

Genealogical records in Pocahontas, Bath, and Highland show extensive intermarriages between the Armstrongs and established pioneer clans:

Intermarried Family	Regional Connection & Geographic Footprint
Ewing	Jackson River, Muddy Run, and Swago Creek
Moore / McCarty	Knapp's Creek, Marlinton, and Laurel Run
Burgess / Kinnison	Levels, Stamping Creek, and Hillsboro vicinity
Sharp / Siron / Pyles	Edray, Frost, and the Highland/Pocahontas border ridges
Taylor / Beale / Clark	Buckeye, Central Greenbrier Valley, and Droop Mountain

Migrations & Destinations

Like many families living in the narrow mountain valleys where arable bottomland became scarce by the 1820s–1850s, successive generations of Armstrongs took part in key outward migration waves:

• Adjacent Central West Virginia Counties: Branches moved westward deeper into the central plateau of West Virginia, particularly settling along the Elk and Little Kanawha watersheds in Braxton, Lewis, Randolph, Webster, Nicholas, and Kanawha counties.
• The Northwest Territory / Ohio Valley: Between 1800 and 1840, several sons and daughters joined the broad migration trail through the Kanawha Valley to southern and central Ohio (notably Gallia, Ross, Pickaway, and Scioto counties) and into Indiana.
• Trans-Mississippi West: By the mid-19th century and the post–Civil War period, Armstrong lines relocated further west to farm the prairie lands of Illinois, Iowa, and Missouri, while others moved into the Pacific Northwest timber and rail settlements.

DRIFTWOOD

 

Historical Report: From Frontier Defense to Industrial Extraction in Pocahontas County, West Virginia

1. Lord Dunmore, Frontier Defense, and the 1774 Campaign

Lord Dunmore and Western Mobilization

John Murray, 4th Earl of Dunmore (1730–1809), served as the final Royal Governor of the Colony of Virginia (1771–1776). While remembered nationally for the 1775 Gunpowder Incident and his loyalist proclamation offering emancipation to enslaved individuals fighting for the Crown, his impact on western Virginia was shaped by Dunmore’s War (1774).

Faced with escalating tensions along the Ohio River following unauthorized settler expansion and frontier violence (including the Yellow Creek Massacre), Dunmore organized an offensive campaign against a confederation of Shawnee, Mingo, Delaware, and Wyandot warriors.

The Campaign and the Battle of Point Pleasant

The Virginian campaign relied on a strategic two-pronged advance:

• The Northern Division: Commanded by Lord Dunmore (~1,200 men), moving via Fort Pitt (renamed Fort Dunmore) down the Ohio River.
• The Southern Division: Commanded by Colonel Andrew Lewis (~1,100 men), rendezvoused at Camp Union (Lewisburg) and marched 160 miles through the Allegheny wilderness along the Kanawha River corridor to the confluence at Point Pleasant.

On October 10, 1774, Shawnee leader Chief Cornstalk executed a night crossing of the Ohio River to strike Lewis’s isolated southern wing before the colonial armies could combine. Cornstalk deployed a crescent-shaped line across the peninsula, using the timbered terrain and coordinated fire to contain the Virginians against the river junction.

After hours of intense engagement, a late-afternoon flanking maneuver along Crooked Creek by Virginia companies under Captains Isaac Shelby, George Matthews, and John Stuart led Native forces to execute a disciplined night withdrawal across the river. The resulting Treaty of Camp Charlotte secured colonial access south of the Ohio River and opened the Kentucky frontier to settlement.

                  [Lord Dunmore's Northern Column]
                        (Down the Ohio River)
                                  │
                                  ▼
[Chief Cornstalk's Force] ──► [POINT PLEASANT] ◄── [Andrew Lewis's Column]
 (Night River Crossing)      (Oct 10, 1774 Battle)     (From Camp Union/Lewisburg)

2. Frontier Fortifications of the Upper Greenbrier Valley

During Dunmore’s War and the American Revolution (1775–1783), the upper Greenbrier Valley (modern Pocahontas County) formed an exposed mountain frontier. Defense relied on an interconnected chain of stockades, blockhouses, and scout patrols.

                    ┌─────────────────────────┐
                    │     WARWICK'S FORT      │ (Near modern Green Bank/Dunmore)
                    │  (Capt. George Moffett) │
                    └────────────┬────────────┘
                                 │
                                 │ [Seneca Trail & Ranging Corridor]
                                 ▼
                    ┌─────────────────────────┐
                    │    CLOVER LICK FORT     │ (Upper Greenbrier River)
                    │     (Jacob Warwick)     │
                    └────────────┬────────────┘
                                 │
                                 │ [River & Ridge Trails]
                                 ▼
                    ┌─────────────────────────┐
                    │    DRENNAN'S FORT /     │ (Central Greenbrier Corridor)
                    │  MARLIN'S / DAY'S FORT  │
                    └─────────────────────────┘

Key Frontier Fortifications

• Warwick’s Fort (Fort Warwick): Erected in June 1774 on Deer Creek near present-day Green Bank and Dunmore on the property of William Warwick. Built by militia companies under Captains George Moffett and George Mathews, it measured approximately 140 by 100 feet with heavy oak stockades, internal cabins, and earth-insulated roofs. It served as a primary staging point for the 1774 Point Pleasant expedition and remained garrisoned through 1783.
• Fort Clover Lick: Established by pioneer cattleman and militia officer Jacob Warwick (c. 1747–1826) along the Greenbrier River. It served as a livestock depot, scouting outpost, and communication link along the Seneca Trail.
• Supporting Outposts: Included Thomas Drennan’s Fort (near Edray), Fort Greenbrier / Marlin's Station (Marlinton), and John Day’s / Cackley’s Fort (Mill Point / Little Levels).

3. The Industrial Transformation: Rail and Lumber

At the turn of the 20th century, the subsistence agriculture and cattle-grazing economy of Pocahontas County gave way to industrial-scale natural resource extraction, enabled by railway engineering.

[Western Maryland Railway] ── (Coal, Manufactured Goods, Empties) ──► ┌──────────────────┐
                                                                       │ DURBIN JUNCTION  │
[C&O Greenbrier Division]  ◄── (Lumber, Pulpwood, Bark, Leather)  ─── └──────────────────┘

The C&O Greenbrier Division (1899–1905)

Chartered as the Greenbrier Railway under the Chesapeake & Ohio Railway, this 101-mile branch extended north from Whitcomb (near Ronceverte) along the water-level grade of the Greenbrier River:

• Reached Marlinton in October 1900 and Cass in December 1900.
• Completed to Durbin in 1902 and Winterburn in 1905.
• Major engineering feats included the construction of Droop Mountain Tunnel and Sharps Tunnel (with its adjacent river bridge).

The Durbin Rail Interchange

At Durbin, the C&O connected directly with the Western Maryland Railway (Coal & Iron Railway branch from Elkins across Cheat Mountain). This junction functioned via a multi-track yard, turnaround runs ("The Durbin Turn"), and freight classification:

• Northbound/Eastbound Flow: Red spruce, hemlock, hardwood lumber, tanning bark, and finished leather from regional tanneries (Frank, Marlinton) were sent to northern markets and ports like Baltimore.
• Southbound/Westbound Flow: Bituminous coal, heavy industrial machinery, and empty rolling stock were routed into the Greenbrier Valley.

4. Timber Operations at Clover Lick

Clover Lick (historically Cloverlick), named for its natural saline spring and wild clover flats, evolved from Jacob Warwick's 18th-century grazing estate into an industrial logging center between 1900 and 1925.

Logging Company	Active Period	Primary Mill & Track Location	Operational Scope
DeRan Lumber Company	c. 1905–1911	Mill on Clover Creek (~1 mile above mouth)	Laid ~9 miles of logging rail west into Cheat/Clover Lick Mountain valleys.
F.S. Wise & Sons	c. 1910s	Mill near the mouth of Laurel Creek	Harvested tracts eastward toward Thomas and Sitlington creeks; direct C&O siding loading.
Harter Brothers Lumber Co.	c. 1903–1912	Located southwest of Clover Lick at Harter	Operated the Pocahontas Central Railroad using Shay geared steam engines on Clover Lick Mountain.
Raine Lumber Company	c. 1920s	Operations based on Thorny Mountain	Utilized 70-ton Shay locomotive power; cooperated in the 1924 state purchase creating Seneca State Forest.

5. Settlement Geography: Dunmore, Clover Lick, and Driftwood

The central Greenbrier River and its tributaries supported distinct settlements shaped by topography, transportation, and resource extraction:

[DUNMORE] ─────────────► Located on Deer Creek (Rt. 28 corridor). Named for Lord Dunmore 
                         during the 1774 frontier mobilization around Warwick's Fort.
   │
   │ (~10 Miles Southwest via River / Rail Grade)
   ▼
[CLOVER LICK] ─────────► Located at MP 71.3 on the Greenbrier River. Evolved from Jacob 
                         Warwick's 1770s fort and cattle farm into a major sawmill and C&O depot hub.
   │
   │ (~12 Miles Southwest Downstream)
   ▼
[DRIFTWOOD] ───────────► Located near Swago/Stony Creek bottoms below Marlinton. 
                         Named for river driftwood deposits; featured a school, post office, and C&O siding.

Driftwood Overview

• Name Origin: Derived from natural accumulations of river driftwood, flood flotsam, and runaway drive-logs caught along river gravel bars and eddies below Buckeye and Marlinton.
• Post Office: Operated as a fourth-class rural post office in the early 1900s to serve river-bottom farmsteads and timber workers before consolidation into Marlinton/Buckeye routes under Rural Free Delivery.
• Schoolhouse: A standard one-room district schoolhouse providing elementary education (grades 1–8) and community gathering space, later phased out during 20th-century school consolidation.
• C&O Siding: Served as a flag stop and loading spur for agricultural livestock, cross-ties, chemical pulpwood, and farm provisions.

6. Modern Conservation and Heritage Transition

As timber resources were exhausted by the late 1920s, the region transitioned toward reforestation and public land stewardship:

• Seneca State Forest (1924): West Virginia’s oldest state forest was established through the acquisition of over 10,000 acres of cutover timberland on Thorny Mountain from operations including Raine Lumber.
• Greenbrier River Trail State Park: Following the abandonment of the C&O Greenbrier Division in 1978–1979, the 78-mile rail corridor between North Caldwell and Cass was converted into a non-motorized recreational trail, preserving historic depots (such as Clover Lick), bridges, and tunnels.
• Heritage Tourism: The preserved rail infrastructure at Cass and the Durbin Rocket excursion line north of Durbin maintain operating examples of the geared steam locomotives (Shay and Climax) that drove the early-20th-century timber economy.

CPS

 

Noncompliance issues involving Child Protective Services (CPS) in Pocahontas County reflect systemic failures within the West Virginia Department of Human Services (DoHS, formerly DHHR), combined with local operational challenges in rural jurisdictions. These issues fall into three primary categories: statutory audit findings, workforce and capacity deficits, and judicial process breakdowns.

1. Statutory & Administrative Audit Findings

• Intake and Assessment Timeline Failures: A comprehensive audit by the U.S. Department of Health and Human Services Office of Inspector General (OIG) revealed that approximately 91% of reviewed child abuse and neglect cases statewide failed to meet one or more federal or state compliance mandates.
• Mandatory Notice Deficiencies: Caseworkers routinely failed to document or issue mandatory written outcome notifications to parents and alleged maltreaters within the required 15-day certified mail window under state policy.
• Delayed Response to Referrals: In rural districts, geographic distances and intake backlogs have led to noncompliance with mandatory statutory response times (which require initial contact within 24 to 72 hours depending on the triage priority level).

2. Staffing Shortages & Caseload Noncompliance

• Caseload Ceilings: High turnover and persistent vacancies at the local Marlinton office and surrounding regional hubs have forced remaining caseworkers to manage caseloads far exceeding recommended professional standards.
• Missed Monitoring Protocols: Excessive caseloads have resulted in missed monthly face-to-face visits with children placed in out-of-home or kinship care, violating the state's Safety Assessment and Management System (SAMS) protocols.
• Delayed Multidisciplinary Coordination: Under West Virginia Code, CPS is required to coordinate with local law enforcement and the Child Youth Advocacy Center (CYAC) via the local Multidisciplinary Investigative Team (MDIT). Staff shortages and remote geography in Pocahontas County have created recurring friction in maintaining rapid joint forensic interviews.

3. Circuit Court Orders & Legal Accountability

• Case Plan Delays: Under Rule 49 abuse and neglect procedures, CPS must submit individualized family case plans and progress reports prior to adjudicatory and dispositional hearings. Circuit court proceedings frequently face continuances due to late or incomplete agency filings.
• Placement & Service Delivery Deficits: Regional circuit judges have repeatedly scrutinized the agency for failing to timely secure court-ordered behavioral health treatment, specialized foster placements, or remedial services for families during statutory improvement periods.
• Qualified Immunity Litigation: Multiple civil actions challenging CPS response delays to repeated abuse/neglect reports have reached West Virginia appellate courts. While courts have largely shielded the agency under qualified immunity for discretionary duties, these cases highlighted repeated failures to follow internal administrative guidance.

Child Protective Services (CPS) in Pocahontas County evolved from early county-level poor relief and almshouse systems into a state-supervised, county-administered child welfare model. While local cases are investigated and managed through the local county office (located in Marlinton) and adjudicated in the Pocahontas County Circuit Court, the legal authority and administrative structure follow West Virginia’s broader statutory framework.

Early Relief & The Almshouse Era (1863–1918)

• County-Level Responsibility: When West Virginia was established in 1863, the legislature placed the legal and financial burden of destitute families and orphaned children directly onto individual counties.
• Overseers of the Poor: Child welfare was not yet a distinct professional practice. Dependent, neglected, or orphaned children were typically indentured, bound out as apprentices, or placed alongside adults in the Pocahontas County Poor Farm/almshouse.
• Mothers’ Pension Law (1915): The state enacted legislation permitting county courts to provide small monthly stipends to impoverished mothers, marking the first formal effort to keep vulnerable children in their own homes rather than sending them to institutions.

Formalization of Child Welfare (1919–1960s)

• Board of Children’s Guardians (1919): West Virginia created its first statewide body tasked specifically with supervising the care of dependent and neglected children.
• Public Welfare Law of 1936: In response to the Great Depression and the federal Social Security Act of 1935, West Virginia reorganized its welfare apparatus. The state established the Department of Public Assistance (DPA) and mandated local county departments of public assistance.
• Local Administration: Pocahontas County formed a local welfare board and dedicated staff in Marlinton, shifting child welfare from county commission charity to professional case management, foster home licensing, and child placement.

The Modern CPS Era & DHHR Consolidation (1970s–2000s)

• Mandatory Reporting & Title XX: During the 1970s, West Virginia passed mandatory child abuse and neglect reporting laws under Chapter 49 of the West Virginia Code, establishing the modern investigative mandate for Child Protective Services workers.
• Creation of the DHHR (1989): The West Virginia Department of Health and Department of Human Services merged into the Department of Health and Human Resources (DHHR). Child Protective Services was housed under the Bureau for Children and Families (BCF).
• Judicial Integration: Abuse and neglect proceedings became heavily formalized in local circuit courts. In Pocahontas County (part of the 11th Judicial Circuit, and later reformed judicial circuits), the local CPS unit worked closely with the Pocahontas County Prosecuting Attorney, Court Appointed Special Advocates (CASA), and circuit judges under Rule 49 abuse/neglect procedural rules.
• Family Resource Networks: In the 1990s and early 2000s, community-level prevention grew alongside state CPS, leading to the formation of the Pocahontas County Family Resource Network (FRN) in Marlinton to assist at-risk families with basic needs, parent education, and diaper/food security.

Recent Restructuring & Contemporary Operations (2010s–Present)

• The Opioid Epidemic Impact: Beginning in the 2010s, a steep rise in substance use disorders placed severe strain on rural CPS units across West Virginia, driving up the number of children removed from parental custody and placed in kinship care or foster care.
• Staffing & Caseload Pressures: Rural counties faced recurring challenges with CPS caseworker vacancies, retention, and extensive geographic coverage across mountainous terrain.
• 2024 DHHR Division: Effective January 1, 2024, the West Virginia Legislature dissolved the monolithic DHHR and split it into three separate cabinet-level agencies. Child Protective Services and child welfare administration were transferred to the Bureau for Social Services under the newly formed West Virginia Department of Human Services (DoHS).
• Current Footprint: Today, CPS operations in Pocahontas County run out of the DoHS District/County Office on 9th Street in Marlinton. Caseworkers operate through the state’s centralized Centralized Intake hotline for report triaging, follow the Safety Assessment and Management System (SAMS) protocols for family investigations, and coordinate with local law enforcement, school personnel, and community service providers.

‐---------

In West Virginia, county-level Multidisciplinary Investigative Teams (MDIT) are governed primarily by W. Va. Code § 49-4-402 (with complementary duties under § 49-4-504). Their statutory purpose is to coordinate the civil and criminal aspects of child abuse investigations, reduce systemic trauma to child victims through shared forensic procedures, and provide joint recommendations to the county prosecutor.

Statutory Leadership & Composition

By statute, the prosecuting attorney of each county is required to establish and direct the MDIT. Under W. Va. Code § 49-4-402(a), permanent members include:

 * The Prosecuting Attorney (or an assistant prosecutor designee).

 * A local Child Protective Services caseworker from the Department of Human Services (DoHS).

 * A local law enforcement officer representing an agency within the county (e.g., Sheriff's Department, West Virginia State Police, or municipal police).

 * A Child Advocacy Center (CAC) representative (where locally available or serving the jurisdiction).

 * A health care provider with pediatric and child abuse expertise (where available).

 * A mental health professional with pediatric and child abuse expertise (where available).

 * An educator (representing the local public school system).

 * A domestic violence program representative from a licensed program serving the county.

Agencies must submit written designations of their appointees to the prosecutor within 30 days of a request, and the prosecutor must formally notify the chief circuit judge within 15 days of appointment.

Mandatory Case Referrals & Scope

The MDIT is legally mandated to coordinate and review investigations involving:

 * Civil and Criminal Allegations: All cases involving child sexual assault, child sexual abuse, and severe child abuse and neglect.

 * Child Fatalities: All cases involving the accidental death of any child reported to a member agency, as well as any death of a child while in the legal or physical custody of the state.

Operational Protocols & Duties

 * Meeting Frequency: The team is statutorily required to meet at regular intervals, at least once every calendar month.

 * Joint Investigation & Forensic Coordination: The team coordinates interviews—typically utilizing the Child Advocacy Center’s recording and observation suites—to avoid multiple, repetitive interrogations of the child by CPS, deputies, and state troopers.

 * Prosecutorial Recommendation: Following case review, the MDIT makes formal recommendations to the prosecuting attorney regarding whether to file an emergency civil petition for child removal under Chapter 49, initiate criminal charges against the perpetrator, or pursue both concurrently.

Information Sharing & Confidentiality

 * Inter-Agency Disclosure: State, county, and local agencies are required by law to provide the MDIT with relevant records upon written request or pursuant to a circuit court order.

 * Confidentiality: All discussions, records, and evidence reviewed within MDIT meetings are strictly confidential under W. Va. Code Chapter 49, Article 5, shielding sensitive investigatory material from public disclosure while permitting necessary multi-agency exchange.

MDIT (Investigative) vs. MDTT (Treatment)

West Virginia law distinguishes the Investigative Team (MDIT, § 49-4-402) from the Multidisciplinary Treatment Team (MDTT, § 49-4-405). While the MDIT handles pre-petition and concurrent criminal/civil evidence gathering, the MDTT is convened within 30 days after a civil petition is filed in circuit court to manage parental improvement plans, foster placements, and family rehabilitative services.

Documented violations and systemic noncompliance by Child Protective Services (CPS) in Pocahontas County have surfaced through civil tort claims, federal audits, and state circuit court oversight.

1. Failure to Enforce Case Plans & Protect Wards

• Spradlin (Bennett) v. DHHR: In a notable legal action stemming from Pocahontas County Circuit Court child welfare proceedings, the state agency was sued for failing to enforce court-mandated safety restrictions. After emergency custody was granted due to abuse by a live-in partner, the agency prematurely returned physical custody to the mother while maintaining legal custody. Despite multiple reports that the known abuser remained in the home violating the Family Case Plan, the agency failed to intervene or remove the children, culminating in the fatal abuse of child Alisha Bennett.

2. Statutory Intake and Response Time Violations

• Mandatory Triage Deadlines: Federal OIG oversight reviews and state administrative reviews have repeatedly identified violations of statutory investigation timelines under W. Va. Code Chapter 49. In rural jurisdictions including Pocahontas County, high caseworker turnover and geographic distance have led to failures in meeting mandatory 24-hour, 72-hour, or 14-day initial face-to-face contact windows following Centralized Intake referrals.
• Failure to Provide Written Disposition Notices: Audits revealed systematic failures to issue mandatory written outcome notifications to parents and alleged perpetrators within the required 15-day certified mail timeframe following the conclusion of an investigation.

3. Family Case Plan & Circuit Court Procedural Lapses

• Delays in Rule 49 Filings: In abuse and neglect proceedings before the Pocahontas County Circuit Court, the agency has periodically faced scrutiny for failing to submit required individualized Family Case Plans and multidisciplinary reports within statutory deadlines prior to dispositional hearings.
• Reunification and Remedial Service Delays: Judicial reviews have highlighted instances where court-ordered supportive services (such as specialized substance use treatment, supervised visitation, and parenting education) were not timely mobilized during statutory improvement periods, delaying permanent placement or reunification efforts.

4. Monitoring and Caseload Breaches

• Missed Monthly Visits: Persistent vacancy rates at the local Marlinton office have caused caseloads to exceed recommended state thresholds. Consequently, caseworkers have missed mandatory monthly face-to-face health and safety visits for children placed in kinship or foster care settings, violating the state's Safety Assessment and Management System (SAMS) protocols.

Lithium at Dunmore

 

 

### Early Settlement and Frontier Context


The community of Dunmore in Pocahontas County is situated along Sitlington Creek in the Upper Greenbrier Valley, surrounded by the Allegheny Mountains. Long before formal settlement, natural mineral springs and salt licks across the region drew wildlife and served as vital points along indigenous travel paths, including branch routes connecting with the Seneca Trail.

During the late 18th century, frontier leaders such as Major Jacob Warwick and the Mathews family settled the area. During Lord Dunmore’s War (1774) and the American Revolution, local fortifications (often referred to as Fort Dunmore or Warwick's Fort) were established nearby to protect homesteaders along the frontier.

---

### The Mineral Springs & 19th-Century "Springs Culture"

Throughout the 19th century, western Virginia and the newly formed state of West Virginia experienced a boom in mineral spring tourism. While grand luxury resorts developed around prominent thermal and sulfur waters in the neighboring valleys (such as White Sulphur Springs, Warm Springs, and Hot Springs), Pocahontas County contained numerous smaller local mineral springs valued by residents and travelers:

* **Water Composition:** The springs around Dunmore and the surrounding valley are typical of the Allegheny karst and shale formations, featuring cool, clear waters with natural mineral profiles—primarily chalybeate (iron-bearing), magnesia, and mild sulfur properties—which 19th-century physicians and locals widely recommended as restorative tonics for digestion and overall vitality.
* **Community Life:** Unlike the commercialized plantation-era resorts, Dunmore Springs primarily functioned as a local health retreat and community resource. Farmsteads and early mills along Sitlington Creek made the area an active rural hub where neighbors gathered to fetch water and socialize.

---

### 20th Century: Recreation and Bottling

In the 20th century, the site evolved into a favored spot for community recreation:

* **Campground & Social Grounds:** Archival records and local photographs from the mid-20th century show Dunmore Springs as an active venue for family camping trailers, church picnics, reunions, and seasonal outdoor gatherings featuring picnic pavilions and shaded grounds.
* **Bottled Spring Water:** The purity and mineral balance of the natural mountain aquifers surrounding Dunmore later entered the bottled water market, earning honors at competitive events such as the Berkeley Springs International Water Tasting.

Today, while the era of historic mineral spa convalescence has transitioned into modern mountain tourism, Dunmore Springs remains a notable chapter in Pocahontas County’s rich regional folklore, early settlement heritage, and natural resource history.

An increase in the clinical adoption of microdose lithium (low-dose lithium carbonate or compounds like lithium orotate, typically under 5–30 mg elemental lithium) for neuroprotection and Alzheimer's disease holds specific clinical and logistical implications for rural communities like Dunmore in Pocahontas County.

Clinical & Pharmacological Context

Recent neurodegenerative research highlights low- and micro-dose lithium for its ability to:

• Inhibit Glycogen Synthase Kinase-3 (GSK-3β): Reduces hyperphosphorylation of tau proteins and slows amyloid-beta plaque aggregation.
  
  
• Evade Standard Plaque Binding: Novel microdose formulations help restore normal brain lithium levels without requiring high systemic concentrations.
  
  
• Bypass Psychiatric Toxicity Profiles: Standard bipolar regimens (900–1,200 mg/day) require frequent renal, thyroid, and serum monitoring; microdoses substantially reduce the risk of toxicity and organ strain in geriatric populations.
  
  

Local Impact on Dunmore & Upper Pocahontas County

+------------------------------------+---------------------------------------------------+
| Domain                             | Local Impact in Dunmore                           |
+------------------------------------+---------------------------------------------------+
| Caregiver & Home Support           | Prolongs independent living; delays nursing home  |
|                                    | placement out of the Deer Creek / Route 28 valley |
+------------------------------------+---------------------------------------------------+
| Rural Healthcare Logistics         | Lowers need for weekly lab visits in Marlinton    |
|                                    | or Elkins due to wider therapeutic margins        |
+------------------------------------+---------------------------------------------------+
| Community Age Density              | Directly serves Pocahontas County's above-average |
|                                    | proportion of senior residents                    |
+------------------------------------+---------------------------------------------------+

• Mitigating Geographic Isolation: Dunmore residents face a 25–30 mile round trip down Route 28 to Pocahontas Memorial Hospital or Pocahontas Center in Marlinton, and even further to regional neurology hubs in Elkins or Lewisburg. Treatments requiring minimal therapeutic drug monitoring (TDM) eliminate recurring winter travel hazards.
  
  
• Preserving Family-Based Care Systems: In tight-knit rural settlements, slowing the transition from Mild Cognitive Impairment (MCI) to advanced dementia keeps aging residents in multi-generational family homes rather than requiring out-of-area memory care units in Randolph or Greenbrier counties.
  
  
• Primary Care Prescribing Feasibility: Because microdosing carries a broader safety margin than traditional mood-stabilizer lithium regimens, local primary care physicians and rural health clinics (such as those in Green Bank or Marlinton) can manage protocols without constant subspecialist titration.
  
  

Key Hurdles to Implementation

1. Standardization & Insurance Coverage: Microdose regimens and over-the-counter supplements lack the standardized FDA-approved dosing pathways of monoclonal antibodies, creating reimbursement barriers for fixed-income seniors on Medicare.
   
   
2. Clinical Trial Translation: While animal models and pilot human trials show preservation of verbal memory and reduced atrophy, large-scale Phase III biomarker-guided trials are still determining exact target dosage thresholds for clinical efficacy.

Naturally occurring trace lithium ($Li$) in drinking water has emerged as a major focus in environmental neurobiology and Alzheimer’s disease (AD) prevention.

Integrating trace lithium into the analysis of Dunmore, West Virginia connects local groundwater geology directly with these emerging clinical findings.

1. The Science: Micro-Dose Lithium & Alzheimer's Pathology

Recent epidemiological and preclinical studies—including landmark findings from Harvard, JAMA Psychiatry, and Nature—show that lifelong exposure to micro-dose lithium in tap water (measured in micrograms per liter, $\mu\text{g/L}$) is associated with lower rates of dementia and Alzheimer's mortality:

• Inhibition of GSK-3$\beta$: Lithium directly inhibits Glycogen Synthase Kinase-3 beta ($GSK\text{-}3\beta$). In Alzheimer's pathology, hyperactive $GSK\text{-}3\beta$ drives the formation of neurofibrillary tau tangles and promotes amyloid-beta ($\text{A}\beta$) plaque deposition.
  
  
• Autophagy & Brain Waste Clearance: Micro-doses of lithium stimulate cellular autophagy, helping neurons break down misfolded proteins before they aggregate into neurotoxic plaques.
  
  
• Reversal of Deficiencies: Recent 2025–2026 neurochemical studies revealed that post-mortem brain samples from patients with mild cognitive impairment (MCI) and AD show significant lithium depletion compared to healthy controls, suggesting environmental trace intake may act as a baseline nutritional neuroprotectant.
  
  

2. Local Groundwater Dynamics in Dunmore

According to nationwide groundwater modeling by the U.S. Geological Survey (USGS) and EPA UCMR monitoring:

• Baseline Regional Concentrations: Across West Virginia, modeled drinking water lithium levels average $\sim 3.1\ \mu\text{g/L}$, which is below the national population-weighted average ($\sim 5.7\ \mu\text{g/L}$) and the EPA Health-Based Screening Level ($10\ \mu\text{g/L}$).
  
  
• Aquifer Variation in Pocahontas County:
  
  
  • Shallow karst limestone springs and sandstone aquifers (common in rural Pocahontas valleys like Dunmore) generally yield low natural lithium concentrations ($<4\ \mu\text{g/L}$).
    
    
  • Deeper bedrock wells or water contacting mineralized Devonian shale formations can contain elevated trace lithium levels, though private wells in Dunmore are rarely deep enough to tap these high-mineral brine layers.
    
    
• Filtration Stripping: Residents in Dunmore who install whole-house Reverse Osmosis (RO) systems to remove contaminants (like lead, bacteria, or excess hardness) also unintentionally strip out beneficial trace ions—including lithium, magnesium, and calcium.
  
  

3. Testing for Lithium in Dunmore Private Wells

Because lithium is not regulated under the National Primary Drinking Water Regulations, standard local health department test panels do not include it.

Parameter	Standard Well Test	Targeted Environmental / Trace Panel
Analytes Covered	Bacteria, Nitrates, Lead, Copper, Iron	Lithium ($Li$), Manganese ($Mn$), Arsenic ($As$), Strontium ($Sr$)
Laboratory Method	Wet Chemistry / EPA 200.8 basic	ICP-MS (Inductively Coupled Plasma Mass Spectrometry)
Detection Limit Needed	$1\text{–}10\ \text{mg/L}$	$0.1\text{–}1.0\ \mu\text{g/L}$ (parts per billion)
Availability	Local Health Dept. / State Lab	Certified Commercial Labs (e.g., Pace Analytical, Eurofins)

If you are testing well water in Dunmore to measure both neuroprotective minerals (like lithium and magnesium) and potential neurotoxic metals (like manganese and lead), request a Total Metals by ICP-MS (EPA Method 200.8) scan from a certified laboratory.

HYPOTHETICAL

 

It begins not with a corporate breakthrough, but with an anomaly in an epidemiological spreadsheet. A public health researcher cross-referencing regional health metrics notices that Dunmore consistently reports the lowest rates of mood disorders, violent crime, and road rage in the entire commonwealth. When standard explanations like socioeconomic factors, demographics, and healthcare access fail to account for the disparity, a team of environmental geochemists tests the municipal groundwater.

They discover that Dunmore’s aquifer filters through a rare subterranean mineral seam rich in spodumene and lepidolite, naturally infusing the municipal tap with stable, sub-therapeutic micro-doses of lithium—roughly 80 micrograms per liter. It is far below pharmaceutical levels, but consistently present in every cup of morning coffee, every shower, and every garden hose in town.

The inflection point arrives when the findings leak to the national press under headlines dubbing Dunmore "The Zen Oasis." Within weeks, the quiet borough becomes the epicenter of a cultural phenomenon. Tech entrepreneurs, wellness influencers, and biohackers descend on the town, booking out every motel along the highway. Coffee shops in the downtown square begin branding their cold brews as "Hydro-Balanced," drawing long lines of remote workers eager to test if the local tap water actually sharpens focus and soothes burnout.

By the following year, the economic landscape transforms entirely. Rather than bottling and shipping its resource out, the borough council passes strict conservation ordinances to protect the watershed, inadvertently turning Dunmore into a premier wellness tourism and research destination. Major universities establish longevity clinics along Drinker Street to study long-term neuroprotection, while upscale restorative spas open in renovated industrial brick buildings.

Dunmore, once known primarily for its quiet coal-country heritage, cements its place as the world’s first "micro-mineral capital"—a living case study in how geology shapes human temperament and a haven for those seeking calm straight from the tap.