Skip to Content

Darryl Mishler Photography

Underwater Photography

Texas State Parks

Landscape Photography

Wildlife Photography

Bird Photography

Macro Photography

Terms of Service

Darryl Mishler Photography

Underwater Photography

Texas State Parks

Landscape Photography

Wildlife Photography

Bird Photography

Macro Photography

Terms of Service

Folder: Galleries

Underwater Photography

Texas State Parks

Landscape Photography

Wildlife Photography

Bird Photography

Macro Photography

Terms of Service

Some of my favorite Prints › Sunset Over The Falls

Image 1 of 1

Sunset Over The Falls

$24.99

Beautiful sunset over Pedernales Falls

Beautiful sunset over Pedernales Falls

Caprock Canyon State Park

Caprock Canyons State Park highlights millions of years of powerful erosion where the flat, high plains of the Llano Estacado drop into the Rolling Plains of West Texas. Water from the tributaries of the Little Red River has relentlessly downcut through the land, slicing up to 1,000 feet deep to expose ancient layers of Earth's past. This geologic sculpting has forged a ruggedly magnificent, multi-hued landscape defined by soaring, wind-carved bluffs, steep arroyos, and jagged sandstone fins. Brilliant, alternating horizontal bands of fiery orange-red clay, deep lavender mudstone, and contrasting stark-white mineral veins stretch out under the vast Texas sky. This breathtaking, raw geology creates an unforgettable visual masterpiece of color and texture.

The canyon walls reveal beautifully stratified rock layers that tell a story of ancient seas, prehistoric rivers, and shifting climates. At the canyon floor sits the Permian-aged Quartermaster Formation, an intense layer of 250-to-280-million-year-old "red beds" composed of red shale and siltstone. This formation is famously marbled with shimmering white veins of gypsum deposited by long-evaporated tidal flats. Directly overlying the Quartermaster are the softer mudstones and sandstones of the Triassic-aged Tecovas and Trujillo Formations, which show off stunning variations of yellow, gray, and lavender while holding the prehistoric secrets of armored phytosaurs and petrified wood. Capping the entire escarpment at the very rim is the lighter-colored Ogallala Formation, a massive layer of sand and gravel tightly cemented by a hard layer of white caliche that acts as a protective shield against rapid erosion.

The park's dramatic, varied microhabitats support a thriveable ecosystem rich in unique desert and prairie wildlife. Most famously, Caprock Canyons is the home of the official Texas State Bison Herd, direct descendants of the historic southern plains herd originally saved by legendary cattleman Charles Goodnight. Mule deer, agile Barbary sheep, and pronghorn antelope traverse the steep slopes, while coyotes, bobcats, grey foxes, and burrowing owls navigate the canyon floor. Birdwatchers flock to the park to see around 175 bird species, including the cascading echo of the Canyon Wren along the rock faces, the Greater Roadrunner, and soaring golden eagles. During the nesting seasons, vibrant Painted and Indigo Buntings add brilliant color to the cottonwood-lined creek beds. Meanwhile, the historic Clarity Tunnel along the trailway plays host to over half a million migratory Mexican free-tailed bats every summer.

Guadalupe River State Park

Guadalupe River State Park, located in the heart of the Texas Hill Country, features a diverse landscape shaped by its distinct geology, wildlife, and flora. The park's geologic foundation is defined by the Edwards Plateau, featuring prominent Cretaceous limestone bluffs carved out over millennia by the erosive power of the Guadalupe River. This porous karst landscape also includes underground networks tied to the local Trinity Aquifer. Along the water's edge, the flora is dominated by massive, ancient bald cypress trees, alongside sycamores, pecans, and cedar elms. Moving away from the river into the arid uplands, the plant life transitions into a mix of Ashe juniper, live oak woodlands, and native grasslands. This varied ecosystem supports a rich array of wildlife. Mammals like white-tailed deer, armadillos, raccoons, and gray foxes roam the terrain, while the park’s old-growth juniper stands serve as a critical nesting habitat for the endangered golden-cheeked warbler.

South Llano River State Park

South Llano River State Park sits on the southwestern edge of the Texas Hill Country, showcasing a transition from rugged upland backcountry to a lush river basin. The geological foundation of the park features characteristic Edwards Plateau limestone bluffs carved out by the spring-fed South Llano River, which has famously never run dry in recorded history. Moving from the water to the higher elevations, the flora transitions from dense, shaded bottomland groves dominated by pecan trees, chinquapin oaks, and massive cedar elms into more arid, scrubby uplands filled with Ashe juniper, Texas persimmon, and Spanish dagger. This diverse habitat supports an array of wildlife, most notably serving as one of the oldest and largest winter roosting sites for Rio Grande wild turkeys in central Texas. Beyond the turkeys, the park is home to over 250 bird species—including the endangered golden-cheeked warbler—as well as white-tailed deer, axis deer, gray foxes, and armadillos, while the clear river waters support the native Guadalupe bass.

The park is recognized as one of the premier birding destinations in Texas, largely due to its unique position where multiple ecological zones overlap. This crossroads creates a rich habitat that attracts over 250 species of birds throughout the year, including sought-after species like the painted bunting, vermilion flycatcher, and the endangered golden-cheeked warbler. To accommodate the massive influx of birders, the park features several specialized, hidden viewing blinds equipped with water features that allow for up-close observations and photography of both resident and migratory species.

Choke Canyon State Park

Choke Canyon State Park is situated in the brush country of South Texas, surrounding the shoreline of the Choke Canyon Reservoir. The local geology consists of relatively flat, low-lying plains composed of sedimentary layers like sandstone and shale, which were flooded to create the massive water basin. The arid flora is dominated by dense thornscrub ecosystems, featuring mesquite trees, acacia, prickly pear cactus, and low-growing spiny shrubs, though areas near the water provide pockets of green ash and willow trees. This rugged habitat supports a unique mix of wildlife, famously including a large population of American alligators along the shores and in the shallows. Visitors will also encounter mammals like javelinas, white-tailed deer, and coyotes, while the park serves as a renowned birding destination for observing species like the crested caracara, green jay, and various migratory waterfowl.

The Choke Canyon Reservoir is primarily formed by the damming of the Frio River, but it sits within a unique watershed where three distinct rivers converge nearby. Just a few miles downstream from the reservoir, near the appropriately named town of Three Rivers, the Atascosa River flows into the Frio River, which then merges with the Nueces River. Additionally, San Miguel Creek feeds directly into the reservoir itself from the west, making the entire area a major hydrological hub for the South Texas brush country.

Kickapoo Caverns State Park

Kickapoo Caverns State Park is located on the western edge of the Edwards Plateau near the Chihuahuan Desert, presenting a dramatically rugged landscape shaped by its underground features. The geology is defined by massive Cretaceous limestone deposits, which water has hollowed out over millions of years to form thousands of caves, including Kickapoo Cavern and Stuart Bat Cave. The flora reflects a harsh, arid environment where desert scrub meets Hill Country woodlands, showcasing agarita, Texas persimmon, sotol, lechuguilla, and unique stands of pinyon pine and wild black cherry trees. This unique intersection of habitats supports a vibrant wildlife population, most notably the millions of Mexican free-tailed bats that roost inside Stuart Bat Cave from spring through autumn. The park is also home to gray foxes, ringtails, white-tailed deer, and a variety of rare birds, including the black-capped vireo and gray vireo.

Garner State Park

Garner State Park is located in the deeply carved canyonlands of the western Edwards Plateau, boasting some of the most dramatic terrain in the Texas Hill Country. The geology is characterized by high, steep limestone cliffs and bluffs, including the iconic Old Baldy summit, which were carved out by the crystalline, spring-fed waters of the Frio River. The flora is lush and diverse, featuring giant bald cypress trees lining the riverbanks, while the surrounding hills and canyons are covered in Ashe juniper, Texas madrone, lacey oak, and mountain laurel. This rich habitat supports abundant wildlife, making it a haven for white-tailed deer, axis deer, Rio Grande wild turkeys, and rock squirrels. The park's old-growth woodlands also provide critical seasonal nesting grounds for the endangered golden-cheeked warbler and black-capped vireo, while the clear river waters are home to a variety of native fish species.

Inks Lake State Park

Inks Lake State Park is a highly regarded birding destination in the Texas Hill Country, situated within a unique geological transition zone that attracts a wide variety of bird species. The park's combination of permanent water, dense woodlands, and rocky granite outcrops provides a rich habitat for over 180 species of birds throughout the year. Visitors can spot resident Hill Country species like the blue-gray gnatcatcher, black-crested titmouse, and Carolina wren, alongside seasonal visitors like the painted bunting and multiple species of migratory waterfowl. The park accommodates bird enthusiasts with excellent viewing opportunities along its trail system, especially near the shoreline and surrounding woodlands where diverse avian species forage and nest.

Pedernales Falls State Park

Pedernales Falls State Park features a dramatic landscape shaped by millions of years of shifting seas and river erosion. The foundation of the park is composed of tilted, layered stair steps of dark gray Marble Falls limestone that formed in an ancient saltwater ocean roughly 300 million years ago during the Pennsylvanian period. Tectonic forces from the Llano Uplift later deformed and tilted these layers, which were subsequently covered by younger Cretaceous marine deposits, sands, and gravels about 100 to 120 million years ago. The paleontology of the park is preserved within these distinct layers, where sharp-eyed visitors can spot 300-million-year-old crinoid stem fossils embedded as small white discs in the dense gray riverbed limestone, alongside younger marine fossils and shells trapped in the upper bluffs.

This ancient bedrock now supports a rich diversity of Texas Hill Country wildlife. Terrestrial mammals like white-tailed deer, Mexican long-nosed armadillos, coyotes, and raccoons roam the oak and juniper woodlands, while the clear waters of the Pedernales River support catfish, bass, and sunfish. Additionally, the park serves as a vital habitat for more than 150 bird species, including permanent residents like roadrunners and wild turkeys, as well as the endangered golden-cheeked warbler which nests in the canyon-lined forests each spring.

Sunset Over The Falls

Fire In The Sky

White-tailed Deer in Wildflowers