Leighton Photography & Imaging

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  • Ancient basalt columns are a typical sight in Central Washington. They are formed by cooling lava, forming cracks that create these columns by contracting. The faster the lava cools, the thinner the columns. These thick columns cooled gradually over some time. The presence of the lichens that now cover the stony face is an indicator of very good air quality and a lack of pollution.
    Lichen-Covered Basalt Cliff in Cowic..nyon
  • This rock was once molten lava forced from deep within the earth as it covered most of Central Washington, up to three miles deep in some places. Many thousands of years of erosion, weathering and exposure to the elements has left us with massive crumbling rock formations like this basalt rock wall.
    Rocky Basalt Bluffs of Cowiche Canyon
  • The eastern part of the Cascades mountains in Washington state couldn't be more different from the western side. Instead of wet, green and cloudy slopes, there are dry, columnar igneous rock structures, desert scrub plants and big skies!
    Basalt Cliffs at White Pass
  • Eastern Washington's iconic Palouse Falls is a 198-foot waterfall on the Palouse River which empties into the Snake River. These ancient basalt cliffs were created by lava and ground down by massive glaciers.
    Palouse Falls
  • Eastern Washington's iconic Palouse Falls is a 198-foot waterfall on the Palouse River which empties into the Snake River. These ancient basalt cliffs were created by lava and ground down by massive glaciers.
    Palouse Falls
  • Eastern Washington's iconic Palouse Falls is a 198-foot waterfall on the Palouse River which empties into the Snake River. These ancient basalt cliffs were created by lava and ground down by massive glaciers.
    Palouse Falls
  • Eastern Washington's iconic Palouse Falls is a 198-foot waterfall on the Palouse River which empties into the Snake River. These ancient basalt cliffs were created by lava and ground down by massive glaciers.
    Palouse Falls
  • This wildly colorful community of mixed lichen and an (as yet) unidentified moss covered the basalt cliffs in rural Central Washington north of Ephrata in the middle of January.
    Lichen and Moss Community
  • Eastern Washington's iconic Palouse Falls is a 198-foot waterfall on the Palouse River which empties into the Snake River. These ancient basalt cliffs were created by lava and ground down by massive glaciers.
    Palouse Falls
  • Eastern Washington's iconic Palouse Falls is a 198-foot waterfall on the Palouse River which empties into the Snake River. These ancient basalt cliffs were created by lava and ground down by massive glaciers.
    Palouse Falls
  • The Palouse River is a somewhat short river in southeastern Washington that joins the Snake River, which in turn joins the mighty Columbia River that forms the border between Washington and Oregon. It is best known for it's magnificent waterfall - Palouse Falls.
    Palouse River
  • The Palouse River is a somewhat short river in southeastern Washington that joins the Snake River, which in turn joins the mighty Columbia River that forms the border between Washington and Oregon. It is best known for it's magnificent waterfall - Palouse Falls.
    Palouse River
  • Sunset is almost always a dramatic show of light and shadow, as witnessed here in Cowiche Canyon, just west of Yakima, WA. Strong beams of sunlight beautifully backlit these desert wildflowers (Carey's balsamroot).
    Sunset in the Sagebrush Desert
  • The Palouse River is a somewhat short river in southeastern Washington that joins the Snake River, which in turn joins the mighty Columbia River that forms the border between Washington and Oregon. It is best known for it's magnificent waterfall - Palouse Falls.
    Palouse River
  • Not too long ago I was traveling across Oregon Coast on a nature photography trip with an old friend and one of the places he wanted to check out was Thor's Well, located about midway down the state's incredible coastline at a place called Cape Perpetua. <br />
<br />
Formed out of natural volcanic rock (basalt), this wild geologic anomaly was probably formed by a cave beaten into the cliff that eventually collapsed forming this unusual seeming deep hole in the ground but is actually open underwater to the surf. This causes water to explode violently upward through the "well", followed by the foamy water to duck back down into the depths of the earth.<br />
<br />
It was utterly fascinating, even if I did get hit and completely soaked by one of the infamous rogue waves of the Pacific Ocean.
    Thor's Well
  • Typically high-strung and aggressive, this large northern scorpion (Paruroctonus boreus) is perhaps the biggest I've ever seen at just over 4cm in length and the only one that ever let me touch it without trying to sting me. I found this one near Lake Lenore at the base of some basalt cliffs under a rock in rural Grant County, Central Washington.
    Northern Scorpion (Paruroctonus boreus)
  • This beautiful teal-green bullseye lichen was found growing in the Oak Creek Wildlife Recreation Area just west of Yakima, Washington. If you look closely, you can see the small fleshy fruiting bodies in the center of each lichen that will eventually release its spores to propagate the next generation. This region of the Pacific Northwest is very dry and rocky, and most of the basalt surfaces are covered in multiple types of lichen.
    Bullseye Lichen
  • These exceptionally fast fliers feed on insects that they catch in flight, and can often be seen at dawn or dusk in great numbers performing incredible aerobatics in huge numbers over ponds, lakes, and open areas where there are lots of flying insects. This was one of a pair that were circling me as I wound my way up a risky trail up a steep basalt cliff just south of Naches, Washington.
    Violet-Green Swallow
  • Occasionally heard in remote canyons and rocky cliffs, but seldom seen, this curious canyon wren stayed with me for some time as I wound my way up a narrow trail up the steep basalt cliffs of White Pass near Naches, Washington.
    Canyon Wren
  • First light peeks over the steep basalt canyon walls to touch the Yakima River in the incredibly picturesque Yakima Canyon at dawn. With this chilly springtime morning, the sounds of bats, frogs and coyotes fade, only to be replaced by early-rising songbirds, blue herons and the splashing of hungry rainbow trout.
    Wild Grasses in the Yakima River Can..Dawn
  • Rolling arid hills and miles upon miles of aromatic sagebrush, crumbled basalt rocks and heat in this desert-like landscape in Central Washington near Vantage, WA.
    Sagebrush Country
  • Ancient monolithic sentinels of basalt and time, these wondrous sea stacks were photographed near the Pistol River on Oregon's southern coastline.
    Sea Stacks on the Oregon Coast
  • This small daisy is found at lower elevations in the drier, rocky parts of Central and Eastern Washington and Oregon. It is closely related to other similar aster species found in the same region but at higher elevations. This one was found with many others growing from a crack in a basalt canyon rock wall outside of Naches, Washington just west of Yakima.
    Dwarf Golden Daisy
  • Volcanic basalt cliffs, steep slopes and sagebrush steppe pretty much define Central Washington's White Pass. Springtime turns the typical brown desert landscape into a green paradise attracting a plethora of wildlife to the region.
    White Pass in Central Washington 2
  • An invasive, yet beautiful non-native yellow flag iris catches the first rays of sunlight over the basalt walls of Yakima Canyon on the Yakima River at dawn.
    Yellow Flag Iris
  • One of "The Needles" - one of three tall basalt spires of volcanic rock near the massive Haystack Rock on Oregon's coast on Cannon Beach. Around about 15 to 16 million years old, these columns are very slowly eroding with every wave and every changing tide.
    The Needles of Cannon Beach
  • Oregon's North Falls as viewed from within the huge cavern carved out behind the waterfall over many thousands of years. This huge waterfall and a very memorable part of North Silver Creek was formed from 15-16 million-year-old volcanic bedrock (basalt) which has been withstanding the millions of years of water and weather erosion while the surrounding sandstone (once part of the Oregon coastline) which is very slowly wearing away. As it stands now, the waterfall drops 136 and continues downstream through a series of other spectacular waterfalls. The huge cavern behind the falls reaches back about 100 feet, has a ceiling that ranges from 20 to 75 feet high and is (in my estimation) about 800-900 feet wide. Very impressive, to say the least!
    Looking Out from Behind the Waterfall
  • Brightly colored, yet perfectly camouflaged, the somewhat rare canyon wren blends in perfectly with the lichen encrusted basalt cliffs of White Pass, above the Tieton River.
    Canyon Wren
  • One of "The Needles" - one of three tall basalt spires of volcanic rock near the massive Haystack Rock on Oregon's coast on Cannon Beach. Around about 15 to 16 million years old, these columns are very slowly eroding with every wave and every changing tide.
    The Needles at Sunset
  • Cerro Castellan - also known as Castolon Peak or Castellan Peak, is a conical volcanic mountain in West Texas that rises 1000 feet above the desert floor (3,293 feet above sea level) in Big Bend National Park. Cerro Castellan itself is part of an ancient series of summits once known as the Corazones Peaks that has since succumbed to millennia of erosion by wind, precipitation, searing heat and bitterly cold winters. <br />
Geologically, this ancient mountain range remnant is a high stack of volcanic rocks, including ash, lava, and tuffaceous rocks. It is capped by a dense lava flow underlain by various tuffs and basalts. A somewhat northwest fault cuts the eastern face of Cerro Castellan. Although little vegetation grows on the sheer cliffs and steep, pointed profile of its peak, the lower slopes of Cerro Castellan support a sparse growth of Chihuahuan Desert scrub, including most prominently such characteristic species as creosote bush and ocotillo.
    Cerro Castellan
  • Cerro Castellan - also known as Castolon Peak or Castellan Peak, is a conical volcanic mountain in West Texas that rises 1000 feet above the desert floor (3,293 feet above sea level) in Big Bend National Park. Cerro Castellan itself is part of an ancient series of summits once known as the Corazones Peaks that has since succumbed to millennia of erosion by wind, precipitation, searing heat and bitterly cold winters. <br />
Geologically, this ancient mountain range remnant is a high stack of volcanic rocks, including ash, lava, and tuffaceous rocks. It is capped by a dense lava flow underlain by various tuffs and basalts. A somewhat northwest fault cuts the eastern face of Cerro Castellan. Although little vegetation grows on the sheer cliffs and steep, pointed profile of its peak, the lower slopes of Cerro Castellan support a sparse growth of Chihuahuan Desert scrub, including most prominently such characteristic species as creosote bush and ocotillo.
    Cerro Castellan
  • Cerro Castellan - also known as Castolon Peak or Castellan Peak, is a conical volcanic mountain in West Texas that rises 1000 feet above the desert floor (3,293 feet above sea level) in Big Bend National Park. Cerro Castellan itself is part of an ancient series of summits once known as the Corazones Peaks that has since succumbed to millennia of erosion by wind, precipitation, searing heat and bitterly cold winters. <br />
Geologically, this ancient mountain range remnant is a high stack of volcanic rocks, including ash, lava, and tuffaceous rocks. It is capped by a dense lava flow underlain by various tuffs and basalts. A somewhat northwest fault cuts the eastern face of Cerro Castellan. Although little vegetation grows on the sheer cliffs and steep, pointed profile of its peak, the lower slopes of Cerro Castellan support a sparse growth of Chihuahuan Desert scrub, including most prominently such characteristic species as creosote bush and ocotillo.
    Cerro Castellan
  • Cerro Castellan - also known as Castolon Peak or Castellan Peak, is a conical volcanic mountain in West Texas that rises 1000 feet above the desert floor (3,293 feet above sea level) in Big Bend National Park. Cerro Castellan itself is part of an ancient series of summits once known as the Corazones Peaks that has since succumbed to millennia of erosion by wind, precipitation, searing heat and bitterly cold winters. <br />
Geologically, this ancient mountain range remnant is a high stack of volcanic rocks, including ash, lava, and tuffaceous rocks. It is capped by a dense lava flow underlain by various tuffs and basalts. A somewhat northwest fault cuts the eastern face of Cerro Castellan. Although little vegetation grows on the sheer cliffs and steep, pointed profile of its peak, the lower slopes of Cerro Castellan support a sparse growth of Chihuahuan Desert scrub, including most prominently such characteristic species as creosote bush and ocotillo.
    Cerro Castellan