2024 GSA Calendars

I’m excited to announce that one of my photos was chosen for the cover of the Geological Society of America’s annual calendar! The image is of a blue meltwater pool on the west slopes of Mt. Rainier that I took a few years back. Here’s what it looks like on the calendar:

I had a photo of Sunset Arch in Grand Staircase-Escalante National Monument chosen for the inside of the calendar a few years back, but this is my first time on the cover. I received some sample copies of the calendar yesterday and the images are top-notch throughout.
You can order a copy of the calendar here for the low, low price of just $9.95! (It’s possible the price may be higher if you are not a member of GSA, I’m not positive…)
Merry Christmas and Happy New Year!
From A(storia) to B(rookings) Down the Oregon Coast
As another summer comes to a close, I am enjoying looking back at some photos from the past few months. In mid-August we had the chance to spend two weeks in Oregon, most of which we spent along the spectacular Oregon Coast. While not my first trip to the coast, this was my first time visiting some of the more remote southern sections of the coast, and over the course of the two weeks we were actually able to drive the entire Oregon section of Highway 101, all the way from Washington to California.
We began the trip in Astoria, gazing at the mouth of the Columbia River in Fort Stevens State Park and visiting the site of Fort Clatsop, quarters for the Lewis & Clark Expedition during the winter of 1805-1806. From there we travelled south to visit with friends in Rockaway Beach for several nights before continuing on to Newport and then heading inland for other adventures. A few days later we returned to the coast at the mouth of the Rogue River in Gold Beach, just 45 minutes or so north of the California border. After a quick drive into the Golden State, we began moving north, through Coos Bay, Bandon, Florence, and the Oregon Dunes before returning to Newport. After a final few days in the Lincoln City area, it was back up the Columbia River Gorge to Washington and back to work! Here are some of my favorite images from the trip, arranged from north to south:

Late afternoon light on the beach in Rockaway Beach, Oregon. The northern third of the Oregon Coast is characterized by long stretches of wide, sandy beach. Sand is relatively abundant here thanks to the Columbia River, though the supply has been greatly diminished since dams started popping up on the Columbia beginning in the mid 1900s.

I had been hoping to do some night sky photography from the beach, but despite relatively benign daytime weather, most nights looked something like this, with dense mist and fog enveloping the shore. Here, lights from Rockaway Beach illuminate the fog.

Sunset from Rockaway Beach, Oregon.

Sunset from Rockaway Beach, Oregon.

Brown pelican (Pelecanus occidentalis) and Pacific harbor seals (Phoca vitulina) on Salishan Spit near Lincoln City, Oregon.

Thor’s Well is an interesting feature within the Cape Perpetua Scenic Area near Yachats. A ~10 foot wide hole in the rocky coastline, the Well connects to the open ocean via a small cave. The well alternately drains and fills as the waves roll in and out. Watching the water roll into the Well and waves crashing against the rocks was a mesmerizing experience.

Scattered bogs along the Oregon Coast host rare patches of Darlingtonia californica, the California Pitcher Plant. One of the few species of carnivorous plants native to the Pacific Northwest, the translucent patches on the leaves supposedly confuse insects trying to escape from inside the plants.

Darlingtonia californica

What at first glance appear to be rocks sticking up out of the water are actually the remains of a massive tree stump in Sunset Bay near North Bend. Large concentrations of dead trees, often partially buried in sand, are found all up and down the Oregon Coast, and are often referred to as “Ghost Forests”. Some of these trees, particularly the ones found in coastal estuaries, appear to have been killed by rapid subsidence associated with large earthquakes along the Cascadia Subduction Zone just offshore. Analysis and dating of these trees have revealed that large “megathrust” earthquakes are a regular occurrence in the Pacific Northwest. In the case of the trees seen here in Sunset Bay, it appears to be unclear if earthquakes or more run-of-the-mill processes (such as coastal erosion) are the culprit.

These tilted rocks at Shore Acres State Park near North Bend have appeared in many a geology textbook! Shore Acres is home to one of the world’s most striking examples of what geologists call an “angular unconformity,” where flat-lying sedimentary rocks (visible in upper left) rest directly on top of older, tilted sedimentary rocks. The boundary between the flat rocks and the tilted rocks represents a large chunk of geologic time missing from the rock record. Several hundred years ago, geologists recognized angular unconformities as some of the first strong evidence of the Earth’s immense age, as they require multiple cycles of sediment deposition, burial, uplift, and erosion in order to form.

Sea lions and seals hauled out on Shell Rock near Simpson Reef. Interpretive signs at this overlook proclaimed that this is the largest haul-out site for sea lions on the Oregon Coast.

Coastal sand dunes mirror the clouds at Myers Creek Beach south of Gold Beach, Oregon

Sunset at Arch Rock, between Brookings and Gold Beach, Oregon

A closer view of Arch Rock.

The first quarter moon hovers over sea stacks along the Oregon Coast south of Gold Beach, Oregon.

A late afternoon view of Lone Rock Beach and Twin Rocks from the Cape Ferrelo Viewpoint near Brookings, Oregon.
Another Hidden Utah Gem: Pine Park

Panorama overlooking Pine Park at sunset.
Tucked away at the terminus of a winding gravel road in the Dixie National Forest near the Utah/Nevada border, Pine Park would probably be a beloved national monument or state park were it located literally anywhere other than Southern Utah. We’ve been fortunate to come across quite a few places that fit this profile: stunning, unique, reasonably accessible, and—here’s the big one—empty. Places like Zion National Park may be bursting at the seams, but vast swaths of Southern Utah remain deliciously deserted. On a warm and beautiful weekend in early May, we had Pine Park pretty much all to ourselves!

Large Ponderosa Pines complement the smooth knobs of white tuff.
The main draw at Pine Park are the spectacular rock formations carved into the Tuff of Honeycomb Rock. Tuff is a deposit of consolidated volcanic ash combined with rock, mineral, and glass fragments that forms only in very explosive volcanic eruptions. Pine Park sits on the margin of some of the most voluminous and expansive deposits of tuff in the world. Collectively, the thousands of feet of tuff scattered across large swaths of Nevada and western Utah represent a time when, for lack of a better descriptor, all hell was breaking loose across what is now the Great Basin. The Tuff of Honeycomb Rock is just a hair under 12 million years old, and thus one of the youngest deposits from this intense and violent episode of volcanism.
While the backstory of the tuff is intriguing, the real allure is the wonderland of creamy white spires, domes, and hoodoos emerging from the otherwise nondescript juniper, ponderosa, and piñon pine forest. Weathering and erosion have sculpted a masterpiece at Pine Park. In many places, the architecture almost resembles Bryce Canyon, albeit whitewashed, and with no maintained trails (several Forest Service trails wind through this area, according to the official map, but we had difficulty following them for any more than a hundred yards past the trailhead) the many pockets of eroded tuff are truly a blast to explore.

The Ponderosa’s don’t require much soil to gain a foothold in small depressions between ridges of tuff.

This species of lupine (Lupinus aridus?) seemed to love the gravelly, sandy soil produced by weathering of the tuff.

Fantastic rock formations immediately adjacent to our campsite.
The tall, stately Ponderosas and a small stream give Pine Park a high-altitude feel, but in reality it sits at just 5700 feet above sea level, plenty low and warm enough for a plethora of wildflowers to be in full bloom during our visit:

Bitterroot (Lewisia rediviva) are abundant on long-ago burned slopes above Pine Park, now home to open grasslands.

A claret cup cactus (Echinocereus triglochidiatus) in full bloom. I’m fully aware that the color appears somewhat enhanced on this photo, but it’s not; the claret cup flower really is that brilliant!

The lupines were everywhere.

Everywhere!

Multicolored boulders litter a chute in the Tuff of Honeycomb Rock.