One of my personal rules for photography is knowledge of my subjects—I simply get more pleasure from an image when I know something about what I’ve captured. Of the many potential subjects available to a landscape photographer, mountains have always been a particular draw for me. Living my entire life in the shadow of the Sierra Nevada has certainly influenced that connection, as have fond memories of family camping trips in the mountains throughout my childhood, and Sierra backpack trips with friends in my teens and beyond. In college I even majored in geology for several semesters (after astronomy, but before eventually earning my bachelor’s degree in, yawn, economics), and was most interested in the processes responsible for mountain building: tectonics and volcanism.
Given all this, I guess it makes sense that after returning from last month’s Iceland trip I found myself digging a little deeper into the origins of Kirkjufell, the prominent peak that is arguably Iceland’s most recognizable landmark. Game of Thrones fans who recognize Kirkjufell (Arrowhead Mountain) will be relieved to know that, after several visits over the last few years, I can confirm that the White Walkers appear to have moved on. (But come to think of it, maybe that shouldn’t be much of a relief….)
Kirkjufell rises slightly more than 1500 feet above Breiðafjörður Bay on the Snæfellsnes Peninsula. Given Iceland’s volcanic origins, it would be reasonable to assume that this cone-shaped peak is just one of of the island’s many volcanos. But that assumption would be incorrect. Skeptical? The mountain’s clearly visible parallel strata layers are a giveaway that Kirkjufell is not a volcano. (And viewing from other angles would reveal that Kirkjufell isn’t really cone-shaped either.)
Though many of Kirkjufell’s layers were indeed laid down by lava or explosive debris from nearby volcanos, these igneous layers are interspersed with layers of submarine sediment deposits, each layer a product of the environment at the time of its deposition. Kirkjufell’s base layer was a large lava flow that happened sometime in the last 5 to 10 million years (relatively recently in Earth’s grand geological picture). After that came millions of years of alternating sediment and volcanic deposits, separated by thousands or millions of years for which there’s no record.
This assortment of parallel layers created a horizontal layer cake of strata bearing no resemblance to the mountain we know today (or any mountain for that matter). Because all sedimentary layers are deposited horizontally, and Kirkjufell has a slight SE-NW tilt, it would also be reasonable to assume that at some point since the last layer went down, the entire area to the southeast rose relative to the area northwest.
Once all Kirkjufell’s layers were deposited and tilted, the area was squeezed between two glaciers that carved away most of the surrounding rock, leaving the remaining peak jutting above the glaciers like an island. When the glaciers retreated, the peak we see today remained.
The other striking feature in this image is the pink that spreads in the shadowless pre-sunrise/post-sunset sky of civil twilight, when the sun is around six degrees or closer to the horizon. Sometimes called the “Belt of Venus,” we get this color because the only the longest, red wavelengths are able to traverse the atmosphere once the sun drops below the horizon.
The interface between the Belt of Venus and the blue-gray Earth’s shadow directly is called the “twilight wedge,” a designation earned because you can sometimes see the earth’s curve in the shadow, with its apex at the anti-solar point (directly opposite the sun). At sunset, the gradual upward motion of the shadow gives the appearance of a wedge being driven into the darkening sky.
About this image
I won’t pretend that there’s anything especially unique about my composition here (and I have the pictures to prove it)—it’s one of those scenes that improves more with conditions than composition, especially if you haven’t been here enough to get really familiar with it.
Because this was the first evening of photography for Don Smith’s and my 2022 Iceland photo workshop, Don and I stayed especially close to the group. From past visits I knew that to align Kirkjufell and Kirkjufellsfoss (the waterfall), you’re pretty limited for places to set up, but we managed to find prime tripod real estate for everyone. I encourage my groups to move around as much as possible, but the thick snow and steep drop to the river further limited our mobility, so we just lined up along the cable barrier between the trail and the drop. And because there were other people besides our group out there, once you landed a vantage point, you were pretty much stuck there until someone moved.
Given the mobility limitations and my desire to align the mountain and waterfall, my composition options were mostly focal length choices. Another, self imposed, compositional limitation was my desire to exclude the footbridge just out of my frame on the left. I like to believe that if I’d have been here by myself, with lots of time to explore, I’d have come up with something a little more creative. But I’m certainly not complaining—between the fresh snow and beautiful sky, the conditions for photography were off the charts and everyone was thrilled.
This image came late in the shoot, just as the twilight wedge reached peak color. By then I was pretty familiar with all my composition options and opted to go with my Sony 16-35 f/2.8 GM lens at 17mm (an my Sony a7RIV body). Turns out my resulting composition is remarkably similar to my northern lights image from later that night, and a sunrise image I captured here 3 years ago. Since I clearly have this composition nailed, I’ll need to challenge myself to find something different next year.