The last time I wrote about Aquila’s Eagle Eye was in 2018, and I didn’t have much to say about it—other than it was there. That post included a photo I shot with a telephoto lens from miles away. I had to do that because much of the land around the peak is posted as private. There were two comments in that column. The first was from Fred, who thanked me for pointing the bridge to him, and the second was from my old friend Gary, who chastised me for not getting closer.
Since I’ve been hanging around Aguila this month anyway, I thought I’d try to make Gary happy. About three miles south of Aguila are mountains on the east flank of the Harquahala range. They almost have the same name; Eagle Eye Mountain is on the west, while Eagle Eye Peak is the lump of lava to the east (they touch one another). The latter peak is the one with the window on top.
Eagle Eye Peak – A natural arch on top of a peak several miles south of Aguila, Arizona. Behind Eagle Eye is the Harquahala Plain, which stretches south to the Big Horn Range on the horizon.
You can get very close to the arch if you drive to the old cemetery where Eagle Eye Road bends around the mountains. The bad news is that you can’t see the arch from there because it faces east, and all you see are the rocks from the edge. There’s a better view if you scramble up an 800′ cactus-infested lava hill like an insane person, but I did the lazy thing. I brought my drone, and I flew it to the mountaintop. Once it got up there, I rotated it to the right and composed this shot.
The Eagle Eyes, like a lot of low desert mountains, were formed from volcanic activity. This particular pair of mountains is basalt-covered limestone. The rocks are much darker than the rest of the Harquahala Range. They appear as shadows on the horizon. Their surface is rough and pockmarked, like they had a bad case of acne. They are riddled with caves formed by air pockets in the lava.
I didn’t find an article that explains how this arch was formed. I don’t think it was formed from wind erosion. The rocks aren’t polished. It could be from one of those air voids in the thin-walled lava collapsing. My favorite guess is this: If this is Rhyolite—slow-moving lava common to peak formation—then maybe a cone of lava formed vertically, and as it cooled, it slumped over and froze in place. At least, that’s what it looks like to me. What do you think?
Well, Gary, I hope you’re happy. Click here to see a larger version of Eagle Eye Peak on its Web Page. Be sure to return next week when I’ll show you the arch from a different perspective.
It’s already the last day of January. Where does the time go? After looking at this month’s photos, it seems that I spent a lot of my time around Aguila—with good reason. That’s the route that Queen Anne and I take when we travel west, so I knew there was stuff to shoot, and it’s close by—well if you consider an hour close.
Foothill Uplift – A pair of hills thrust into the air by plate tectonics.
This week’s featured image comes from the same area. I didn’t have to travel far after I captured last week’s picture—Harcuvar Forest. In fact, all that I needed to do was turn around. OK, let me explain. I wanted to shoot the saguaro forest ever since I first saw it on a trip to Robson’s Mining World, but it’s miles north of the highway and tucked under the cliffs of the Harcuvar Mountains. My topo map shows a jeep road that runs behind a couple of hills situated between the highway and the forest. The hills screen the cactus patch from the highway. So, me and Archie did a little four-wheelin’.
After I had finished shooting the saguaros, I noticed that the north side of the hilltops behind me weren’t rounded as they appear on the south. Instead, they had a ridge of broken rocks—plate tectonics fractured them and pushed them towards the sky. Since I find edges like these interesting, I decided to waste some time photographing them.
This week’s featured image is the result of my curiosity. I call this photo Foothill Uplift. There are a couple of things that I like about this image. I like how the second hill repeats the pattern of the foreground one. It’s like they’re lined up for presentation. The same wedge shape shows up again on the photo’s right side. Along the horizon and on the far side of the Aguila Valley is our old friend Black Mesa. It’s the western high peak of the Vulture Mountain Range that stretches all of the ways back to Wickenburg. Finally, I love the double-headed saguaro, which I couldn’t see from the trail. It’s the garnish that completes the cocktail.
You can see a larger version of Foothill Uplift on its Web Page by clicking here. Be sure to come back next week, and I’ll see what I can scrounge up from around the neighborhood.
Our home in Congress is on a scenic byway. Each weekend, lines of exotic sports cars and motorcycles pass by our trailer park to prove it. Several roads, like AZ 89, in our state offer motorsports enthusiasts a venue to stretch the legs of their beloved machines. I’m sure that the other states have roads like ours. I’m surprised someone hasn’t compiled an encyclopedia of “The World’s Great Weekend Roadtrips.”
The route passing our home is known as the back road to Prescott because it avoids the weekend traffic on Interstate 17. It’s a longer drive, but that’s not the point. I think this passion is best described in Queen’s song; I’m in love with my car. “. . . get a grip on my boy-racer roll bar…” (Yes, Virginia, Queen recorded songs other than Bohemian Rhapsody). It’s customary to play this anthem at full volume with the top down and the sun flickering through the pines onto your Ray-Bans.
There are actually two ways to get to Prescott from here. The first is to stay on ’89 and drive between the Sierra Prieta and Bradshaw Mountains. The motor-heads like this way because they get to test those big Brembo brakes on their Lamborghinis. This way, it is challenging to keep up with the speed limit; you’re up in the pines quicker, and the road dumps you onto Whisky Row, where everyone parks around the courthouse for an impromptu car show.
The second option is better if you tow a trailer, haul a load of eggs from Costco, or try to keep Queen Anne from throwing up in your lap. To go this way, you turn off at Kirkland Junction and pick up Yavapai County Route 10—Iron Springs Road. This route is more docile as you travel through Kirkland, Skull Valley, and Iron Springs, although it’s a bit trickier to find your way downtown once you get to Prescott.
Kirkland Peak—Runoff from the granite-covered mountain has cut into a limestone layer deposited on an old lake or sea bed.
On this second route, you’ll see the subject of this week’s featured image—Kirkland Peak. The rocky mountain will fill your windshield at the Kirkland stop sign. There’s even a better view if you drive straight and cross the tracks. But right now, we’re going to turn right onto Iron Springs Road toward Prescott because there’s something else I want you to see.
Soon after leaving the junction, CR 10 follows the railroad tracks and Skull Valley Wash, filled with cottonwood trees. In this section, between Kirkland and Skull Valley, there is a cluster of limestone hoodoos where the granite top layer has been eroded. I’ve tried to photograph the outcrops on several occasions, but telephone lines and private property frustrated me. When I visited last week, a new mine began setting up operations, and they scraped the land clean. There are two new five-story silos built beside the road, and I’m afraid that the remaining hoodoos will be gone shortly.
When I drove up to shoot Kirkland Peak this week, I was pleased to find where the mountain’s runoff has exposed more limestone, as seen in this week’s picture, called Kirkland Peak. There are eons of geology exposed in this photo. The bottom layer is an ancient lake or sea bed, covered by granite (lava cooled slowly), and a mountain thrust above it. The evidence of up-thrust is in the grain of its rocks along the ridgeline (you can’t see that on your phone). As Kelly Bundy said, “The mind wobbles.”
Click here to see a larger version of Kirkland Peak on its website. Next week, I’ll bring you another image from our corner of the world.
Sometimes you get lucky. As a photographer, I keep scenes in my head, so I can go back when the light is right when I want to capture them. That’s what happened for last week’s image, Resting Santa. We had a series of dry fronts move through Congress during the month, but the weather forecasts called for an afternoon where the sky would be clear so the evening sun would pleasantly light up the Harcuvars. I left the house at 3:30 and purposely drove out to get that shot. It was practically a product shot.
More often, I pass by beautiful once in a lifetime scenes that will never be replicated, and I chastise myself for not having a camera with me—or worse—not taking the time to stop. That’s almost what happened with this week’s featured image.
Date Creek Clearing – A clearing winter storm hangs over the Date Creek Range in the evening sun.
After I was finished shooting Resting Santa, I drove home on State Route 71. I was looking forward to getting back to a warm home, a nice glass of wine, and one of Queen Anne’s famous home-cooked Stouffer’s dinners. The sun was low on the horizon, and outside my window, a golden cloud hung over the Date Creek range. The conversation in my head went something like this.
“Oh my, that’s gorgeous. I should really come back with the camera sometime when the light is like this.”
“You idiot! Your camera is on the passenger seat, and the light is like this right now. Stop the truck, walk across the road, and take the picture.”
I was very convincing, so I did stop and take a shot—several of them to be exact. The version that I like most is called Date Creek Clearing. There are two prominent peaks in the Date Creek Range; both of them are unnamed. On the left is the rocky pinnacle that ate my first drone, so I call it Drone Eater Mountain. On the right side is the Range’s high point. They are only bit-players in this photo. The real stars here are the clouds caught in a moment that can never be duplicated. Those storm leftovers can never be the same.
I know that my work is considered trivial and will never warrant a Pulitzer Prize or other great awards. I shoot mostly meaningless pretty pictures, valued at a dime-a-dozen. But on a week such as the one we’ve experienced, I needed a bit of calmness and serenity. If you feel the same, then this is my gift to you.
You can see a larger version of Date Creek Clearing on its Web Page by clicking here. Next week, I’ll bring you another image from our small corner of the world. Stay safe.
My first Phoenix visit was during the summer of my high school junior year. It wasn’t much of a visit. Dave and Edith—my mom’s niece and her husband lived here. They moved here from Michigan, and he hadn’t been able to find steady work as a mechanic, so my dad offered him a job maintaining his debilitated fleet of Corvair vans. They accepted and immediately packed up to move to the coast. Since I was on summer vacation and my wallet had that new-drivers-license smell, dad volunteered me to drive one of their trucks.
My father put me on an early flight out of the tiny Burbank Airport, and I arrived at an even smaller terminal where Dave met me. Parked at the curb outside was his white El Camino. I don’t remember the year, but it was loaded with toolboxes and the rest of his shop equipment. I didn’t question if it was overloaded because that was above my pay grade and comprehension at the time. I was only impressed that it had a four-on-the-floor, and it made a rumble when he started it.
We drove straight to their home, where a moving van was packed and ready for the trip. The only things that I got to see in Phoenix were the airport, the freeway, his house, and the biggest Goodyear Tire sign in the world. Even Hollywood didn’t have a sign that big and bright. I do remember that it was only mid-morning, and it was already hot. Automotive air conditioning was an exotic thing back then, so we drove with the windows down.
We didn’t spend much time at the house because everything was packed and ready. I was assigned to drive the El Camino, and he would follow in the U-Haul (or whatever brand he had rented). Both vehicles were packed to the gills, but Dave still had loads of unpacked clothes and threw them on my passenger seat before heading west on Highway 60.
Not many cars had air conditioning in 1963, but they all had wind-wings, little adjustable windows at the front of the door windows. They were useful for defogging the windshield, sucking out cigarette smoke, and when driving across the desert, they would divert the scorching wind from your face. By noon we were driving across the open desert west of Wickenburg, and my wind-wings were wide open.
Cars also had temperature gauges then because they frequently overheated. Nothing was broken; they just did that. While you drove, you watched your speed, the gas gauge, and the water temperature. You planned your stops by what the gauges said. As the day grew hotter, and the overloaded little El Camino began to run hot, and I pulled over to let Dave know. We began stopping at gas stations in each of the little towns we passed in an abundance of caution. There we would hose down the truck’s radiator and then continue on our way.
That was until we stopped at a place in the middle of nowhere. As I looked around, all I could see was the barren desert surrounded by dry, jagged mountains. The water spigot had a lock on it and a sign that read, “Water 1.00 a gallon.” That was five times the price of his gas; it was outrageous. The man behind the cash register justified the cost by saying, “Look around you, kid. Do you see any water? I have to pay to have this trucked in.” We gave in and bought a couple of gallons and slowly poured it over the gurgling radiator.
We drove another 200 miles without another incident, all the while the expensive water ate at my brain. Once we reached the cooler air in San Bernardino, the little truck behaved itself. As we drove the two-lane road crossing the lower Mohave Desert, we saw hundreds of freeway miles under construction off to the right. Interstate 10 was finished from L.A. to the Colorado River when I moved to Phoenix a decade later. In Arizona, it stopped at a place they called The Brenda Cutoff. For years I wondered who Brenda was. After moving to Congress, I realized that Brenda was the town where that infamous gas station was, and I finally put two and two together.
New Water Black Mesa – The early morning sun highlights Black Mesa’s cliffs overlooking Interstate 10 in western Arizona.
Last Tuesday, I pointed out the old station’s ruins and told Fred this story—well, an abridged version—as we drove back from our photo-shoot. We went there to photograph this week’s featured image of the Black Mesa in the New Water Wilderness Area. The Ramsey Mine Road approaches the wilderness, and it starts in Brenda. The lava-rock covered mesa cliffs are another of my favorite Interstate 10 landmarks. When I see them on the south side, I know that we’re almost to Quartzite, and the Colorado River is soon after. I’ve admired these formations each time I pass under them, and it’s taken me decades to figure out how to get closer. I called this shot New Water Black Mesa because there are dozens of Black Mesas throughout Arizona, so I have to start including which mesa I’m talking about.
You can see a larger version of New Water Black Mesa on its Web Page by clicking here. Next week we start a new monthly project as well as a new year. Queen Anne and I will still need to keep close to home, so come back next week and see what subject we chose.
