The upside to the epic Winter we recently experienced is the tremendous amount of snow melt that filled many of the lakes across northern Arizona. Over the past several weeks we have visited several of these by car, mountain bike, running, and hiking.
This is one of my favorites. It shows Upper Lake Mary, a portion of the spillway, and Lower Lake Mary. It’s also nice that there is a nice mirror reflection of the trees in the water. This shot is only possible when both lakes are full.
Earlier we had visitied Marshall Lake. It’s not as full as it was a few years ago but considerably better than the past several years.
We did a trail run along the Arizona Trail on top of Anderson Mesa and visited Prime Lake and Vail Lake, both with lots of water.
Here are some additional images of Lake Mary taken on various days in April.
We rode our mountain bikes up Schultz Pass Road to Schultz Tank. It has been a small puddle the past two seasons but is once again full.
Finally, we did a short hike through the upper portions of Pumphouse Wash to this set of cascades.
The snow melt is done and we are now in our dry season. Lake levels and stream flows will diminish until the summer rainy season starts in July.
Pumphouse Wash is a canyon that is ignored by most of the people who drive past it every day. It is located in the upper reaches of Oak Creek Canyon right at the bottom of the well-known switchbacks. No matter — its best quality is that very few people hike it.
During heavy rains and snow melt there will be water flowing down the canyon. Otherwise it’s a dry wash with a series of pools. The canyon is narrow with steep walls. It’s full of boulders strewn in the stream bed that have been washed down in great floods. The plethora of boulders makes hiking in this canyon a slow, arduous process. One must hop from rock to rock for miles.
But the rewards are worth the effort. You won’t encounter many other hikers. Maybe even none. And there are beautiful pools and narrows if you travel far enough up the canyon. Late in the spring the pools are still deep and clear and inviting enough for swimming. By early summer, however, they have warmed and filled with algae and, maybe, not so inviting. Timing is important.
So we recently hiked up from the bottom of the switchbacks up to the confluence with a small side canyon that comes in from the east. No name is given on the maps for this feature — not to be confused with James Canyon farther upcanyon. This is about 2¼ miles from the start and it took us about 2½ hours. That’s less than one mile per hour. There was no one else around — although we could hear hikers farther downstream owing to the echoes off the canyon walls. We stopped in the shade and had a leisurely lunch followed by a swim in one of the deeper pools. And then back in the shade for more lounging.
But eventually it was time to go. It was now mid afternoon and the sun had moved around to the northwest leaving us in shade for most of the trip down canyon. Good thing, too, because it had been sunny and hot on the way up and we were worried about running out of drinking water. Also, with the canyon floor in the shade it was easier to take photos of the pools of water and the short section of narrows.
And, then, there was that magical moment when the light created a perfect situation. The sun lit up a section of the canyon floor which was reflected upwards to an overhang. The reflected light on this overhang was beautiful — but this illuminated overhang was reflected in a pool of water surrounded by deep shadows. Amazing! Move a little closer and the pool and reflection did not line up. Move a little farther away — same thing. Just one spot — and it was perfect.
Flagstaff’s February weather has been very active with rain and/or snow recorded on seven days out of the first fifteen. Several days of snow on the Kachina Peaks covered the trees with a thick coating of rime ice and lots of new snow on the slopes.
And then we had an “atmospheric river” that produced a significant amount of winter rain with about 1.5 inches falling in the Flagstaff area. The runoff in Oak Creek and its tributaries was impressive.
And the forecast for the next week or so is a continuation of stormy weather with lots of snow for the higher elevations. I believe the long-anticipated El Niño has finally arrived.
Not too far south of Flagstaff lies Pumphouse Wash, a beautiful and narrow canyon that cuts through the Kaibab limestone and Coconino sandstone. The canyon drains from the upper elevations of the Mogollon Rim into the headwaters of Oak Creek. Most of the time Pumphouse Wash is dry with occasional pools but it can run very full during the spring snow melt and after heavy summer thunderstorms.
Shortly after a light snowfall in late November I took a walk up the wash hoping for some interesting photographic possibilities with snow and ice. I wasn’t disappointed. The first image shows a small pothole scoured by the erosive actions of the occasional flood waters. It was filled nearly to the brim with rain and snow melt, perfectly blended with leaves and pine needles, and then frozen in time.
Elsewhere in the canyon a sycamore tree had shed its leaves among the boulders of the wash and upon these leaves some snow was still in place.
Although it was a sunny day in northern Arizona very little of that sun was able to penetrate into the confined narrows of Pumphouse Wash. And I had the canyon to myself that day.