After a pretty smoky early morning, the wind blew it east and away again most of the rest of the day. The wind still is switching between southwest and southeast and south. Cassidy Rain and her band were just leaving water; you can see the mud on her right front leg.
This is a very wide view (cell phone) from the main/original water catchment looking south/southeast. The source (ish?) of the Ferris Fire is at far right. I think it might have been the wind that had the smoke so ragged; clouds were actually visible low to the horizon, through the smoke. (Is that weird? It seems weird; the smoke on the horizon(s) has been so dense that it seems unusual to see anything beyond it, whether that’s the far ridges or even clouds.) You can see how clear it is between here and there. Fortunately for the mustangs, they’re not dealing with a lot of smoke.
From near the western boundary of Spring Creek Basin, looking west/northwest as the sun drops into a bank of smoke drifting from the Utah fires and maybe some farther southwest of Disappointment Valley in Colorado. Earlier in the day, the mountains were fully visible and the smoke was behind (west) of them. Then there was a period during the day when the mountains were fully obscured by smoke again. And here, at the end of the day, they were visible below the band of smoke. I think that great band of smoke was from the southern fires and joining smoke from the northern fires (like the Snyder Mesa Fire).
This last image is from about the same place as the one above, but now we’re looking nearly directly north. See the painterly smoke from left that fingers to the right, right of center? That’s from the western fires. See the greyer smoke at right? That’s from the Ferris Fire. Straight south and to the southwest, we’ve had a clear sky, and straight-ish north, we’ve had a clear sky. Tonight, the smokes from west and east have joined in the north. Wild, right? (If you look closely, those white dots at center left, on the sloping edge of the northern Spring Creek canyon side, are mustangs. :))
We continue to be very lucky in location, and the mustangs are doing very well.
Gratefully, while the Ferris Fire burns 20,560 acres to the southeast and the McCloud Fire and Horse Head Fire burn 113 and 530 acres, respectively, to the southwest (and that smoke is joined from the Snyder Mesa Fire (30,163 acres) to our north/northwest, drifting southish), Spring Creek Basin and lower Disappointment Valley were mostly smoke-free yesterday.
In the pic above, Tenaz and Skywalker, grazing with their band almost at the western boundary of the basin, are highlighted by that drifting smoke to the west. It’s fairly far away, but I haven’t seen Utah’s La Sal Mountains for at least a few days now as the smoke obscures any sight of them.
Now looking east/southeast, that’s the smoke from the Ferris Fire (the Doe Canyon, Far Draw and Ferris fires all have merged and are now being collectively called the Ferris Fire). But see how clear it is between here and there? Not great for folks and critters in that direction … but (again, gratefully), a huge relief for my beloved center-of-the-world Spring Creek Basin.
Huge thanks to sheriff’s deputies from both Dolores and San Miguel counties (Disappointment Valley spans both counties, and Disappointment Road runs from Colorado Highway 141 at the lower north end to the Dolores-Norwood Road at the upper southeast end) who have been diligent in keeping an eye on the fire’s approach: Branson, Todd, Derek, Jeremy and Nick. Also to my BLM folks, especially Ryan and Laura, for keeping an eye on the situation and updating me with information. Anton was on one of the fire crews pulled back Saturday for safety on the Doe Canyon Fire, and he might still be on a fire crew on the merged fire.
This won’t be an easy post to either read or view.
*THE MUSTANGS ARE SAFE*
That’s the important thing (as far as the main topic of this blog, anyway).
Yesterday, Saturday, June 27, at least three wildfires of significance roared to life directly south of Disappointment Valley: Ferris Fire (4,777 acres as of Saturday evening), Far Draw Fire (651 acres) and Doe Canyon Fire (385 acres). There’s also the Horse Head Fire (200 acres) burning to the southwest, in Utah, and the Snyder Fire (28,264 acres) burning north-northwest of here, almost directly west of Grand Junction and just inside Utah.
Red-flag warnings; check.
Wind advisories; check.
Bad air quality; check.
Critical fire weather; check.
Stage 2 fire restrictions in San Miguel and Montrose counties; check (these might extend to other nearby counties, but these are the ones I know about, and most of Spring Creek Basin is in San Miguel County, with the southern/southeastern portion in Dolores County).
Kentucky is flooded, and the West is on fire. Friday night, we had a swift little storm pass through Disappointment Valley – 0.04 inch from four minutes of rain. My guess (guess only; I don’t know yet the cause of these fires) is that they started from lightning strikes. It is one giant tinder box out there. Until the little bit of rain Wednesday, it hadn’t rained here for more than a month.
If images of wildfire smoke bother you (it bothers me), the rest of this post isn’t for you … and the pictures, as usual, don’t convey the bad-ness of the beast. … Again, please know that the mustangs are SAFE. I can’t say what the fires will or will not do, but for now, the horses are OK and not in danger.
I spent most of Saturday in Ridgway with mustang friends, and this is what greeted me and Kat Wilder upon our return to Disappointment Valley. This is from the northern part of the valley, a few miles south of Colorado Highway 141, looking southeast.
Looking west at sunset; this smoke is from the Utah fires.
The majority of the smoke seems to be passing east of the eastern side of Spring Creek Basin; McKenna Peak, Temple Butte and Brumley Point are all visible. … The smoke ain’t great up-valley; it smells like you’re in the middle of a campfire (and by the way, campfires and any other kind of fires are strictly verboten (that means forbidden!), not to mention dumb as hell).
Blue hour appeared while I was waiting for a sunset explosion that never manifested; the clouds in the west ultimately were just too heavy. But there was a nice bit of light highlighting Utah’s La Sal Mountains, and Winona prettied up the scene nicely.
What follows is a random selection of cellphone pix from a couple of evenings ago in wild, woolly and very windy Spring Creek Basin.
First sego lily of the season! That I’ve seen, anyway. It was SO windy, the flower was whipping around like crazy, so I tried to hold it still for my phone. It’s always a bit of a crap shoot to try to take pix of small things with my phone because I can’t see at all whether the *thing* is in focus or whether it’s the background.
Case in point: I took several pix of this beauty, within a couple of feet of the first one, and only the last one was in focus (that could have been the wind). I adore these lilies – in the desert! These seemed smaller than usual, but I’m glad to see them.
While the pix of the sego lilies seem to suggest that it was sunny, mostly we had these crazy, wildly dramatic clouds looming over the basin. These are mammatus clouds. Looking eastish-northeastish.
Google AI says:
Mammatus clouds are distinct, pouch-like cloud protrusions that hang downward from the base of a larger cloud, usually a towering cumulonimbus. Named after the Latin word for “udder” or “breast”, these stunning formations are fascinating for their unique shape and the rare meteorological process that creates them.
How They Form
Unlike most clouds, which are created by rising air (updrafts), mammatus clouds are formed by sinking air (downdrafts). [1]
The Process: Pockets of cold, dense air saturated with heavy ice crystals and precipitation sink downward from the parent cloud (usually the “anvil” of a thunderstorm).
The Shape: As these dense, cool pockets of air descend into warmer, drier air beneath the cloud, the ice and water begin to evaporate. This evaporation cools the air even more, causing the pockets to sink further, creating the characteristic rounded, bubble-like pouches. [1, 2, 3]
What They Indicate
While their ominous, alien-like appearance might make them look like the beginning of a severe storm or tornado, mammatus clouds are generally a sign that the worst part of the storm has already passed or is off in the distance.
Severe Weather Link: They are most commonly spotted in the vicinity of strong thunderstorms. If you spot them during the summer months, it usually means there are powerful storm cells nearby.
Safe or Not: Mammatus clouds themselves do not produce severe weather and are not dangerous to anyone on the ground. However, pilots are warned to avoid them because the sinking air can cause intense turbulence.
Key Characteristics
Composition: Because they hang high in the atmosphere, they are primarily composed of ice crystals rather than liquid water droplets.
Lifespan: They are relatively short-lived, typically appearing and dissipating within 10 to 30 minutes.
The Best Time to See Them: They are particularly striking at sunset or sunrise, when the low angle of the sun illuminates the underside of the pouches, turning them brilliant shades of gold, orange, pink, or deep blue.
In our case, they appeared around three hours before sunset, so we didn’t get the color, but they’re still pretty amazing to see, even if they also did NOT bring us any rain.
This was taken at about the same time, now looking eastish to southeastish. And quite a bit later, it looked REALLY rainy out beyond our local horizon. So hopefully somebody somewhere got some wet stuff.
Have to have a pony walking the skyline. 🙂 He was heading to the Spring Creek arroyo (down to the left), and pretty soon, his band followed. Looked like it was raining somewhere out in that direction, too (westish-southwestish).
And at the very end of the day (an hour or more later than the last pic), a pretty glorious and somewhat unexpected (and *very* brief) shot of sunset brilliance from the west end of the basin looking westish-northwestish. There were horses immediately behind me, but they were already in the shade of the hill, and that side was already fairly darkrainydusty (? did I mention the howling wind?).
Even under the “worst” conditions, there’s always such beauty. 🙂
Tuesday was a wild and crazy day … and that was just the weather. It was ultimately a successful day, though at least one part left me shaking my head at, well, how life unfolds. And it was a reminder that sometimes the smallest things, and the simplest things, are the most enjoyable of all.
From yesterday’s post, are you wondering what graupel looks like? (Thanks, Valerie, for your comment that led to this post!)
What? I hear you asking. That looks like snow or rain, you’re saying (zoom in to see the streaks). Look on the ground in the lower right corner. I was backed in under a (dead) tree to sit out one wave of it (it wasn’t very hard, and it didn’t last long) at that little side “road” to Disappointment Road, which is across the whole pic. See the little white “balls”?
AI says this: “Graupel, or soft hail, forms when supercooled water droplets freeze onto falling snowflakes, creating soft, small white pellets (2-5 mm) that resemble Dippin’ Dots or Styrofoam. These fragile, slushy particles are often called snow pellets and, unlike hard hail, crumble easily. They occur during wintry mix scenarios, causing sudden, slick conditions, and are identified in aviation reports as ‘GS’.”
I liked this part: Types of Graupel While commonly called graupel, it is sometimes referred to as:
Matsaaruti: A term used in the Nunavik region of Canada to describe wet, soft snow pellets.
Another pic from the same location as the first pic, looking pretty much straight north at what I call west-of-favorite hill (because it’s, you know, west of what I call favorite hill, which I so-named because once upon a very long time ago, “the pintos” really favored that hill and could very often be found atop it).
Also from the same spot, looking eastish again as the graupel wave recedes, driven by a strong out-of-the-south wind (I lost track, but at least three, maybe four went over us Tuesday morning). You can see Brumley Point very distinctly, submarine ridge and McKenna Peak to the left it it, and you can’t quite make out Temple Butte. If you slide back up to the first pic, Temple Butte is juuuuuust barely visible at far left, just under the power lines. And yes, the sunshine IS coming back out over the rest of us while the wave pushes north to the east.
With Artemis II and its remarkable human beings on board, their mission, their accomplishments, the images they sent back, from space looking home, in mind … and realizing the absolute tiny-ness of this one itty-bitty part of our great, wide, wild, wonderful, big blue marble … ain’t Earth gorgeous? Now you can see Temple Butte’s promontory emerging from behind Brumley Point (see the graupel/moisture evidence shining below its rimrocks?) and submarine ridge and McKenna Peak. And though you can’t see them in this pic, there were two groups of mustangs out there. Across the road and on the other side of that fence IS Spring Creek Basin.
Anybody know what this prickly little caterpillar is called? I’m not sure of the plant it’s on, either.
I tried a lot, but I could NOT get the eye end (far left – is that an eye?) in focus. Of course, I didn’t know that in the field, not having my eyeball glasses on and looking through the glare of my phone screen, but I did try a number of shots with high hopes. One of our BLM range guys recently posted a pic of the same caterpillar, but he’s a plant guy (and an extraordinarily awesome one), not a bug guy, so I’m sure he can tell me the plant, if not the bug (!). If I reach him for an ID before this posts (or even after), I’ll update.
** Update from Ryan, BLM rangeland management specialist and all-around plant guy!:
“Cool that you’re seeing the same caterpillar! [He saw the same kind recently in Canyons of the Ancients National Monument, southwest of Spring Creek Basin.] I’m very curious as to what species of butterfly/moth they will turn into, I’m not good at insect ID but will ask Nate West [BLM wildlife biologist]. The plant that those are on is a mustard species called Alyssum simplex, commonly just called madwort. It’s a pretty prevalent non-native annual that is really common around here, unfortunately. It’s a beautiful picture of the hair-structure on the caterpillar!” Thanks, Ryan!
The reason you can’t see Utah’s La Sal Mountains in this pic – way northwest of Spring Creek Basin, from the very far southeastern part of Spring Creek Basin – is because the rain/graupel/snow wasn’t through sending waves over them. 🙂 You CAN see, from right to left, Round Top, Flat Top (looks sloping), Filly Peak and the south-facing rimrocks. Disappointment Road is over to the left somewhere (not far)
From here, we’re looking over not much of the southern part of Spring Creek Basin Herd Management Area (the pic above this one has a perspective to the right of this one) but a lot of the south/southwestern part of Disappointment Valley (most but not all of the pinon-juniper woodlands as far as the eye can see). The near pinon-juniper is within Spring Creek Basin.
From the same spot now looking back to the south/southeast at another little rain/snow/graupel-fall, toward the Glade and Benchmark Lookout (hi, Rick and Linda! (I think they’re not at the fire lookout tower quite yet)). The near hills and pinon-juniper are all within Spring Creek Basin. The far, thickly treed ridges are partly (middle-ish ground) part of upper Disappointment Valley and partly (farther) part of San Juan National Forest lands beyond Disappointment Valley and its watershed.
And what the heck was I doing at the high end of a long drop? See the horse trail? 🙂 I was following where the sure-footed have gone before me (and not for the first time).
The above are in order of how I took them … hours apart from first to last.
And because you came here for the mustangs …
Mysterium, modeling her scruffy-chic look (fashion designers, take note – ha!) below Temple Butte. 🙂 Yes, those are a couple of cuts on the inside of her left hind leg, but she’ll heal quickly, as mustangs do!
Thanks, as always, for coming along for glimpses of this special world. 🙂
Alegre does the slow saunter through the greasewood. She’d been grazing away from the band, and I took advantage of waiting for her to catch up, catching her as she walked through the backlighting and past the mountains.
Going back a couple of days, to the time before the wind when the mountains were still clear on the northwestern horizon.
I read an article recently about how lack of dust on the snow of the mountains is a good thing. … And it is (dust causes the snow to melt more rapidly). … But I imagine that those same researchers will find a pretty “good” layer of dust after this weekend, and that just joins the bad news of “skimpy snow” (according to the article) to begin with.
Still, we have to admire the positive, and that’s Flash and all our other wild ones in that magnificent landscape. … And pray for a wet(ter???) spring.
2-
5
mm) that resemble Dippin’ Dots or Styrofoam. These fragile, slushy particles are often called snow pellets and, unlike hard hail, crumble easily. They occur during wintry mix scenarios, causing sudden, slick conditions, and are identified in aviation reports as ‘GS’.”
