More mining claims staked at #BearsEars: Plus, the story of #LakePowell’s 26,000-ton pile of radioactive waste — Jonathan P. Thompson (LandDesk.org) #ColoradoRiver #COriver #aridification

Several of the latest claims located within the pre-shrinkage Bears Ears National Monument are on the north side of the Tables of the Sun, seen here in the background on the right. Jonathan P. Thompson photo.

Click the link to read the article on The Land Desk website (Jonathan P. Thompson):

September 25, 2026

⛏️ MINING MONITOR ⛏️

The mining claim game continues to heat up in the areas Trump illegally slashed from Bears Ears National Monument, and the top player is, once again, Kimmerle Mining of Moab. Since the Land Desk last wrote about this mini-land rush, Kimmerle has filed seven additional claims areas that had been within the national monument, and therefore off limits to new mining claims.

The latest claims are in the White Canyon area. During the post-War uranium frenzy, the federal government, county crews, prospectors, and mining companies webbed this area with roads, poked it full of prospect holes and mine adits, and contaminated waters with radioactive materials. Part of that legacy includes a 26,000-ton pile of uranium tailings entombed within the waters silt of Lake Powell.

It’s important to keep in mind that the presence of active mining claims does not necessarily mean anyone is going to mine or even explore these pieces of land. And while the claims may be active, which simply means the claimant is up to date on their $200/year location and maintenance fee, they may not be valid. That requires, at least theoretically, proof that the claim contains valuable minerals.

But it does appear as if Kimmerle is targeting viable mining areas, which indicate that the firm either intends to mine the claims, or consolidate enough of them to sell them to a larger company. The newly revealed claims are located in two clusters on either side of Natural Bridges National Monument.

The notices of location have been declared with the San Juan County Recorder, but have not yet shown up on the Bureau of Land Management database. Just before publishing this, I checked the San Juan County records search and found that an entity called Land Survey Advisers — which typically stakes claims for other firms or individuals — filed location notices on more than three dozen claims in San Juan County. At least some of those claims appear to be within the pre-shrinkage BENM boundaries, but the location description on many of them included sections that don’t exist (43, 47) in the public land survey system, and the document download function isn’t working for me, so I have yet to confirm any of this. Still, it’s potentially alarming.

Map showing the approximate location of the claims filed by Kimmerle Mining in Sept. 2026. It also shows pre-existing active claims (in pink) that were staked before Bears Ears’ 2016 establishment, or following the Trump I-shrinkage. Map: BLM and Land Desk.

The Kimmerle claims include: 

  • Six lode claims (each at 20.66 acres) on the north slope of the Tables of the Sun formations in the upper Fry Canyon drainage, just on the boundary line of the original Bears Ears National Monument. While this specific area has seen little mining activity in the past, it is in the same vicinity as the Daneros Mine, which was up for expansion as recently as 2016. And the new claims are adjacent to Kimmerle’s Lucky group of claims. 
    The nearest historic mining activity was at the Fry # 4 mine1, an underground uranium mine with over 400 meters of workings. In 1977, the operator was Utah Power & Light Co., which was the main mining company of the area at the time.
  • One lode claim on the east slope of Upper Lost Parks, an appendage of Elk Ridge just north of Natural Bridges National Monument and south of the Woodenshoe formation. It’s across Deer Creek Canyon from Kimmerle’s Geitus and Cedar claims, which the firm staked just before President Barack Obama designated Bears Ears, and right after President Donald Trump shrunk the monument for the first time. It’s also in the vicinity of the Sandy claims that Kimmerle held, but that [those?] were closed in 2015. The area was mined and prospected heavily during the Cold War. The nearest historical mines and prospects were the Big Red, the Sandy, and the Hideout. In 1977, the Big Red — operated by Utah Power & Light — was reported to have a flooded, a caved, and an open adit. While the Hideout sparked a 1950s prospecting boom in the area, none of these were ever large producers. However, a 1965 USGS report did indicate this part of Elk Ridge was favorable for uranium deposits, which is likely one reason the Trump administration stripped it of national monument protections.

The White Canyon area was known to contain rich uranium reserves back in the 1940s and 1950s, but its remoteness and the rugged landscape created challenges for mining companies looking to exploit the resources. One of the biggest hurdles was getting the ore to the Monticello processing plant, which required driving gnarly roads across the crinkled landscape and up and over Elk Ridge.

So in 1949, the Vanadium Corporation of America built a small mill at the confluenceof White Canyon and the Colorado River, primarily to process uranium ore from the nearby Happy Jack Mine, located upstream in the White Canyon drainage (and just within the original Bears Ears National Monument boundaries). For the next four years, the mill went through about 20 tons of ore per day, crushing and grinding it up, then treating it with sulfuric acid, tributyl phosphate, and other nastiness. One ton of ore yielded about five or six pounds of uranium, meaning that each day some 39,900 pounds of tailings were piled up outside the mill on the banks of the river.

In 1953 the mill was closed, and the tailings were left where they sat, uncovered, as was the practice of the day. Ten years later, water began backing up behind the newly built Glen Canyon Dam; federal officials decided to let the reservoir’s waters inundate the tailings. There they remain today, though at current lake levels they are probably buried by and mixed in with the Dominy Formation of silt, rather than covered with water.

Satellite image showing the location of the White Canyon Mill and its silt-entombed tailings pile.

During the uranium days of the West, more than a dozen mills — all with processing capacities at least ten times larger than the one at White Canyon — sat on the banks of the Colorado River and its tributaries. Mill locations included: Shiprock, Mexican Hat, Monument Valley, Tuba City, Monticello, Rifle, Grand Junction, Moab, Uravan, Green River, and Naturita. There was even an ore upgrading mill at Fry Canyon, followed by a copper heap leaching operation. Groundwater contamination continues to today, and was partially responsible for the Fry Canyon Lodge’s demise.

At the Durango mill the tailings were piled into a hill-sized mound just a stone’s throw from the Animas River. They weren’t covered or otherwise contained, so when it rained tailings simply washed into the river. Worse, the mill’s liquid waste stream poured directly into the river at a rate of some 340 gallons per minute, or half-a-million gallons per day. It was laced not only with highly toxic chemicals used to leach uranium from the ore and iron-aluminum sludge (a milling byproduct), but also radium-tainted ore solids.

Radium is a highly radioactive “bone-seeker.” That means that when it’s ingested it makes its way to the skeleton, where it decays into other radioactive daughter elements, including radon, and bombards the surrounding tissue with alpha, beta, and gamma radiation. According to the Toxic Substances and Diseases Registry, exposure leads to “anemia, cataracts, fractured teeth, cancer (especially bone cancer), and death.”

It wasn’t any better at any of the other mills. In the early 1950s, researchers from the U.S. Public Health Service sampled Western rivers and found that “the dissolved radium content of river water below uranium mills was increased considerably by waste discharges from the milling operations” and that “radium content of river muds below the uranium mills was 1,000 to 2,000 times natural background concentrations.”

That was just from daily operations. In 1960, one of the evaporation ponds at the Shiprock mill broke, sending at least 250,000 gallons of highly acidic raffinate, containing high levels of radium and thorium, into the river. None of the relevant officials were notified and individual users continued to drink the water, put it on their crops, and give it to their sheep and cattle. It wasn’t until five days later, after hundreds of dead fish had washed up on the river’s shores for 60 miles downstream, that the public was alerted to the disaster.

Of course, what’s dumped into the river at any of these places doesn’t stay there, but makes its way downstream. In the early 1960s, while Glen Canyon Dam was still being constructed, the Public Health Service folks did extensive sediment sampling in the Colorado River Basin, with a special focus on Lake Mead’s growing bed of silt, which had been piling up at a rate of 175 million tons per year after Hoover Dam started impounding water in 1935. The Lake Mead samples had higher-than-background levels of radium-226. The report concludes:

And so, the billions of tons of silt that has accumulated in Lake Mead and Lake Powell serve as archives of sorts. They hold the sedimental records of an era during which people, health, land, and water were all sacrificed in order to obtain the raw material for weapons that are capable of destroying all of humanity. If the new mining claim mini-rush is any indication, some more records may be added to the archive before long.

📸 PARTING SHOT 🎞️

There’s snow in them thar hills!

There’s snow on the peaks just as the aspens are peaking around Silverton, Colorado. Sept. 23, 2026. Andy Gleason photo.

1 This also appears on some maps and documents as Frey #4. In fact, many of the “Fry”s in the Fry Canyon area show up as “Frey” on older maps (while some still say “Fry.”). Oh my oh my I don’t know why it’s Frey or Fry.

Riverfront dining in southern Utah — Zak Podmore

Opening the black box: in situ imaging of arbuscular mycorrhizal fungal structures in soil using synchrotron-based micro-CT — Henri M. Braunmiller, Michael Bitterlich, Nicolai Koebernick, Eva Jacob, Anna S. Heck, Andrea Schnepf, Johanna Pausch, Jussi-Petteri Suuronen, Bernhard Hesse, Sylvain Delzon, Jonathan Perrin, Andrew King, Jan Jansa, Mutez A. Ahmed (New Phytologist)

Fig. 7 Grayscale images and segmentations of intraradical arbuscular mycorrhizal fungal (AMF) structures in Rhizophagus irregularis-colonized Solanum lycopersicum (cv 76R) roots. In the images, segmented materials include roots (in green), hyphae (pink), vesicles (light pink), arbuscules (white), a spore (purple, round shape at the bottom right), and air (light blue). Upper panel, cross section through a colonized root: (a) 2D grayscale slice showing intraradical structures; (b) corresponding 2D-segmentation; and (c) violin plot with horizontal median line of the gray value distributions of different tissues. Lower panel, longitudinal positioning of AMF structures: (d) Computed microtomography grayscale image showing extraradical hyphae and bright arbuscules (red arrows) in the underlying root cortex; (e) 3D segmentation of arbuscules and intraradical hyphae within the same 600-lm root segment; (f) same 3D segmented arbuscules in the root cortex in soil (extraradical soil structures have been left gray)

Click the link access the report on the New Phytologist website (Henri M. Braunmiller, Michael Bitterlich, Nicolai Koebernick, Eva Jacob, Anna S. Heck, Andrea Schnepf, Johanna Pausch, Jussi-Petteri Suuronen, Bernhard Hesse, Sylvain Delzon, Jonathan Perrin, Andrew King, Jan Jansa, Mutez A. Ahmed). Here’s the summary:

Summary

  • Arbuscular mycorrhizal fungi (AMF) contribute to plant nutrient and water uptake via their extraradical hyphal networks. However, in situ methodologies to quantify architectural and morphological traits of these networks in soil are largely lacking, limiting our understanding of AMF-mediated resource transport.
  • Using synchrotron-based X-ray computed microtomography (micro-CT), we established a workflow to cultivate, noninvasively image, and quantitatively analyze AMF hyphosphere and rhizosphere structures in the interaggregate space across two soil textures and biological contexts.
  • We developed a pipeline for quantitative three-dimensional (3D) assessment of key architectural and morphological traits including structure counts, hyphal length, branching frequency, volume, and surface area. Our method further permits (1) measurement of AMF–soil and AMF–root interface areas and (2) microscale quantification of pore space occupancy by AMF.
  • Micro-CT offers a tool for noninvasively visualizing AMF in air-filled soil pore space. We outline how such quantitative 3D information can be incorporated into image-based and functional-structural soil–plant models, thereby supporting a better mechanistic understanding of AMF-mediated processes in soils and plants

Arbuscular mycorrhizal fungi (AMF) may enhance host plant access to soil nutrients and hence contribute to global food security and nutrition (Antunes et al., 2012; Rodriguez & Sanders, 2015; Thirkell et al., 2020). These fungi can supply noticeable proportions of essential plant nutrients, including phosphorus, nitrogen, zinc, and copper (Marschner & Dell, 1994). In addition, numerous studies showed that AMF improve plant water uptake, particularly under dry soil conditions (e.g. Bitterlich et al., 2018; Kakouridis et al., 2022; Abdalla et al., 2023), suggesting a potentially increasing contribution to plant performance under future climate scenarios. A proposed mechanism for AMF-mediated enhancement of water and nutrient acquisition involves the formation of extensive extraradical hyphal networks (Kokkoris, 2026). These networks increase the absorptive surface area and enlarge the effective root radius (Abdalla & Ahmed, 2021), growing beyond depletion zones and thus facilitating access to yet undepleted soil (Schnepf et al., 2008). The degree to which AMF improve plant water and nutrient uptake likely depends on the architecture and morphology of their hyphal network, including hyphal length, diameter, and connectivity among individual hyphae, roots, and soil particles (Abdalla & Ahmed, 2021; Kakouridis et al., 2022). Thus, for a better mechanistic understanding of the role of AMF on water and nutrient transport, characterization of hyphal network structure in soil is indispensable.

Click the link to read Fungi Are Holding the Food Web Together. New Research Images This Underground Network on the EOS website (Emily Gardner). Here’s an excerpt:

September 29, 2026

More than 80% of plants on Earth partner with mycorrhizal fungi to extract nutrients from soil. Underground, in a zone of soil known as the rhizosphere, these fungi grow into vast networks of tubular cells called mycelium (individual cells are called hyphae). These tiny hyphae—about one tenth to one hundredth the width of a human hair—can gather nutrients in the soil and send them into plants. If plants don’t get enough nutrients, neither do the animals that depend on them or the animals that depend on those animals. Furthermore, some research has suggested that mycorrhizal fungi absorb the equivalent of 13 billion tons of carbon dioxide annually. All of this makes the rhizosphere essential to the health of our planet and its inhabitants.

“Basically everyone on Earth is dependent on this really, really tiny zone around roots, in a way,” said Henri Braunmiller, a soil ecologist and graduate student at the Technical University of Munich.