Scientists map where orphan wells pose threats to aquifers
Cliff Simmons, an oil and gas inspector supervisor for the Pennsylvania Dept. of Environmental Protection, points a methane sensor at an abandoned well on the Murrysville property of Pamela and Ivan Schrank on Thursday, March 28, 2024. Simmons visited the well site with other DEP officials, journalists and Rep. Summer Lee (PA-12). (Steve Mellon/Pittsburgh Union Progress)
This article originally appeared on Inside Climate News, a nonprofit, non-partisan news organization that covers climate, energy and the environment. Sign up for their newsletter here.
For the first time, scientists have mapped groundwater variables nationally to understand which aquifers are most vulnerable to contamination from orphan wells.
Oil and gas wells with no active owner that are no longer producing and have not been plugged are considered orphan wells. These unplugged wells can create pathways for contaminants like hydrocarbons and brine to migrate from the oil and gas formation into groundwater zones. Plugging a well seals off these potential pathways.
USGS scientists Joshua Woda, Karl Haase, Nicholas Gianoutsos, Kalle Jahn and Kristina Gutchess published a geospatial analysis of water-quality threats from orphan wells this month in the journal Science of the Total Environment. They found that factors including large concentrations of orphaned wells and the advanced age of wells make aquifers in Appalachia, the Gulf Coast and California susceptible to contamination.
Using a USGS dataset of 117,672 documented orphan wells nationwide, the researchers found that 54 percent of the wells are within aquifers that supply 94 percent of groundwater used nationally.
'No matter where you live across the nation, you can go look at what's happening in your backyard, how your aquifers compare to other aquifers and what the threats are,' said Gianoutsos.
The researchers mapped the locations of orphaned wells over principal and secondary aquifers using Geographic Information Systems datasets. They then analyzed the aquifers based on factors that could contribute to vulnerability to groundwater contamination, such as the average age of the orphan wells.
Older wells were subject to less regulation and are more prone to failure. The authors found that Pennsylvanian aquifers, which span several Appalachian states including Pennsylvania, present the 'maximum confluence' of risk factors. The first oil wells in the country were drilled in Pennsylvania. Orphan wells can be over 100 years old and located near coal seams and residential water wells.
The Gulf Coast aquifers, including the Coastal Lowlands aquifer system, which stretches from Texas to the Florida Panhandle, were found to be susceptible in part because wells are located in areas like wetlands and open water that are more prone to contamination.
The analysis also considered the rates of pumping from each aquifer. That led them to the California Coastal aquifers and the Central Valley, where a high density of old orphan wells overlaps with highly urbanized areas and intensive groundwater use for agriculture.
The researchers found that the Ada-Vamoosa aquifer, in central Oklahoma, has the highest concentration of orphan wells per square mile of any principal aquifer in the country.
The authors note the paper is not an analysis of the amount of groundwater contamination from orphan wells or the number of leaking orphan wells. But they suggest that policymakers and researchers could use it as a basis to target aquifers for additional investigation.
'This could be a good starting point if someone wanted to do a local investigation,' said Woda.
Gianoutsos noted that the active list of orphan wells is changing as research into orphan wells and well plugging advances. He said some 40,000 orphan wells have been added to the national list since their dataset was created. Another approximately 10,000 orphan wells have been plugged in that time.
'The threats are still there,' he said. 'Just as we discover more wells, we discover additional threats.'
The research was part of the U.S. Department of the Interior Orphaned Wells Program Office through the Bipartisan Infrastructure Law.
Orphan wells have been linked to groundwater contamination in states including Pennsylvania, Ohio and Texas. A 2011 Ground Water Protection Council study found that orphan wells caused 41 groundwater contamination incidents in Ohio between 1983 and 2007. The study found orphan wells and sites caused 30 groundwater contamination incidents in Texas between 1993 and 2008.
The Pennsylvania Department of Environmental Protection (DEP) has reported several recent cases of orphan wells contaminating groundwater. An orphan well in Vowinckel in Clarion County contaminated a family's drinking water before it was plugged last year, according to the DEP. Another orphan well in Shinglehouse, in Potter County, was plugged by DEP in 2024 with emergency funds after a homeowner reported contamination of their water well.
John Stolz, a professor of environmental microbiology at Duquesne University in Pittsburgh, has researched how fluids from oil and gas wells can migrate underground with unintended consequences.
Stolz said some of the wells in Pennsylvania are so old they were cased with wood or metal, unlike the cement that has been standard for decades. He said the wooden casings have often deteriorated completely. He said conventional drilling and more recent fracking have left much of Pennsylvania 'looking like Swiss cheese.'
'It's good to see a study that focuses on the water resources,' he said in response to the USGS study. 'We are going to have greater periods of drought, and these water resources are going to become far more valuable.'
Stolz is studying a 'frack-out' in the town of New Freeport in southwestern Pennsylvania. An unconventional well being fracked communicated with an orphan well over 3,000 feet away, forcing fluids to the surface. Residents of the town resorted to drinking bottled water, according to NBC News.
'The industry refuses to admit this stuff happens,' he said. 'The reality is it happens on a somewhat regular basis.'
Hashtags

Try Our AI Features
Explore what Daily8 AI can do for you:
Comments
No comments yet...
Related Articles


USA Today
6 hours ago
- USA Today
The Big One: Is California 'overdue' for a devastating major earthquake?
The Big One: Is California 'overdue' for a devastating major earthquake? A near-certain disaster looms for California, but there are real things people can do to prepare. Here's what to know about the risks. Show Caption Hide Caption California governor signs emergency declaration after quake California's governor says "we're concerned about damage" from magnitude 7 earthquake." It's the unavoidable series of questions Christine Goulet gets every time she's asked what she does for a living. "When is the next big earthquake coming? Do you know where? When should we get ready?" Goulet, director of the U.S. Geological Survey's Earthquake Science Center in Los Angeles, told USA TODAY. "It's almost without fail once they know I study earthquakes. If I received a dollar every time I'm asked, I'd be rich." Goulet has answers, but she can't predict the future. The ominous truth: The Big One could happen any time, and there's more than one possible "Big One." "It's gonna happen. An earthquake could be in a matter of minutes, the next hour, tomorrow, or in a week from now, we can't predict that precisely at this time. We don't know," Goulet said. "But the point in general is we want and need to prepare for them." 'Swaying back and forth': Magnitude 7 earthquake, aftershocks rock California The most authoritative research on the risk to California was conducted in 2015, but little has changed in the past decade. The state will almost certainly face a magnitude 6.7 or larger earthquake within the next three decades, the USGS concludes. Some of the most at-risk locations are San Francisco and Los Angeles. California's continuous temblor risk coincides with a huge earthquake brewing along the Cascadia Subduction Zone off the coast of the Pacific Northwest. San Francisco Bay Area faces high chances of getting a Big One With nearly four dozen faults in the region stretching from Napa to Monterey, the San Francisco Bay Area has a 72% chance of a major quake registering 6.7 magnitude or higher by 2043, USGS researchers previously estimated. The findings also indicate that the Bay Area has a 51% chance of experiencing an earthquake with a magnitude of 7 and a 20% chance of measuring a magnitude of 7.5 or higher within that time frame. "The earthquake threat is very real," said Richard Allen, a professor at the University of California, Berkeley and the director of the Berkeley Seismology Lab. "It is a real challenge as we have to take that long-term view, but also not to live our lives in fear." In December, thousands in the Bay Area and across Northern California were worried after a magnitude 7 earthquake struck along a sparsely populated northern coast of California, triggering a tsunami warning across a swath of the West Coast stretching from southern Oregon to San Francisco. Traci Grant, 53, a public relations specialist who felt the quake in San Francisco, told USA TODAY at the time she felt her retrofitted apartment move in slow motion. "It just kept going and going," Grant said. "It was scary and a bit exciting at the same time. It was more of a roll than just shake, shake, shake." Fragile environment: A collapsing glacier destroyed a Swiss village. Is climate change to blame? Less than two hours after the initial quake, some areas experienced 13 different aftershocks, ranging from 5.1 to 3.1, the USGS reported. Two hours after that, at least 39 aftershocks of at least a 2.5 magnitude occured in the region, authorities said. No earthquake-related injuries or major damages were reported. Goulet said if the quake had been directly on land, "the impact would've been more devastating." Goulet said December's quake magnitude conjured up the Great San Francisco Earthquake and Fire of 1906. It was a nearly minute-long 7.9 magnitude quake followed by a fire that burned for three days, destroying thousands of buildings. The San Francisco quake killed an estimated 3,000 people and destroyed roughly 80% of the city. It is known as one of the deadliest in U.S. history. Allen also noted the 1868 Hayward Fault earthquake that struck the heart of the Bay Area and killed 30 people. With all the Bay Area faults, Allen said his research shows there's a "two-in-three chance" the Big One could be soon. "We're overdue for a recurrence," Allen said. The last major earthquake in the Bay Area occurred more than a decade ago, when an earthquake rattled Napa Valley in 2014. The 6.0 magnitude quake in Wine Country killed one person and injured 300 people. The incident caused more than $1 billion in damage across Napa and neighboring cities, including Vallejo, California, which took years to rebuild. Then there was the Loma Prieta earthquake that rocked the San Francisco Bay Area in 1989, killing 63 people and injuring nearly 3,800 others. The earthquake disrupted the World Series and damaged the Bay Bridge, Oakland's Cypress Freeway, and swaths of San Francisco. It caused up to $10 billion in damage. "There's this perception that large quakes are frequent, but actually, they are quite rare," Goulet said. "We just don't know when they will happen." Los Angeles is ripe for a Big One as well The Los Angeles area also stands a chance of getting a major earthquake, as there's a 60% chance of a 6.7 magnitude quake within the next 30 years, the USGS said. Additionally, there is also a 46% probability that a 7.0 magnitude earthquake will hit L.A. and a 31% chance a 7.5 magnitude quake will strike during that same period. Allen, the Berkeley seismologist, said Southern California has just as high an earthquake risk compared to its Northern California counterparts. "They face a similar threat, if not higher," Allen said. Goulet added that with Los Angeles and the surrounding areas being so populous (nearly 18.6 million residents according to California Finance Department statistics), there is a high probability for major destruction. She cites the disastrous 6.7 earthquake in Northridge, California, in 1994, which killed 60 people and injured more than 7,000. The devastation also left thousands of buildings and structures collapsed or damaged across Los Angeles, Ventura, Orange and San Bernardino counties. Thousands of residents became homeless as the aftermath caused between $13 billion to $20 billion in damages. "The closer an earthquake is to a large population, the greater the impact will be," Goulet said. Goulet also points to a sequence of earthquakes in 2019 in Ridgecrest, California. A 7.1 magnitude earthquake rattled the city two days after an initial 6.4 magnitude quake. Goulet was among a USGS on-site team researching the first quake when, surprisingly, the second temblor struck. "It was terrifying," Goulet said. "We were there taking measurements and just as we were finishing our work and planning for the next day, the second one occurred about six miles away from us. That was extremely close." Goulet said she remembers reassuring panicked residents that everything would be okay. "That's why we cannot specifically predict earthquakes, when and where they will occur and how big they will be," Goulet added. "But what we can do is collect all of the research that causes earthquakes and the probabilities, which are called probabilistic seismic hazard analysis." Now what?: Federal database that tracked costly weather disasters no longer being updated How to prepare for an earthquake disaster Huge earthquakes have long been an existential crisis for millions along the West Coast, as described in a 2022 USA TODAY article. But experts said there are real things people can do to help them prepare for a major disaster. If you experience an earthquake, Sarah Minson, a research geophysicist with the USGS's Earthquake Science Center in Mountain View, California, advises not to run. "If you feel shaking, you should drop, cover and hold on to protect yourself," Minson said. "Don't go anywhere. Don't run outside. A huge number of the injuries that occur in earthquakes are people stepping on broken glass or trying to run during the shaking and falling down." Allen, the Berkeley seismologist, recommends that households create an earthquake plan, including where they will meet and possibly have a bag or suitcase ready for at least a couple of days. Residents will at least want a flashlight and a way to charge their phone. They should also be prepared to have access to electricity or water cut off for days or weeks. Here are a few practical tips: When trying to use your phone, text – don't call. In a disaster, text messages are more reliable and strain cell networks less. To power your phone, you can cheaply buy a combination weather radio, flashlight and hand-crank charger to keep your cell running even without power for days. A cash reserve is good to have, USGS seismologist Lucy Jones previously said. You'll want to be able to buy things, even if your credit card doesn't work for a time. Simple things like securing bookshelves can save lives. Downloading an early warning app can give you precious moments to protect yourself in the event of a big quake. Buying earthquake insurance can protect homeowners. And taking part in a yearly drill can help remind you about other easy steps you can take to prepare. Contributing: Elizabeth Wiese and Joel Shannon

Yahoo
3 days ago
- Yahoo
Steam and debris erupt again at Yellowstone thermal pool, webcam shows
A small hydrothermal eruption was captured on camera at Yellowstone National Park last weekend at the same site where a massive explosion destroyed a section of boardwalk last summer. According to the U.S. Geological Survey, the eruption occurred at 8:39 p.m. local time on Saturday, May 31, at Black Diamond Pool in Biscuit Basin, just north of Old Faithful. It was recorded by a newly installed webcam set up on May 14 to monitor activity at the site. "It is likely that these small eruptions are a result of the hydrothermal plumbing system for the pool adjusting after the major disruption of the larger explosion last summer," USGS Scientist-in-Charge Michael Poland told USA TODAY. Hydrothermal explosions occur when superheated water rapidly turns to steam underground, triggering sudden bursts of steam, rock and debris. The July 2024 explosion at the same pool scattered boulders, destroyed nearby infrastructure and altered the shape of the pool itself. No injuries were reported. As of June 3, the parking lot and boardwalk at Biscuit Basin remain closed due to continued risk of hydrothermal activity.

Associated Press
3 days ago
- Associated Press
Troy Minerals Reports Drilling Results from the Lake Owen Project, Wyoming
Show 240.73 meters of Critical Metal Mineralization, Iron, Titanium, Vanadium, Scandium and Gallium VANCOUVER, BC / ACCESS Newswire / June 4, 2025 / Troy Minerals Inc. ('Troy' or the 'Company') (CSE:TROY)(OTCQB:TROYF)(FSE:VJ3) is pleased to announce that complete results from Hole LO24-01 show strong critical metal mineralization over continuous 240.73 meters (from 10.67 meters to 251.40 meters) from its maiden drilling program on its 100% owned Lake Owen Project (the 'Project'), located 50 km southwest of Laramie, Wyoming, USA (see Figures 1,2). The Project is a Proterozoic layered mafic intrusion complex historically explored for Platinum Group Elements (PGE). Similar to the Stillwater Complex in the USA and the Merensky Reef of South Africa, the Lake Owen Complex shows strong potential for vanadium, titanium, PGE, and associated metals. In late 2024, the Company drilled two diamond holes totaling 607.77 meters near the southwestern claims' boundary (see Figure 3), marking Troy Minerals' first drill holes on the Project. These holes targeted titanium (TiO2) and vanadium (V2O5) mineralization linked with magnetite in gabbro, as well as reef-style PGE mineralization (see Company News Release dated February 28, 2025). A first pass of selective sampling of the drill holes had been carried out and demonstrated presence of anomalous titanium and vanadium mineralization. Elevated values of vanadium are correlative with the titanium. Sampling was selected to assess various lithological units and all zones with magnetite content up to 15-20% and/or visible sulfide mineralization. Magnetite content in the gabbro in hole LO24-01 is consistently about 5-10%. In LO24-01, the initially limited sampling suggested a large zone of titanium and vanadium-enrichment and higher relative values correlate well with the green gabbro. Associated with these anomalous zones have been elevated concentrations of scandium. Based on these initial results, additional infill sampling through all prospective lithologies was carried out by Company personnel in January, 2025. Results exhibit robust critical metal mineralization over 240.73 meters in hole LO24-01, including: Concurrent with Company infill sampling, geologists from the USGS and Wyoming State Geological Survey (WSGS) collected samples for Whole Rock, Major Oxides, and thin section analyses. Results of the USGS and WSGS work are pending. 'Our recent geological and geophysical findings, coupled with promising initial drilling results, are significantly enhancing our confidence in the Lake Owen Project. Each new insight reinforces our belief that this project deserves a robust exploration budget in the near future.' Said Yannis Tsitos, President of Troy. 'Beyond the historically recognized high grades of iron, titanium, and vanadium, the recent discovery of scandium and gallium-critical metals essential for applications in metal alloys, military and civil aviation, semiconductors, electric vehicles, and solar panels-underscores the project's immense potential for both our Company and the State of Wyoming in USA. We are committed to maximizing shareholder value through strategic development plans for Lake Owen, alongside our silica and rare earth element (REE) initiatives.' Table 1: Drill hole specifications Drill hole LO24-01 was designed to test the extent of the Lower Mag Gabbro down to the basement contact. Drilling revealed a series of interlayered magnetic gabbro and a distinctive coarse-grained green gabbro. The green coloration is imparted by pyroxenes altering to chlorite. These layers are generally constrained to widths of less than 4 metres. Table 2: Drill hole LO24-01 intersections 1: All intersections lengths are drill indicated thicknesses; insufficient work has been completed to reliably determine true thicknesses. 2: Elemental geochemical analyses were converted to oxides using following conversion factors Titanium - 1.6681, Vanadium - 1.7852, Iron - 1.2865, Scandium - 1.5338, Gallium - 1.3442 Drill hole LO24-02 intersected gabbroic units that are weakly magnetic and contain no anomalous values of titanium, vanadium, or scandium. This drill hole was collared deeper in the sequence than hole LO24-01; further down dip and stratigraphically lower in the Lower Mag Unit. Drill core was detail logged and sampled by Company staff. Core was split by saw with samples sent to ALS Global's laboratory in Reno, NV for preparation and analysis. Samples were analyzed for multi-elements (ME-MS61). The Company's quality control monitoring consisted of inserting certified reference and blank material in the sample stream. No quality control issues were identified. Only a very small portion of the Lake Owen Complex and therefore our Claims has been drill-tested to date. As currently mapped, the prospective Lower Mag Gabbro unit continues along strike to the west. The Company has yet to drill test the stratigraphically higher Upper Mag Gabbro. Surface mapping and sampling in 2023 identified two massive magnetite rock samples that returned 8.812% TiO2 and 0.548% V2O5, and 15.505% TiO2 and 0.586% V2O5 respectively (Figure 5). These represent priority drill targets for 2025. An historical drill hole was completed here not by Troy, but there was no assessment of titanium, vanadium, or scandium. Troy Minerals is planning its summer fieldwork for the Lake Owen Project. After analyzing airborne geophysical data, as reported in the May 21, 2025 news release, Troy will collect soil samples and conduct geological mapping and sampling. The aim is to refine drill targets for the 2026 season, including a relevant drilling pads application. Qualified Person The information contained in this news release has been reviewed and approved by Ted Vander Wart, a consultant to the Company, who is a qualified person as defined under National Instrument 43-101. About Troy Minerals Troy Minerals is a Canadian based publicly listed mining company focused on building shareholder value through acquisition, exploration, and development of strategically located 'critical' mineral assets. Troy is aggressively advancing its projects within the silica (silicon), vanadium, and rare earths industries within regions that exhibit high and growing demand for such commodities, in both North America and Central-East Asia. The Company's primary objective is the near-term prospect of production with a vision of becoming a cash-flowing mining company to deliver tangible monetary value to shareholders, state, and local communities. ON BEHALF OF THE BOARD, Rana Vig | CEO & Director Telephone: 604-218-4766 Email: [email protected] Forward-Looking Statements Statement Regarding Forward-Looking Information: This release includes certain statements that may be deemed 'forward-looking statements'. All statements in this release, other than statements of historical facts, that address events or developments that Troy Resources Inc. (the 'Company') expects to occur, are forward-looking statements. Forward-looking statements are statements that are not historical facts and are generally, but not always, identified by the words 'expects', 'plans', 'anticipates', 'believes', 'intends', 'estimates', 'projects', 'potential' and similar expressions, or that events or conditions 'will', 'would', 'may', 'could' or 'should' occur. Although the Company believes the expectations expressed in such forward-looking statements are based on reasonable assumptions, such statements are not guarantees of future performance and actual results may differ materially from those in the forward-looking statements. Factors that could cause the actual results to differ materially from those in forward-looking statements include results of exploration activities may not show quality and quantity necessary for further exploration or future exploitation of minerals deposits, volatility of commodity prices, and continued availability of capital and financing, permitting and other approvals, and general economic, market or business conditions. Investors are cautioned that any such statements are not guarantees of future performance and actual results or developments may differ materially from those projected in the forward-looking statements. Forward-looking statements are based on the beliefs, estimates and opinions of the Company's management on the date the statements are made. Except as required by applicable securities laws, the Company undertakes no obligation to update these forward-looking statements in the event that management's beliefs, estimates or opinions, or other factors, should change. The Canadian Securities Exchange has not reviewed this press release and does not accept responsibility for the adequacy or accuracy of this news release. SOURCE: Troy Minerals Inc. press release