Recent breakthroughs suggest that hydrogen reservoirs are buried in countless regions of the world, including at least 30 U.S. states.

Finding such reservoirs could help accelerate a global energy transition, but until now, geologists only had a piecemeal understanding of how large hydrogen accumulations form — and where to find them.

“The game of the moment is to find where it has been released, accumulated and preserved,” Chris Ballentine, a professor and chair of geochemistry at the University of Oxford and lead author of a new review article on hydrogen production in Earth’s crust, told Live Science in an email.

Ballentine’s new paper starts to answer those questions. According to the authors, Earth’s crust has produced enough hydrogen over the past 1 billion years to meet our current energy needs for 170,000 years. What’s still unclear is how much of that hydrogen could be accessed and profitably extracted.

In the new review, published Tuesday (May 13) in the journal Nature Reviews Earth and Environment, the researchers draw up an “ingredient” list of geological conditions that stimulate the creation and build-up of natural hydrogen gas belowground, which should make it easier to hunt for reservoirs.

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“The specific conditions for hydrogen gas accumulation and production are what a number of exploration companies (e.g. Koloma, funded by a consortium led by Bill Gates Breakthrough Energy fund, Hy-Terra funded by Fortescue, and Snowfox, funded by BP [British Petroleum] and RioTinto) are looking at carefully and this will vary for different geological environments,” Ballentine said.

Natural hydrogen reservoirs require three key elements to form: a source of hydrogen, reservoir rocks and natural seals that trap the gas underground. There are a dozen natural processes that can create hydrogen, the simplest being a chemical reaction that splits water into hydrogen and oxygen — and any type of rock that hosts at least one of these processes is a potential hydrogen source, Ballentine said.

“One place that is attracting a lot of interest is in Kansas where a feature called the mid continental rift, formed about 1 billion years ago, created a huge accumulation of rocks (mainly basalts) that can react with water to form hydrogen,” he said. “The search is on here for geological structures that may have trapped and accumulated the hydrogen generated.”

Based on knowledge of how other gases are released from rocks underground, the review’s authors suggest that tectonic stress and high heat flow may release hydrogen deep inside Earth’s crust. “This helps to bring the hydrogen to the near surface where it might accumulate and form a commercial resource,” Ballentine said.

Within the crust, a wide range of common geological contexts could prove promising for exploration companies, the review found, ranging from ophiolite complexes to large igneous provinces and Archaean greenstone belts.

An ophiolitic landscape in Italy’s Sondrio province. The rocks are rich in iron, which gives them a reddish-brown color. (Image credit: Michele D’Amico supersky77/Getty Images)

Ophiolites are chunks of Earth’s crust and upper mantle that once sat beneath the ocean, but were later thrust onto land. In 2024, researchers discovered a massive hydrogen reservoir within an ophiolite complex in Albania. Igneous rocks are those solidified from magma or lava, and Archaean greenstone belts are up to 4 billion-year-old formations that are characterized by green minerals, such as chlorite and actinolite.

The conditions discussed in the review are the “first principles” for hydrogen exploration, study co-author Jon Gluyas, a professor of geoenergy, carbon capture and storage at Durham University in the U.K., said in a statement. The research outlines the key ingredients that companies should consider when developing their exploration strategies, including processes through which hydrogen might migrate or be destroyed underground.

“We know for example that underground microbes readily feast on hydrogen,” co-author Barbara Sherwood Lollar, a professor of Earth sciences at the University of Toronto, said in the statement. So environments where bacteria could come in contact with hydrogen-producing rocks may not be great places to look for reservoirs, Sherwood Lollar said.

Hydrogen is used to make key industrial chemicals such as methanol and ammonia, which is a component in most fertilizers. The gas could also aid the transition away from fossil fuels, as hydrogen can power both cars and power plants.

But hydrogen today is produced from hydrocarbons, meaning manufacture of the gas comes with huge carbon emissions. “Clean” hydrogen from underground reservoirs has a much smaller carbon footprint, because it occurs naturally.

Earth’s crust produces “plenty of hydrogen,” Ballentine said, and it is now a question of following the ingredient list to find it.

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