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Mars Wasn’t Just Ice: Curiosity Rover Identifies Wind-Shaped Wave Marks Proving the Existence of Open Lakes 3.7 Billion Years Ago and Transforming What Science Knew About the Planet’s Past

Published on 05/01/2026 at 17:09
Rover Curiosity ao lado de um lago de água líquida em Marte, em terreno avermelhado, representando evidências científicas de lagos abertos no passado do planeta.
Ilustração mostra o rover Curiosity analisando um antigo lago de água líquida em Marte, evidência de que o planeta teve ambientes abertos e sem gelo há bilhões de anos.
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Unique Discovery Shows That Mars Had Shallow Lakes Without Ice on The Surface, Shaped by The Wind and Supported by A Denser Atmosphere Than Previously Thought

For decades, scientists debated whether primitive Mars was merely a frozen world, with water trapped under layers of ice, or whether it ever hosted real lakes of liquid water exposed to the atmosphere. Now, a new scientific discovery helps to settle this discussion. Tiny marks preserved in Martian rocks indicate that shallow, ice-free lakes existed about 3.7 billion years ago, being directly shaped by the action of the wind.

This information was disclosed by Science Advances, according to an article published on the Science.org, based on observations made by the Curiosity rover, from NASA. The evidence was found in Gale Crater, a region near Mars’ equator where the robot has been exploring since 2012. According to the researchers, this is the clearest evidence ever identified of liquid water exposed to the air on the ancient Martian surface.

Symmetrical Ripple Marks (A) are observed on the outcrop AMB. The crests of the ripples are identified by yellow arrows (A) and are almost vertically aligned (white arrow) in successive layers of ripples. The internal laminations can be continuously traced across the valleys of the ripples. In the plan view (B), the crests of the ripples are linear, with occasional forked bifurcations, consistently oriented in the northwest/southeast (NW/SE) direction. The set of ripples of the AMB exhibits great lateral extent, uniform thickness, and is concordantly covered by a flat laminating unit [(C): the contact is covered at this point — the dashed line indicates an inferred contact]. The ripple unit of the AMB in the Amapari region is approximately 15 cm thick and is composed of five resistant layers containing symmetrical ripple marks. Image Credit: NASA/JPL-Caltech/MSSS.

These formations, called “wave ripples”, function as a true geological diary. They form when the wind blows over water, creating small waves that move sandy sediments on the bottoms of shallow lakes. Over time, these patterns are recorded in the rock, preserving detailed information about the environment in which they arose.

Microscopic Waves Function as Climate Record of Ancient Mars

The researchers identified two distinct sets of ripples in rocky outcrops of Gale Crater. The first was photographed in 2022, in an area nicknamed Prow, while the second appeared in a nearby band known as Amapari Marker Band. Both locations point to different episodes when liquid water accumulated, instead of remaining frozen.

The ripples are extremely small: about six millimeters high, with an average spacing of four to five centimeters. These details are crucial for scientific interpretation. On Earth, ripples of this size only form in environments with shallow water and gentle waves, indicating relatively calm lakes.

Using computational models, researcher Michael Lamb, co-author of the study, estimated that these lakes were less than two meters deep, approximately the height of a person. According to geologist Claire Mondro, leader of the research at the California Institute of Technology (Caltech), “the shape of these ripples can only be explained by liquid water exposed to the atmosphere and influenced by the wind.”

Moreover, the symmetrical pattern of the marks reinforces that wind, sediment, and liquid water acted simultaneously, which is impossible in completely frozen environments. Therefore, the study describes these structures as “the most definitive examples of wave ripples ever found on another planet”.

Thicker Atmosphere and Warmer Climate Sustained Martian Lakes

Currently, Mars is a cold, dry planet shrouded in an extremely thin atmosphere. Under these conditions, liquid water cannot remain stable on the surface, evaporating or freezing quickly. However, the ripples found indicate that, in the distant past, the planet had a thicker atmosphere and higher temperatures, at least for prolonged periods.

This point is crucial for planetary climate models. For years, scientists have debated whether Mars experienced short episodes of warming or maintained relatively stable conditions capable of sustaining liquid water over long intervals. The new evidence favors the latter hypothesis, expanding the timeframe in which Mars could have been a habitable environment.

According to Mondro, “extending the period during which liquid water was present significantly increases the possibilities for microbial habitability throughout Mars’s history.” Although water is not a guarantee of life, it is considered an essential prerequisite for any known form of biology.

This discovery also aligns with other ongoing missions. The Perseverance rover, for example, operates in a different crater and collects samples of sediments formed in ancient river deltas. Future missions to return these samples to Earth may allow for the search for organic molecules or subtle chemical signatures of past life, including in rocks associated with ancient lakes like those in Gale Crater.

Discovery Guides Future Human Missions and Reveals Planetary Lessons

In addition to scientific interest, identifying regions where water accumulated in the past has practical implications for future crewed missions. Areas with a history of lakes may hide subsurface ice or hydrated minerals, resources that could be used to produce drinking water, oxygen, and even rocket fuel, reducing reliance on supplies from Earth.

More than mere marks on rocks, these ripples reveal how planets can change drastically by losing their atmosphere and climate balance. For researchers studying Earth’s climate, Mars serves as an extreme natural experiment, showing what happens when a world loses its capacity to retain liquid water.

Meanwhile, the Curiosity continues its slow ascent through the rock layers of Gale Crater, deciphering the past of the red planet centimeter by centimeter. The study published in Science Advances transforms a few centimeters of rippled sandstone into one of the most important records ever found regarding Mars’s climatic and environmental history.

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Felipe Alves da Silva

Sou Felipe Alves, com experiência na produção de conteúdo sobre segurança nacional, geopolítica, tecnologia e temas estratégicos que impactam diretamente o cenário contemporâneo. Ao longo da minha trajetória, busco oferecer análises claras, confiáveis e atualizadas, voltadas a especialistas, entusiastas e profissionais da área de segurança e geopolítica. Meu compromisso é contribuir para uma compreensão acessível e qualificada dos desafios e transformações no campo estratégico global. Sugestões de pauta, dúvidas ou contato institucional: fa06279@gmail.com

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