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Photo caption: Waves received in the wind tunnel of Ben Gurion University of the Negev with glass balls with a diameter of 90 microns. Two scales of waves can be seen in the image.

New theory explains sand ripples on Mars and on Earth

Diamond

Ancient diamonds shine light on the evolution of Earth

Earth

Researchers probe molten rock to crack Earth’s deepest secrets

Anelasticity spectra with respect to water content.

Exploring the Effect of Water on Seismic Wave Attenuation in the...

Tiny mineral inclusions picture for the first time oxygen accumulated in the atmosphere and changed the composition of the mantle. Credit: Hugo Moreira / Nature Geoscience

New research reveals Earth’s ancient ‘breath’

Oxidised apatite inclusions. Credit: Dr Hugo Moreira

New research reveals connection between Earth’s atmospheric changes and mantle chemistry

Dalian Coherent Light Source revealing vacuum ultraviolet photodissociation of sulfur dioxide as an important prebiotic-O2 source. Credit: Yuan Kaijun

A possible trigger for Earth’s great oxidation event

Inner Earth. Credit: Gary Hincks/Science Photo Library

Earth’s solid metal sphere is ‘textured’

An MIT study of the freshwater greenfin darter fish suggests river erosion can be a driver of biodiversity in tectonically inactive regions. Credits: Image: Jose-Luis Olivares/MIT with fish photo by Isaac Szabo

River erosion can shape fish evolution

Metamorphosed banded iron formation from southern Wyoming showing deformation and folding. The rock is approximately 2.7 billion years old. Dark bands are iron oxides (magnetite, hematite) and yellow-orange bands are chert with iron oxide inclusions (jasper). (Photo by Linda Welzenbach-Fries/Rice University)

Iron-rich rocks unlock new insights into Earth’s planetary history

A microscope image from an experiment conducted for this study. The image contains glass (brown), large garnets (pink) and other small mineral crystals. The field of view is 410 microns wide, about size of a sugar crystal. Credit: Science (2023). DOI: 10.1126/science.ade3418

Study presents new clues about the rise of Earth’s continents

An illustration showing how some Earth’s signature features, such as its abundance of water and its overall oxidized state could potentially be attributable to interactions between the molecular hydrogen atmospheres and magma oceans on the planetary embryos that comprised Earth’s formative years. Illustration by Edward Young/UCLA and Katherine Cain/Carnegie Institution for Science.

How did Earth get its water?

Earth

Where did Earth’s water come from? Not melted meteorites, according to...

Earth

Activity deep in Earth affects the global magnetic field

Seismogram

Bouncing seismic waves reveal distinct layer in Earth’s inner core

Earth

Deep earthquakes could reveal secrets of the Earth’s mantle

hydrothermal vent

Deep-sea black carbon comes from hydrothermal vents

Meteorites

Meteorites reveal likely origin of Earth’s volatile chemicals

inner core (USC Graphic/Edward Sotelo)

Earth’s inner core rotating slower than surface

Dimitri Laurent explores a typical gallery in the Nébélé Cave, which was formed by sulfuric acid speleogenesis. You can see a deep notch that indicates the former presence of a river, and sodium sulfate on the left that is produced from weathering by sulfuric acid. Credit: Christophe Durlet

Unearthing the sources of cave-forming sulfuric acid

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