Magma ocean crystallisation sets up the early structure and long-term evolution of terrestrial planets. Recent seismic evidence signals the presence of a silicate layer at the base of Mars’ mantle.
geology
How Rock Removes CO2 From The Atmosphere
Rocks can bind carbon dioxide — and much faster than previously thought. For a long time, it was assumed that the transformation of CO2 into carbonate rock depends on very […]
What Triggered Earth’s Shift From A Greenhouse To An Icehouse Climate And The Onset Of The Late Paleozoic Ice Age?
Scientists have debated for decades what caused the Late Paleozoic climate transition from a greenhouse to an icehouse state ~350 million years ago. Some invoke a pronounced increase in continental […]
Serendipitous Discovery Of Martian Ripple Marks Reveals An Ancient Sandstorm
The search for life on Mars involves the efforts of scientists from many different disciplines. An important aspect of that search is to study Martian sedimentary rocks for information about […]
Desert/Water Planet Interaction: Sahara Dust Storm Over The Canary islands
Earlier this week strong winds over the Saharan Desert blew westwards pushing clouds of dust and sand over southern and central Morocco and out into the Atlantic Ocean. This is […]
Earth Formed From Local Building Blocks
Planetary scientists have long debated where the material that formed our Earth comes from. Despite its location in the inner Solar System, they consider it likely that 6–40 per cent […]
Tianwen-2 Target Asteroid (469219) Kamo’oalewa Probably Develops An Itokawa-compositional But Ultra-highly Space-weathered Surface
China’s Tianwen-2 mission plans to return samples from a small, rapidly spinning Earth quasi-satellite (469219) Kamo’oalewa. Previous studies linked Kamo’oalewa to lunar composition and origin.
Iron Isotope Anomalies And The Origin Of The Earth
Understanding the origin of the Earth requires determining the original formation location of its building material.
Study Shows Movement Of Tectonic Plates 3.5 Billion Years Ago
The history of the Earth is written on the great tablets of tectonic plates.
Investigation Of Venus’ Thermal History, Crustal Evolution, And Core Dynamics With A Coupled Interior-lithosphere-atmosphere Model
We simulate Venus’ evolution with a coupled one-dimensional solar-atmosphere-lithosphere-mantle-core model to predict currently unobservable features and its eruptive mass flux.
