The Bagnold dune field, Gale crater
A series introducing aeolian processes and deposition, comparing the conditions on Earth and Mars. Mars’ landscaping over the past three […]
A series introducing aeolian processes and deposition, comparing the conditions on Earth and Mars. Mars’ landscaping over the past three […]
A series on clay minerals – their crystal chemistry, identification, formation Weathering of sediment and rock at Earth’s surface is
A series on clay minerals – their crystal chemistry, identification, formation Sedimentary clays are tiny. The Udden-Wentworth upper grain-size limit
A series on clay minerals – their crystal chemistry, identification, formation Clays are a ubiquitous component of nearly all siliciclastic,
A series on clay minerals – their crystal chemistry, identification, formation Clays belong to the phyllosilicate group of minerals, that
This biography is part of the series Pioneering women in Earth Sciences – the link will take you to the
The orbiter and rover missions that allow us to step into Martian geology Most formal publications on planetary science incorporate
How do we know there are sedimentary rocks on Mars? Some of the criteria that justify our inclusion of sedimentary
The rheology of soft sediment and weak rock. This post is part of the Lithofacies Series. See the companion post
Slump folds, slides, convoluted laminae, enterolithic folds, normal and thrust faults, glide planes, fractures, boudinage, ball-and-pillow, load casts, dewatering pipes,