The Open University ’ s repository of research publications and other research outputs A branching , positive relief network in the middle mem - ber of the Medusae Fossae Formation , Equatorial Mars

A branching, positive relief network in the middle member of the Medusae Fossae Formation, Equatorial Mars - evidence for sapping?

The dispersal of pyroclasts from Apollinaris Patera, Mars: Implications for the origin of the Medusae Fossae Formation

The Medusae Fossae Formation (MFF) has long been thought to be of Amazonian age, but recent studies propose that a significant part of its emplacement occurred in the Hesperian and that many of the Amazonian ages represent modification (erosional and redepositional) ages. On the basis of the new formational age, we assess the hypothesis that explosive eruptions from Apollinaris Patera might hav...

Inverted fluvial features in the Aeolis-Zephyria Plana, western Medusae Fossae Formation, Mars: Evidence for post-formation modification

[1] The Aeolis and Zephyria Plana contain the western-most portion of the Medusae Fossae Formation (MFF), an enigmatic and extensive light-toned deposit located in the Martian equatorial region and dated from the Hesperian to Amazonian epochs. This area hosts a large population of sinuous ridges (SRs), interpreted as inverted fluvial features, formed by precipitation, indurated by chemical ceme...

The Open University ’ s repository of research publications and other research outputs “ He was the father of us all . ” Ernie Guillemin and the teaching of modern network theory

The Open University's repository of research publications and other research outputs " He was the father of us all. " Ernie Guillemin and the teaching of modern network theory Conference Item How to cite: Bissell, Christopher C. (2008). " He was the father of us all. " Ernie Guillemin and the teaching of modern network theory.

The Open University ’ s repository of research publications and other research outputs CO 2 drawdown following the middle Miocene expansion of the Antarctic Ice Sheet