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Postgraduate Open Day MAPS

Postgraduate Open Day - at Mathematical & Physical Sciences.

The open day is a chance for prospective students for taught and research postgraduate degrees (MSc, MRes, PhD) to find out more about UCL's courses, as well as to meet potential tutors. It's also an opportunity to visit UCL's campus and see if this is the place for you. More...

Sowerby Book by P. Henderson

James Sowerby: the Enlightenment’s natural historian.

Who wanted to know about the science of minerals, meteorites and fossils? Quite a lot of people – including Humphry Davy, William Wollaston, William Smith and Joseph Banks – at the turn of the eighteenth century. A key player in meeting their needs was James Sowerby (1757-1822) who had the skills and resources to discover, illuminate and inform as well as being the focus of a network of active natural historians. Sowerby is often overlooked as a major contributor but that is a mistake. He might have lacked the social status of many scientists but he produced a remarkable body of original work that is still applicable to the present day. The first full biography of Sowerby by Paul Henderson is now published, is well illustrated and gives a fascinating insight into the science of those times. More...

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Deep-Water Research

The Ainsa Deepwater Channel Project, Spanish Pyrenees

An Integrated Outcrop Study: Project Manager: Professor Kevin T. Pickering

Introduction to the Ainsa Channel System

The Ainsa Channel System, south-central Pyrenees, occurs in the oldest part of the Campodarbe Group, and it is of Upper Eocene age. The Ainsa Channel Complex is per- haps the most famous of the submarine channel outcrops within Western Europe. The Ainsa channels consist of two principal channel complexes (Ainsa I and Ainsa II) which are separated by thin- and very thin-bedded sandy turbidites and marls. The Ainsa I Channel Complex is an example of an erosional-depositional system. The Ainsa II Chan- nel Complex contains significant erosional cut-downs, with infill of essentially non- erosive sandy facies. The channel dimensions are at a seismic scale.