Meeting the Challenge: Geological Disposal of UK higher activity radioactive waste (lecture)
Column 2 ContentProfessor Rebecca Lunn, Civil and Environmental Engineering Department, University of Strathclyde
Founded 1858 | Promoting public interest in geology and advancing geological knowledge
Founded 1858
Professor Rebecca Lunn, Civil and Environmental Engineering Department, University of Strathclyde
Dr Diarmad Campbell, British Geological Survey
Anyone interested in geoconservation is invited to attend this meeting.
Dr Derek Fabel, University of Glasgow
Professor Iain Stewart, Professor of Geoscience Communication at Plymouth University
Professor John Parnell, School of Geosciences, University of Aberdeen
We will see a fascinating variety of rocks covering a huge span of geological time, ranging from the Moine to the Palaeogene. We will also see rocks from the Ordovician, Silurian, Carboniferous, Triassic and Jurassic periods.
We will see a fascinating variety of rocks covering a huge span of geological time, ranging from the Moine to the Palaeogene. We will also see rocks from the Ordovician, Silurian, Carboniferous, Triassic and Jurassic periods.
A series of short oral presentations by society members, followed by desktop presentations, nibbles and drinks.
We shall be looking at the igneous rocks of the Clyde Plateau Volcanic Formation, the Carboniferous sedimentary rocks of the Clyde Sandstone Formation and the Ballagan Beds.
A visit to the former lead mine near Tyndrum followed by a trip to Glen Orchy to examine outcrops of Dalradian rocks
A guided tour of the Glasgow Museums Resource Centre in Nitshill
We will examine beautifully exposed examples of contact metamorphic changes to the Dalradian Aberfoyle slate adjacent to a late Caledonian diorite intrusion, the Comrie pluton at Craig More.
An opportunity to examine Dalradian rocks (slates and grits of the Southern Highland Group) and structures related to the Tay Nappe
In this easy coastal walk we will examine sedimentary structures formed during the Early Carboniferous, the consequent changes of the flora and fauna, and tectonic structures imposed during the Late Carboniferous.
