GeologyRocksintrusion
Tue, 07/01/2008 - 16:31 — DuncanHill
- Location:
- Date Taken (dd-mm-yy): 25th June 2008
A rough sketch of a phacolith, denoted by the red area. A phacolith is an igneous intrusion in folded sedimentary rocks that is convex upwards and concave below.
This work is licensed under a Creative Commons Attribution-No Derivative Works 2.5 License.
Mon, 02/05/2007 - 13:11 — Jon
- Location: Holyrood Park, Edinburgh, UK
- Date Taken (dd-mm-yy): 05-10-2008
Close up of the deformation caused by an igneous intrusion on the country rock. See this image for a differnt view.
This work is licensed under a Creative Commons Attribution-No Derivative Works 2.5 License.
Mon, 02/05/2007 - 13:08 — Jon
- Location: Holyrood Park, Edinburgh, UK
- Date Taken (dd-mm-yy): 05-10-2008
View of Hutton's section in Holyrood park. The upper rocks are the igneous sill, the lower rocks are the sedimentary country rock.
This work is licensed under a Creative Commons Attribution-No Derivative Works 2.5 License.
