Igneous rocks are involved in a wide range of smaller topics.
Dating
Igneous events are slotted into the relative time scale by using the Law of Cross-Cutting Relations and the Law of
Included Fragments. Igneous rocks are given an absolute date by radiometric methods.
In this way the whole of the Geological Column can be assigned ages (in millions years).
Jointing
Many igneous masses are crossed by systems of joints which are caused by the stresses during their formation and
cooling. Jointing is important in weathering and erosion, including the formation of tors (see below), and in
quarrying.
Tors
Tors upstanding tower of unweathered blocks separated by widened joints most commonly found in granite, as for
example in Devon and Cornwall. Theories for their formation suggest that differential weathering widens the joints
and periglacial 'erosion' removes the weathered material from the joints.
China Clay
Minerals in granite may be altered to clay minerals by reacting with water containing acids and other chemicals.
For the granites of Devon and Cornwall, the water probably came from depth, changing the feldspars into kaolin,
or china clay.
Building stone
Igneous rocks are widely used for decorative building stone, as any visit to a city
centre will show, and for other construction materials such as concrete blocks and roadstone.
Granite is widely because it
- is strong and doesn’t crush easily
- is hard wearing
- doesn’t weather quickly
- looks good – light in colour
- can be polished
- is plentiful
Geopix Study Topic "Igneous Miscellany"
- gives full images of the examples shown below, and others, to illustrate these features
- describes each of the topics in more detail
The Igenous Miscellany Study Topic contains the following pages:
'Miscellany' is part of the Igneous Processes Study Guide CD.
To order this CD go to the Geopix Online Store