Definitions Flashcards
Crystalline rocks
Form directly from magma and volcanic activity
geomorphology
The shape of an environment
Fragmentary rocks form after
crystalline rocks have been broken down by weathering, transported, accumulated in deposits, then formed into rocks by heat and pressure of deep burial - lithification
Mineral
Naturally occurring mineral, limited range of chemical composition
Rock
Combination of many minerals, few rocks are formed of a single mineral - marble (calcite) and quartzite (Quartz)
Igneous rocks
Cooling and crystallisation of magma. Mixture of several minerals.
Basalt
Forms oceanic crust
Andesite
Forms continental crust, lower density than basalt.
Partial melting
Silicate minerals, lower melting temps.
Fractional crystallisation
Silicate minerals with higher melting temps may crystallise as magma rises to cooler parts of the crust.
Sedimentary rocks
Fragmentary rocks, brought together by sedimentation.
Metamorphic
Crystalline - undergone a process of change through heat and pressure, often by deep burial.
Crystalline structure of metamorphic rocks
Crystalline components are changed into different minerals. Layered appearance. Crystal growth is at right angles to show a squeezed out appearance of crystals.
Hydrolysis is
The breakdown by water
Hydration is
Part physical and part chemical absorption of water by minerals