Classification of sandstones
This post is part of the How To… series – how to classify sandstones using QFL plots In science, classification […]
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Some controls on grain size distributions
This post is part of the How To… series What processes determine the size distribution of clasts in clastic sediments?
Analysis of sediment grain size distributions
This post is part of the How To… series The graphical display and statistical analysis of sediment grain size became
Grain size of clastic rocks and sediments
This post is part of the How To… series You have collected a sandstone that has been described as coarse-grained.
Describing sedimentary rocks – some basics
This post is part of the How To… series Once you have read this article, you may find it useful
Kinematic analysis of deformed rock
This post is part of the How To… series Kinematics is the branch of classical mechanics that studies movement. Questions
Cleavage and cleavage-bedding intersections
This post is part of the How To… series Cleavage is a fabric. It is a close, regularly spaced planar
Stereographic projection – poles to planes
This post is part of the How to… series Stereographic projection is used in geology to decipher the complexities of
Using S and Z folds to decipher large-scale structures
This post is part of the How to… series A problem frequently encountered when mapping structurally deformed rocks is deciding
Folded rock – some terminology
This post is part of the How to… series Folds invoke a sense of awe, of some gargantuan, earth-bound push-and-shove.