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 […]
In the field
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.
The Rule of Vs in geological mapping
Deciphering the outcrop expression of beds and topography This post is part of the How To… series Geology maps and
Measuring a stratigraphic section
Some ideas on field measurement of stratigraphic sections This post is part of the How To… series Next to measuring
The hydraulics of sedimentation; Flow Regime
This post is part of the How To… series We introduce some basic hydraulics of sediment movement, bedforms and the
Crossbedding – some common terminology
This post is part of the How To… series Eocene fluvial tabular crossbeds exposed along MacKenzie River, northern Canada Crossbeds
Measuring and representing paleocurrents
This post is part of the How To… series Identifying sedimentary structures that indicate paleocurrent directions is an important task