Strike, dip and geological map constraints
Strike is the bearing of a horizontal line in a plane; dip is the maximum inclination from horizontal, perpendicular to strike, with direction specified.
Key knowledge
Strike is the bearing of a horizontal line in a plane; dip is the maximum inclination from horizontal, perpendicular to strike, with direction specified. Field orientations, contacts and topography constrain map patterns and cross-sections. Subsurface interpretation remains an inference constrained by the observations.
Conditions and scope
- A dip angle without dip direction can be ambiguous; horizontal planes have no unique strike.
- A cross-section must state its orientation and assumptions; apparent and true dip differ.
Sources · 1
References
Sources retain their recorded scope. A source link alone does not establish verification of every statement.
Evidence and review
Read strike/dip definitions, directional ambiguity and map/cross-section illustration text.
2026-10-10 · Independent AI editorial review: All36 Life-authored Earth compact statements/conditions/displayed equations and all81 origin semantic links read; all36 author exact-source matrix rows and exclusions assessed. All18 inherited Earth compact records read for combined inventory. Targeted independent actual primary sections listed below; not every source body or proof independently reread. AI editorial reference review, not human certification/field proficiency or whole-field completion. Receipt: earth-life-independent-content-review.1.
Entry details
Permanent link to this entry ↗- Record identity
- uni-earth-strike-dip-maps
- Revision
- core.1
- Structured reference record
- University core expansion