Syncline and anticline
In structural geology, a syncline is a fold with younger rock layers closer to the center of the structure, whereas an anticline is the inverse of a syncline.
In structural geology, a syncline is a fold with younger rock layers closer to the center of the structure, whereas an anticline is the inverse of a syncline.
Normal fault within Permian-Triassic Sediment located at Paradox Basin (Moab Utah).
Interpreted Unmanned Aerial Vehicle (UAV) model of a cliff showing igneous intrusions. Profile is from the Entrada Formation (160 Ma, Utah).
The colour-vision deficiency friendly, time-uniform geologic time scales from the s-Ink science graphics collection.
The colour-vision deficiency friendly geologic time scale from the s-Ink science graphics collection.
An artistic version of the geologic time scale that is, for flexible use, provided with variable content.
Schematic illustration of the emplacement of subduction zone initiation (SZI)-typical rock evidence during SZI, and a typical SZI ophiolite sequence.