by Gelogia Team | Jul 7, 2025 | Physical Geology & Geomorphology, Structural Geology
Faults are fractures in the Earth’s crust where blocks of rock have moved past each other due to tectonic forces. These movements are caused by stresses such as compression, tension, and shearing. Understanding the types of faults is essential in geology to interpret...
by Gelogia Team | Jul 6, 2025 | Physical Geology & Geomorphology, Structural Geology
Soil properties are fundamental characteristics that define how soil behaves under various conditions. In geotechnical engineering, understanding these properties is essential for analyzing ground stability, designing foundations, and ensuring safe construction...
by Gelogia Team | Jun 21, 2025 | Physical Geology & Geomorphology, Structural Geology
Magnitude is a measurement of the energy released by an earthquake. Earthquake magnitude scales in general do not directly represent any physical parameters of the source. Magnitude scales can be used to represent the relative size of earthquakes. Why Are Magnitude...
by Gelogia Team | Jun 19, 2025 | Physical Geology & Geomorphology, Structural Geology
Continental rifts are geological zones where the Earth’s crust is stretched and broken, forming deep fault-bounded valleys. These structures play a key role in understanding plate tectonics, continental breakup, and the formation of new ocean basins. This...
by Gelogia Team | Jun 13, 2025 | Historical Geology, Structural Geology
What Are Terranes? Terranes are fault-bounded crustal blocks that have distinct lithologic and stratigraphic successions and geologic histories different from those of neighboring terranes (Schermer et al., 1984). Most terranes have collided with continental...
by Gelogia Team | Apr 25, 2025 | Structural Geology
The sea level means the level of the surface of the sea. It is the mean position or midway between the mean high and mean low water levels, computed from the records of tidal oscillations over a long period and seasonal variations. It is defined based on the...
