Faults and folds just support the idea that there lithospheric plates are in motion because folds appear when the plates move towards each other. The faults appear when the plates drift apart and cause an empty space.
Folds are the when the rock layers bend. Faults are breaks in the rock layers. Folds are called anticlines and synclines. Faults are called reverse faults, normal faults, or strike-slip faults.
OK!over 99 active faults!
id say faults the answer is faults
vein minerals form between faults.
faults are caused by the plates under neath earth crashing together and/or parting
Before 1965, geologists were unable to explain the abrupt disappearance of transcurrent faults in crustal rocks. Wilson explained the phenomenon with his suggestion that the vanishing faults could be explained by the presence of zones of contraction and expansion in the crustal bedrock. He named these "disappearing" faults transform faults.
The boundaries between lithospheric plates are most effectively outlined by features such as earthquakes, volcanic activity, and the distribution of mountain ranges. These boundaries can be further classified into divergent, convergent, and transform plate boundaries based on the type of plate movement occurring.
Rift Valley:A valley that has developed along a rift, especially one bounded by normal faults in an area of lithospheric thinning.
The three major types of faults are normal faults, reverse faults, and strike-slip faults. Synclines are not faults but rather geological structures that describe the folding of rock layers.
Describe the three types of plate motion and the faults that are characteristic of each type of motion.
A rift valley forms when the lithospheric stretches, tension stress occurs, causing rock to pull apart, break, and form normal faults.
You can download the detailed map of trenches,faults and Volcanoes in the Philippines.
fault
Lithospheric plates build up pressure due to the movement of the underlying mantle causing stress to accumulate along transform faults. The build-up of pressure is a result of the friction and resistance between adjacent plates. When this pressure exceeds the strength of the rocks, it causes the plates to suddenly slip past each other, resulting in an earthquake along a transform fault.
strike slip
When lithospheric plates rub against each other, it can create earthquakes. The friction between the plates causes energy to build up until it is released in the form of seismic waves. This movement along plate boundaries can result in a variety of geologic features, such as faults or mountain ranges.
You can download the detailed map of trenches,faults and Volcanoes in the Philippines.