A slip-strike fault is one where the two areas move sideways with regard to one another. A normal fault is where one area drops down, and a reverse fault is one where an area is thrust upwards.
The type of fault that occurs when one portion of rock slides over the top of another is called a reverse fault. In a reverse fault, the hanging wall moves upward relative to the footwall, typically due to compressional forces. This type of faulting is commonly associated with convergent plate boundaries where tectonic plates collide.
The 2004 earthquake in northern Sumatra, Indonesia was caused by a megathrust subduction zone fault between the Indian Plate and the Burma Plate. This type of fault is known as a subduction zone fault, where one tectonic plate is forced beneath another.
A strike-slip fault is the type of fault that primarily moves sideways. In this fault type, the movement occurs horizontally along the fault line, with rocks on either side sliding past each other. This lateral movement can be observed in regions where tectonic plates slide against one another, often leading to significant seismic activity. A well-known example of a strike-slip fault is the San Andreas Fault in California.
It is a solution.
A fault that results from horizontal shearing between tectonic plates is called a strike-slip fault. In this type of fault, the movement is primarily horizontal, with the blocks of crust sliding past one another laterally. The San Andreas Fault in California is a well-known example of a strike-slip fault, where the Pacific Plate and North American Plate move in opposite horizontal directions.
Transforming- The plates rub each other as they push one another.
It is called subduction.
The type of fault that occurs when one portion of rock slides over the top of another is called a reverse fault. In a reverse fault, the hanging wall moves upward relative to the footwall, typically due to compressional forces. This type of faulting is commonly associated with convergent plate boundaries where tectonic plates collide.
A thrust fault results when one plate is compressed up onto another plate during an earthquake. This type of fault occurs in convergent boundary settings where the two plates are moving towards each other.
The 2004 earthquake in northern Sumatra, Indonesia was caused by a megathrust subduction zone fault between the Indian Plate and the Burma Plate. This type of fault is known as a subduction zone fault, where one tectonic plate is forced beneath another.
Wave is a propagation of substance's or field disturbances. If disturbances are small, waves are linear. Simply they distinguished one from the other by their wavelength, frequency & geometrically - by wave front. There are cross-section (for example light - electromagnetic wave) and longitudinal (f.e. sound) waves, which distinguished by directions of substance or field oscillation via wave propagation...Generally, one type of wave distinguished from another by their by their physical behavior.
wavelengths
it means it is different from one thing to another
A strike-slip fault is the type of fault that primarily moves sideways. In this fault type, the movement occurs horizontally along the fault line, with rocks on either side sliding past each other. This lateral movement can be observed in regions where tectonic plates slide against one another, often leading to significant seismic activity. A well-known example of a strike-slip fault is the San Andreas Fault in California.
It is a solution.
A fault that results from horizontal shearing between tectonic plates is called a strike-slip fault. In this type of fault, the movement is primarily horizontal, with the blocks of crust sliding past one another laterally. The San Andreas Fault in California is a well-known example of a strike-slip fault, where the Pacific Plate and North American Plate move in opposite horizontal directions.
by their method of mobility