Why are there no earthquakes at the Marianas Trench? square the rocks slip past one another there is no movement at the trench explosive volcanoes release the pressure

The correct answer is: the rocks slip past one another.The Marianas Trench is a deep oceanic trench located in the western Pacific Ocean. It is the deepest part of the ocean, reaching depths of up to 36,070 feet (11,034 meters). The trench is formed by the subduction of the Pacific Plate beneath the smaller Mariana Plate.Earthquakes occur when there is a sudden release of energy along a fault line, which is a fracture or zone of fractures in the Earth's crust. In the case of the Marianas Trench, the subduction of the Pacific Plate creates a complex network of faults and fractures. As the Pacific Plate is pushed beneath the Mariana Plate, the rocks on either side of the fault lines slip past one another, causing earthquakes.The movement of the rocks along the fault lines generates seismic waves, which are the vibrations that cause the ground to shake during an earthquake. The intensity and frequency of earthquakes in the Marianas Trench can vary depending on the specific location and the rate of subduction.It is important to note that earthquakes can occur at the Marianas Trench, but the question seems to be asking why there are no earthquakes at the trench itself. The answer is that the rocks slip past one another along the fault lines, causing earthquakes. The other options, "there is no movement at the trench" and "explosive volcanoes release the pressure," are not accurate explanations for the absence of earthquakes at the Marianas Trench.