A fault.
A Fault.
A fault is a fracture in a large volume of rock, generally caused by tectonic activity. Faults, such as the San Andreas Fault in California, are often regions of frequent seismic activity for the same reason.
Depending on the context, a break in a rock may be a fault (where the rock on one side of the break has been displaced relative to the other), or a joint where there is no relative displacement of the rock on either side of the break. These may also be known generically as discontinuities, especially in the field of rock mechanics. Also the "break" in the depositional record of a sedimentary rock may be known as an unconformity.
A fault-block mountain is formed by blocks of the Earth's crust moving along a fault.
it is formed when a large block of land is pushed upwards along a crack or between two cracks in the crust
A graben is a down-thrown block which is bounded by faults along its sides. A horst is an up-thrown block which is bounded along its sides. When a horst and graben are beside each other, they are considered to be a horst and graben structural system.
The bending of rock layers due to stress
A fault is a fracture in a large volume of rock, generally caused by tectonic activity. Faults, such as the San Andreas Fault in California, are often regions of frequent seismic activity for the same reason.
Friction is encompassed by Newton's laws, as opposed to operating out side of it. If a block slides down a wedge, there is friction acting against the block up the slope. From the wedge's perspective, the block produces a frictional force against it, trying to drag it downwards along the slope.
Slides down
A place that is near the destination (example: it is one block north of the Chinese restaurant.) Unlike a definite location, relative location is dependent upon another factor and will change.
4 meters/second
Unknown. Everything after the collision depends on the nature of the friction between the block and the surface on which it slides. We have no way of estimating the energy dissipated as the 13.4 kg scrapes along for 15 cm before coming to rest, so we can't calculate the KE of the putty before the merger.
Depending on the context, a break in a rock may be a fault (where the rock on one side of the break has been displaced relative to the other), or a joint where there is no relative displacement of the rock on either side of the break. These may also be known generically as discontinuities, especially in the field of rock mechanics. Also the "break" in the depositional record of a sedimentary rock may be known as an unconformity.
It's called a "portcullis"
For a fingernail, yes.For a city block, no.It's all relative.
Fault-block mountain: Mountain that forms along a normal fault where stress causes huge blocks of rock to tilt up.
26° relative to bore centerline and then 4° relative to crank centerline. Exhaust is 17° and also 4°.