On the contrary, the main force in the nucleus keeps particles together. This is called the strong nuclear force, and it keeps similarly charged protons together, overcoming the electrostatic
Tension stress
Microtubules pull the chromatids from the chromosome apart. Each former sister c
When there is a divergent boundary, regardless if the plates are ocean-ocean or continental-continental, tensional stress pulls on the crust. Rocks have weaker tensional strength than compressive strength, so they are easier to pull apart.
The process called plate tectonics is responsible for plates pulling apart. Over time, and with the combination of carbon dioxide, erosion, and force, plates are able to pull apart. This will eventually cause some plates to separate from one another.
Divergent plate boundaries form once two plates begin to pull apart from each other.
When to plates pull apart on the ocean floor it's called "Tectonic Plate Drift or, "Contenetial Drift." This allows countries to move centimeters every year in any direction the plate travel. Sometimes the plates rub and can cause earthquakes ,volcanos or tsunamis.
Divergent Pull Ex.<--_-->
Compressional stresses (reverse or thrust fault) cause a rock to shorten. Tensional stresses (normal fault) cause a rock to elongate, or pull apart. Shear stresses (strike-slip or horizontal fault) causes rocks to slip past each other.
Microtubules pull the chromatids from the chromosome apart. Each former sister c
If they are farther apart, there is less gravitational pull. Opposite if they are closer together.
When the magnets pull apart they are attracting each other because, there is a South Pole of a magnet and a North Pole i of a Magnet. :)
They pull the sister chromatids apart.
Deconstruct means to pull apart or to damage something.
During the middle ages, they'd use 4 horses to pull a person apart attaching a limb to each horse, as the picture above shows, it was called being "drawn and quartered" or "disruption".
The process called plate tectonics is responsible for plates pulling apart. Over time, and with the combination of carbon dioxide, erosion, and force, plates are able to pull apart. This will eventually cause some plates to separate from one another.
When there is a divergent boundary, regardless if the plates are ocean-ocean or continental-continental, tensional stress pulls on the crust. Rocks have weaker tensional strength than compressive strength, so they are easier to pull apart.
Some magnets are stronger than others, making them harder to pull apart. For strong magnets, you can pull the magnets sideways to get them apart.
They are all mechanical stresses. Push is a compressive stress. Pull is a tensile stress and Twist is a type of shear stress.