International dateline. Zulu. 180 and 0 degrees longitude are the same figure on opposite sides of our world.
When the earth's crust splits apart, it is called a rift. This process occurs when tectonic plates move away from each other, creating a gap in the crust. Overtime, this rift can lead to the formation of new ocean basins or rift valleys.
Putting your legs apart from each one
pull your legs apart and sit down
The rocks cracks on everything
When the earth's crust splits apart and a ravine is formed, it is called a rift valley. Rift valleys are created by the stretching and thinning of the Earth's crust, often associated with tectonic plate movements or volcanic activity. Examples of rift valleys include the East African Rift and the Rhine Valley in Europe.
At the Equator.
The wedge splits things apart best when it meets resistance, such as a material that it cannot easily move through. The sharp point of the wedge concentrates force, making it easier to penetrate and break apart objects.
The stage of mitosis that splits the chromosomes and pulls them apart with spindle fibers is called anaphase. In anaphase, the sister chromatids separate and are moved towards opposite poles of the cell by the spindle fibers, ensuring each daughter cell receives a complete set of chromosomes.
Lines of longitude are farthest apart at the equator and closest together at the poles. This is because the lines of longitude converge at the poles and spread apart at the equator due to the Earth's shape being an oblate spheroid.
No! According to me the splits are not suppose to be all the way down. Flexing your leg does not mean sitting with your legs spread apart
Yes, lines of longitude converge at the poles, so their distance apart decreases as they approach the poles. At the poles, lines of longitude are essentially touching, whereas at the equator they are farthest apart.
A mineral that splits evenly along flat surfaces is said to have a cleavage fracture. Cleavage occurs when a mineral breaks along weak atomic planes due to the internal atomic structure and bonding of the mineral.