A lower boundary is the minimum value or limit in a set or range of values. It is used to define the starting point or bottom limit of a particular range or interval.
The lower boundary of the Earth's crust is called the Mohorovičić discontinuity, or Moho for short. It is typically located between 5 and 10 kilometers beneath the ocean floor and around 20 to 70 kilometers beneath the continents.
The plate boundary at which plates collide or come together is called a convergent boundary. At convergent boundaries, one plate is typically forced beneath the other in a process known as subduction. This collision can lead to the formation of mountain ranges, deep ocean trenches, and volcanic activity.
Divergent Boundary, (Constructive Boundary).
Another term for diverting boundary could be a redirecting boundary or a deflecting boundary.
coliding boundary
In statistics the class boundaries are numbers that separate classes without forming gaps. To find the lower, you subtract 0.5 and to find the upper, you add 0.5. If the class is 3-7 the lower class boundary would be 2.5 and the upper 7.5. The upper boundary of one class will equal the lower boundary of the next class.
Moho
The median is the middle number in a data set. The lower class boundary is the first quartile or number that is 25 percent lowest in the data set.
pearl
class boundary is the midpoint between the upper class limit of a class and the lower limit class of the next class sequence when making a class interval starting at the lowest lower limit in the bottom of a table.
The lower boundary of the Earth's crust is called the Mohorovičić discontinuity, or Moho for short. It is typically located between 5 and 10 kilometers beneath the ocean floor and around 20 to 70 kilometers beneath the continents.
Limits give upper and lower bounds for integration. One simple example is in finding an enclosed area. The upper and lower limits form vertical lines which enclose an area between the function and the x-axis and then integration from the lower limit (smaller x boundary) to the upper limit (larger x boundary).
Factors affecting boundary layer thickness include fluid velocity, fluid viscosity, surface roughness, and boundary layer separation. Higher velocities and lower viscosity tend to result in thinner boundary layers, while rough surfaces and separation zones can lead to thickened boundary layers.
The Earth's mantle temperature ranges from about 500°C to 900°C near the upper boundary, and it can reach up to 3000°C near the lower boundary.
Goverment of India can make changes in the boundary of states through a bill passed by the lower and upper houses of the parliament with the concent of the state in question.
boundary between the lower mantle and the outer core
The boundary separating the Earth's mantle and core is known as the core-mantle boundary. This boundary is characterized by a sharp decrease in seismic wave velocities, indicating a difference in composition and properties between the outer core and the lower mantle.