sometimes, the map view of an area is not enough. you can get a better feeling for the topography of earths surface from a profile view,or cross section. A profile view looks as though you were standing on earths surface and looking toward the horizon. examine the map view and profile view.
It is called the Earth's ORBIT around the Sun.
Scientists who study earth's oceans are called oceanographers.
The final section of the Earth might be compared to the yolk of the egg
We are called Earth. "Blue Planet" is a nickname for Earth, since our planet comprises primarily of water.
Any way you slice the earth, you get a chunk whose outline is a circle. (or approximately a circle if you look closely the mountains and valleys that the cross section cuts through disturb the circle). a mathematical sphere will give a mathematical circle at all cross sections.
A Cross-Section of the Earth
It is a cross section of the Earth. It has no specific name. You can find one at the link below
The Equator
The cross section of earth exposed by digging.
Along with their attached rigid uppermost mantle, they are referred to as tectonic plates.
A cross section of Earth cut from pole to pole would reveal a roughly circular shape. This is because Earth is an oblate spheroid, meaning it is slightly flattened at the poles and bulging at the equator due to its rotation.
You can't see the outline because there is no outline on the earth. It is just made in maps to make it easier to go somewhere.
The densest layer of the Earth's cross-section is the inner core, which is composed primarily of solid iron and nickel. The inner core has a density of about 12.8 to 13.1 grams per cubic centimeter, making it the most dense layer of the Earth.
My $210 Physical Geography class text book does not have the answer. It just says it would be smaller than the diameter of a cross section through the equator.
It is the fault.
Each cross section of soil typically shows the horizontal layering of soil types and depths down to around 20 to 30 feet beneath the Earth's surface, depending on the location and the scale of the cross section. This can vary depending on factors such as soil composition, topography, and human activities in the area.