Taken along a line drawn on a map, it is a diagram of the structure and position of the rock layers present beneath the surface along this line.
Geologists learn how to construct this 3rd dimensional information from a Geologic map,
If you want to know how to get at an ore body hidden underground, you need a Geologist to work out where and how deep to dig. Cross sections will be needed to do this.
A geological cross section is an graphical illustration of the earth as if it were cut open. This is used to show the arrangement of the various of the earth.
A topographic profile is a plot showing the shape of the surface of the ground (so hills, hillocks, dips, valleys and the like). Whereas a geologic cross section shows the order and structure of soils and / or rocks below the ground surface. Geologic sections are typically created by first drawing a topographic profile of the section of interest then adding in the underlying strata. An example of the way they are created is given in the related links.
The guidelines used to determine the relative ages of the rocks and events shown by a geologic cross-section is the Law of Superposition. It is the basic law of geochronology.
cross-section of a root
Most plant stems are hollow - giving a cross-section that resembles a donut.
Precambrian, Paleozoic, Mesozoic and Cenozoic.
a cross section map is a map that shows the layers of rock inside a landform.
Erosion
The guidelines used to determine the relative ages of the rocks and events shown by a geologic cross-section is the Law of Superposition. It is the basic law of geochronology.
A topographic profile is a plot showing the shape of the surface of the ground (so hills, hillocks, dips, valleys and the like). Whereas a geologic cross section shows the order and structure of soils and / or rocks below the ground surface. Geologic sections are typically created by first drawing a topographic profile of the section of interest then adding in the underlying strata. An example of the way they are created is given in the related links.
The guidelines used to determine the relative ages of the rocks and events shown by a geologic cross-section is the Law of Superposition. It is the basic law of geochronology.
A cylinder has a circular cross section that is parallel to its base.
Not a right cross-section.
cross-section of a root
cross-section of a root
A profile is a cross section in soil.
Yes a prism can have a square cross-section
No, a cube cannot have an octagonal cross-section.