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To make a cross section of a volcano, you can first gather geological data and topographic maps of the volcano. Then, use software like GIS or CAD to create a profile or elevation model of the volcano, and finally cut a vertical slice through the model to visualize the internal structure of the volcano.
Basically, a volcano cross section is where one "cuts" a volcano in half to visually show what the insides of a volcano (such as the magma chamber that fuels eruptions, which would otherwise be invisible to observers of the surface).
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Most plant stems are hollow - giving a cross-section that resembles a donut.
The cross-section of a root helps in identifying the root structure, such as the presence of the epidermis, cortex, endodermis, and vascular tissues. In contrast, the cross-section of a stem helps in identifying the stem's internal structure, including the epidermis, cortex, vascular bundles, and pith. These cross-sections are important for studying plant anatomy and understanding the functions of roots and stems.
The transition probability is the likelihood that a particle will change from one state to another during a collision, whereas the cross section represents the effective area that the particle presents to a collision. The transition probability is related to the cross section by the formula: transition probability = cross section * particle flux, where the particle flux is the rate at which particles are incident on a target.
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A marine volcano.