What are the types of resources? mention them​

Anything that is useful to us is known as a resource. Some resources have financial value, while others have no economic value. For example, milk has economic worth, but it has no economic value in a beautiful landscape. But both are important because they meet certain human needs.

Explanation:

In general, resources are classified into three different types: natural, human, and human resources.

Natural resource: natural resources are known as natural resources. Some natural resources can be used straight away, while some other technologies require the help of.

Human-made resources: When a natural resource is dramatically modified through human intervention, it becomes a human resource. E.g. iron ores are processed into steel and thus steel is a resource made by humans. Examples of human resources are buildings, bridges, railways, machinery, etc. Tech is also a resource made by human beings.

Human resource: Human resources are people. People. The quality of human resources is improved by education and health. The development of human resources is known as improving the quality of people's skills to help them create more resources.

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the earth’s crust is broken into separate pieces called tectonic plates (fig. 7.14). recall that the crust is the solid, rocky, outer shell of the planet. it is composed of two distinctly different types of material: the less-dense continental crust and the more-dense oceanic crust. both types of crust rest atop solid, upper mantle material. the upper mantle, in turn, floats on a denser layer of lower mantle that is much like thick molten tar.

each tectonic plate is free-floating and can move independently. earthquakes and volcanoes are the direct result of the movement of tectonic plates at fault lines. the term fault is used to describe the boundary between tectonic plates. most of the earthquakes and volcanoes around the pacific ocean basin—a pattern known as the “ring of fire”—are due to the movement of tectonic plates in this region. other observable results of short-term plate movement include the gradual widening of the great rift lakes in eastern africa and the rising of the himalayan mountain range. the motion of plates can be described in four general patterns:

collision: when two continental plates are shoved together

subduction: when one plate plunges beneath another (fig. 7.15)

spreading: when two plates are pushed apart (fig. 7.15)

transform faulting: when two plates slide past each other (fig. 7.15)