There are three primary characteristics that an object must exhibit in some form in order to be considered 'alive' by scientific standards:
It must
A) Conduct growth or self-sustenance by metabolism, or the intake, processing, and use of nutrients,
B) Reproduce so as to produce progeny and prolong the longevity of its species, and
C) Adapt to its environment and circumstances via endogenous (self-originating) changes.
Each of these qualifications may be broken down extensively into subsequent qualifications. However, something that cannot exhibit some form of these characteristics is not considered biologically 'alive.'
Earth cannot metabolize anything. As a non-organic object, essentially a rock, Earth grows by the accretion of matter. Examples of objects that grow in this way are mineral deposits, sand dunes, and back-rent. Such objects grow in size as more and more matter is added to them. They do not physically 'eat' things, though it may seem like they can.
Earth cannot reproduce. It might be cool to have Earth giving birth to litters of happy little protoplanets or planetoids, but in actuality, Earth is incapable of reproduction. At no point will Earth produce an offspring to continue being an Earth.
Earth cannot adapt. If suddenly it were to be faced by a collision with another planet, Earth would not adapt by scampering off or fighting, so as to maintain its orbit. If confronted with a superflare, Earth would adapt to become more heat-resistant. If flung into deep space, Earth would not learn to conserve energy. It is incapable of adaptation.
Additionally, all known biological life is organic. This means that it is made up of complex carbon compounds. The vast majority of life, in fact, is primarily built out of carbon, nitrogen, hydrogen, and oxygen (there are many other components, but these are by far the most populous). Earth is composed of an extremely simple layered collection of iron, nickel, silicon, and some other elements (obviously including carbon, but not in anything like the comparative proliferation found in life). Earth is essentially a gigantic rock, floating through space like so many other gigantic rocks.
By this process of examination, it should be obvious why Earth cannot be considered biologically alive. Metaphor, religion, poetry, and substance abusers may consider or refer to Earth as alive, but any competent analysis shows that it has absolutely no characteristics of life.
Mineral
Interactions between living and nonliving parts of the Earth occur in ecosystems. Living organisms rely on nonliving elements like air, water, and soil for survival, while nonliving elements are influenced by the activities of living organisms through processes like decomposition and nutrient cycling. These interactions are essential for the functioning and balance of an ecosystem.
Soil is made up of broken down pieces of living and nonliving earth material. Living material can include plant matter, organisms, and bacteria, while nonliving material can include rocks, minerals, and organic matter.
The nonliving material that makes up the Earth includes rocks, minerals, soil, water, and air. These components play a crucial role in shaping the Earth's landscape, providing essential resources for life, and influencing various geological processes and systems.
The Earth is considered non-living as it is an inanimate object made up of physical materials such as rock, water, and metal. While it sustains life through ecosystems and natural processes, the Earth itself is not living.
the earth is nonliving but has living organisms on it
Abiotic factors
minerals
organism
organism
you
Mineral
geology
Rock.
Rock would be one answer, as would be coal, both non-living, and solid.
Interactions between living and nonliving parts of the Earth occur in ecosystems. Living organisms rely on nonliving elements like air, water, and soil for survival, while nonliving elements are influenced by the activities of living organisms through processes like decomposition and nutrient cycling. These interactions are essential for the functioning and balance of an ecosystem.
Soil is made up of broken down pieces of living and nonliving earth material. Living material can include plant matter, organisms, and bacteria, while nonliving material can include rocks, minerals, and organic matter.