When subjected to heat and pressure, a chemical sedimentary rock can be changed into which rock type?

a-metamorphic rock

b-a foliated rock

c-a clastic sedimentary rock

d-a non-foliated igneous rock

Option (A)

Explanation:

The metamorphic rocks are defined as those rocks that are formed due to the increasing pressure and temperature conditions. They are known as the secondary rocks because they are directly derived from either igneous or sedimentary or other metamorphic rocks. For example, Quartzite, Schist, Gneiss and Marble.

Due to the high amount of temperature and heat conditions, the chemical composition of the rock alters and changes to a more higher grade rocks. This metamorphic rocks are mainly of 2 types. They are as follows-

(1) Foliated- For example, Schist and Gneiss

(2) Non-foliated- For example, Marble and Quartzite.

Thus, the correct answer is option (A).

i believe you meant to say air rather than hair so the answer is below ")

the dead sea, the lowest place on earth at 430 metres (1,410 ft) below sea level, has a correspondingly high typical atmospheric pressure of 1065 hpa.

4.) metal

"-the movement of carbon from the nonliving environment into living things and back to the environment

-carbon is the essential component of proteins, fats, and carbohydrates (which make up all organisms)

-carbon exists in air, water, and living organisms

-producers convert carbon dioxide in the atmosphere into carbohydrates during photosynthesis

-bacteria in the atmosphere cycles through the system in filtration units

-in cellular respiration, carbon is released back into the atmosphere as carbon dioxide

-some carbon is stored in limestone (forming one of the largest "carbon sinks" on earth)

-largest carbon reservoir on earth= limestone

-carbon stored in the bodies of organisms as fat, oils, or other molecules may be released into the soil or air when the organism dies

-this may form deposits of coal, oil, or natural gas (fossil fuels, which increased the atmospheric carbon dioxide)

-fossil fuels store carbon left over from bodies of organisms that died millions of years ago

-they are located in the surface of earth, deep within the earth and beneath the ocean floor."