Environmental science is actually a lot of fun, and not that difficult, provided you are good with science such as geology, chemistry and biology. Environmental science is a field which can change rapidly, so much of what you learn in school can become obsolete in a few short years.

Ecology, a specific branch of environmental science, focuses on the interaction between organisms and their environment. The field of environmental science studies humanity’s effects on the environment, while ecology does not.

Environmental science is important because it enables you to understand how these relationships work. For example, humans breathe out carbon dioxide, which plants need for photosynthesis. Plants, on the other hand, produce and release oxygen to the atmosphere, which humans need for respiration.

Ecology enriches our world and is crucial for human wellbeing and prosperity. It provides new knowledge of the interdependence between people and nature that is vital for food production, maintaining clean air and water, and sustaining biodiversity in a changing climate.

The solid crust of the earth is known as lithosphere. It provides us with forests, grasslands fro grazing and valuable land for agriculture and human settlements. It is also an important source of mineral resources.

Answer: lithosphere provides you soil and land on which you are walking or sitting right now, they also help in growing plants and help in building of apartments or house etc.

The asthenosphere is now thought to play a critical role in the movement of plates across the face of Earth’s surface. Some observers have described the asthenosphere as the ‘lubricating oil’ that permits the movement of plates in the lithosphere. …

Complete answer: Lithosphere is used by human beings in a variety of ways, we use it for agriculture as well as fuel. Lithosphere has so many varied uses because it contains so many valuable items for human beings. -The lithosphere is used by us to cultivate crops, feed livestock and ourselves.

The asthenosphere is the denser, weaker layer beneath the lithospheric mantle. It lies between about 100 kilometers (62 miles) and 410 kilometers (255 miles) beneath Earth’s surface. The temperature and pressure of the asthenosphere are so high that rocks soften and partly melt, becoming semi-molten.

The asthenosphere is a solid but it can flow, like toothpaste. The lithosphere rests on the asthenosphere.

Earth’s crust is divided into two types: oceanic crust and continental crust. The transition zone between these two types of crust is sometimes called the Conrad discontinuity. Silicates (mostly compounds made of silicon and oxygen) are the most abundant rocks and minerals in both oceanic and continental crust.