The earth can be divided into four interconnected spheres:
All four spheres can be and often are present in a single location. For example, a piece of soil will contain minerals from the lithosphere. Additionally, there will be elements of the hydrosphere present as moisture within the soil, the biosphere as insects and plants, and even the atmosphere as pockets of air between soil pieces. The complete system is what makes up life as we know it on Earth.
- biosphere, and
These four interconnected parts that make up a complete system of life on earth. Environmental scientists use this system as base to classify and study the organic and inorganic materials found on the planet.
The lithosphere, sometimes called the geosphere, refers to all of the rocks of the earth. It includes the planet’s mantle and crust, the two outermost layers. The boulders of Mount Everest, the sands of Miami Beach, and the lava erupting from Hawaii’s Mount Kilauea are all components of the lithosphere. The actual thickness of the lithosphere varies considerably and can range from roughly 40 km to 280 km. The lithosphere ends at the point when the minerals in the earth’s crust begin to demonstrate viscous and fluid behaviors. The exact depth at which this happens depends on the chemical composition of the earth as well as the heat and pressure acting upon the material. The lithosphere is divided into about 12 major tectonic plates and several minor plates that fit together like a jigsaw puzzle. The main plates include the Eurasian, Indo-Australian, Philippine, Antarctic, Pacific, Cocos, Juan de Fuca, North American, Caribbean, South American, Scotia, and African plates. These plates aren’t fixed; they’re slowly moving. The friction created when tectonic plates push against one another causes earthquakes, volcanoes, and the formation of mountains and ocean trenches.
The hydrosphere is composed of all of the water on or near the planet’s surface. This includes oceans, rivers, and lakes, as well as underground aquifers and the moisture in the atmosphere. Scientists estimate the total amount at about 1.3 billion cubic kilometres. More than 97% of the earth’s water is found in its oceans.3 The remainder is freshwater, two-thirds of which is frozen within the earth’s polar regions and mountain snowpacks. It’s interesting to note that even though water covers the majority of the planet’s surface, water accounts for a mere 0.023% of the earth’s total mass.
The planet’s water doesn’t exist in a static environment, it changes form as it moves through the hydrological cycle. It falls to the earth in the form of rain, seeps into underground aquifers, rises to the surface from springs or seeps from porous rock, and flows from small streams into larger rivers that empty into lakes, seas, and oceans, where some of it evaporates into the atmosphere to begin the cycle anew.
The biosphere is composed of all living organisms: plants, animals and one-celled organisms alike. Most of the planet’s terrestrial life is found in a zone that stretches from 3 meters below ground to 30 meters above it. In the oceans and seas, most aquatic life inhabits a zone that stretches from the surface to about 200 meters below. But some creatures can live far outside of these ranges: some birds are known to fly as high as 7,000 meters above the earth, under certain circumstances. On the other side of the spectrum, the Mariana snailfish has been found living at a depth below 6,000 meters in the Marianas Trench.7 Microorganisms are known to survive well beyond even these ranges. The biosphere is made up of biomes, which are areas where plants and animals of a similar nature can be found together. A desert, with its cactus, sand, and lizards, is one example of a biome. A coral reef is another.
The atmosphere is the body of gasses that surrounds our planet, held in place by earth’s gravity. Most of our atmosphere is located close to the earth’s surface where it is most dense. The air of our planet is 79% nitrogen and just under 21% oxygen; the small amount remaining is composed of argon, carbon dioxide, and other trace gasses. The atmosphere itself rises to about 10,000 kilometers in height and is divided into four zones. The troposphere, where about three-quarters of all atmospheric mass can be found, stretches from about 8 to 14.5 kilometers above the earth’s surface. Beyond this lies the stratosphere, which rises to 50 kilometres above the planet. Next comes the mesosphere, which extends to about 85 kilometres above the earth’s surface. The thermosphere rises to about 600 kilometres above the earth, then finally the exosphere, the outermost layer. Beyond the exosphere lies outer space.