Atmosphere

Atmosphere

Atmosphere: The atmosphere of a terrestrial planet is an outermost series of layers that comprises gaseous phase elements within part of the planet’s gravitational field. For instance, the Earth’s atmosphere exists in the air spaces that are approximately 95 kilometers above the ground surface. And within it, are the troposphere, stratosphere, mesosphere, and thermosphere. As of the date of this post, the exosphere and ionosphere are not part of the Earth’s gaseous envelope or atmosphere.

Order of Layers in the Earth’s Atmosphere

1. Troposphere

On Earth, the troposphere exists roughly 0 to 10 kilometers above mean sea level.

2. Stratosphere

The stratosphere exists roughly 10 to 50 kilometers above mean sea level on Earth.

3. Mesosphere

Earth’s mesosphere exists approximately 50 to 85 kilometers above mean sea level.

4. Thermosphere

The thermosphere starts at roughly 85 kilometers above mean sea level. As of the date of this post, there isn’t a clear understanding of the upper boundary of Earth’s thermosphere. However, it may terminate approximately 95 kilometers above mean sea level.

5. Exosphere

As of the date of this post, there isn’t a clear understanding of the lower or upper boundaries of Earth’s exosphere. However, it may commence approximately 95 kilometers above mean sea level, and terminate roughly around 190,000 kilometers above mean sea level. This distance is

Similar Posts

  • Hydro-Geology (Hydrogeology)

    Hydro-Geology (Hydrogeology) Hydro-Geology (Hydrogeology): Hydrogeology is a branch of geology that relates to the study of the earth’s natural groundwater and surface water systems. Whereby geologists study the physical and chemical properties of unconfined aquifers, confined aquifers, river systems, lake beds, oceanwater, natural geysers, and more.

  • Silicates

    Silicates Definition In the fields of geology and mineralogy, the term “silicates” refers to compounds whose crystal structure contains SiO4 tetrahedra. Silicates are either isolated or joined to form groups, rings, single or double chains, sheets, or three-dimensional frameworks.

  • Fault Scarp

    Fault Scarp Fault Scarp: In the field of geology, a dip-slip fault scarp is a steep slope that is formed directly by fault movement. It occurs along the line of a normal fault, reverse fault, or transform fault. A fault scarp represents the planer surface of the fault before erosion and weathering modify it.

  • Rock Stratigraphic Unit

    Rock Stratigraphic Unit In the field of geology, a rock stratigraphic unit, or a lithostratigraphic unit, is a geologic formation that is identifiable by a specific lithology, as well as a consistent stratigraphic position. For example, the Monterey Formation is a rock stratigraphic unit, as it tends to consistently comprise the same gravel and sand…