Similarities: Both Earth's early environment and Mars's early environment had water sources, volcanic activity, and a thin atmosphere.
Differences: Earth's early environment had a stronger magnetic field, which helped protect its atmosphere from solar winds and retain water, whereas Mars's weak magnetic field led to the loss of most of its atmosphere and surface water. Additionally, Earth experienced plate tectonics and a stable climate, while Mars did not.
Environmental scientists study the Earth's environment and the interactions between humans and the natural world. Geologists and geographers also study Earth's resources such as minerals, water, and land.
Earth's heat is transferred by convection, which is the movement of heat through a fluid due to differences in temperature. It is also transferred by conduction, which is the direct transfer of heat through a material due to a difference in temperature between two points.
The division of Earth's atmosphere into layers is based primarily on changes in temperature with altitude. The layers are the troposphere, stratosphere, mesosphere, thermosphere, and exosphere, with each layer characterized by its unique temperature profile and composition. These layers are determined by the balance between the absorption of solar radiation and the emission of infrared radiation by gases in the atmosphere.
Similarities: Both slow changes, like continents moving and tectonic plate shifts, can result in geological events such as earthquakes and volcanic eruptions. Both have long-term impacts on the Earth's landscape and ecosystem through changes in land formations and habitats. Differences: The movement of continents is driven by plate tectonics, while tectonic plate shifts involve the movement of sections of the Earth's lithosphere. The movement of continents is a more visible and long-term process, while tectonic plate shifts can occur more frequently and lead to more immediate geological events.
Changes in atmospheric composition throughout Earth's history, such as the increase in oxygen due to photosynthetic organisms, demonstrate the interconnectedness between living and nonliving components of the environment. Living organisms, through their metabolic processes, can alter the atmospheric composition, which in turn can influence the evolution and distribution of different life forms. This relationship highlights how life and the environment continually shape and influence each other over geological timescales.
a volcanic mountain is a cone shaped mountain formed when molten rocks erupts from a hole in the earths crust.
changes in buoyancy due to changes in density differences between the magma and surrounding rock.
mountains and stable ground- i would competely agree!
Based on temperature differences.
Justin Bieber
27
The two are completely unrelated.
by destroying the earths crust
it affects the earths ozone layer and the pollution in the air
Sun Mercury Diameter: 1,377,648 km 4,880 km Temperature: approx. 10,000 degrees (F) 333 degrees (F) Mass: 1.9891 x 10 (30) kg (333,000 earths) 3.3022 x 10 (23) kg (0.055 Earths)
subduction is when a piece of the earths crust slides back into the mantle due to density differences
Because the side of the earth you're on doesn't face the sun when it's night time.