i was taught by my amazing science teacher ..lol... that the 2 original gasses were methane and ammonia. hope this is a good enough answer. its as accurate as superman! :)
-stachova witness
Hydrogen gas was not part of Earth's original atmosphere. The early atmosphere primarily consisted of carbon dioxide, water vapor, and nitrogen, among other gases. Hydrogen was likely lost to space due to its low mass and the sun's radiation.
Gases like oxygen, methane, and carbon dioxide were not part of Earth's original atmosphere. These gases were introduced over time through processes like photosynthesis, volcanic activity, and industrial activity.
Earth's original atmosphere is believed to have been formed by outgassing from the planet's interior, which released gases such as water vapor, carbon dioxide, and nitrogen. These gases accumulated around the young Earth to create the primordial atmosphere.
The primitive Earth's atmosphere is hypothesized to have consisted mostly of gases like carbon dioxide, water vapor, nitrogen, and methane. These gases played a key role in shaping the early Earth's climate and environment. Over time, these gases changed through processes like volcanic activity and the emergence of photosynthetic organisms.
It is believed that the early Earth's atmosphere likely consisted of gases like water vapor, carbon dioxide, nitrogen, and methane. Over time, as the Earth cooled and life forms evolved, the composition of the atmosphere changed due to processes like photosynthesis.
Hydrogen gas was not part of Earth's original atmosphere. The early atmosphere primarily consisted of carbon dioxide, water vapor, and nitrogen, among other gases. Hydrogen was likely lost to space due to its low mass and the sun's radiation.
The Earth's early atmosphere consisted of Carrbon Dioxide, methane, sulphur, ammonia, nitrogen and smaller amounts (aprox. 0.05%) of other gases.
The original gases on Earth 4.6 billion years ago likely consisted of hydrogen, helium, methane, and ammonia. These gases were present during the planet's formation and early geological processes. Over time, the atmosphere evolved into what we know today through volcanic activity and biological processes.
Gases like oxygen, methane, and carbon dioxide were not part of Earth's original atmosphere. These gases were introduced over time through processes like photosynthesis, volcanic activity, and industrial activity.
The primitive Earth atmosphere is hypothesized to have consisted of gases like nitrogen, carbon dioxide, water vapor, and small amounts of methane and ammonia. These gases eventually formed the basis for the development of more complex atmospheric compositions and the evolution of life on Earth.
Earth's original atmosphere is believed to have been formed by outgassing from the planet's interior, which released gases such as water vapor, carbon dioxide, and nitrogen. These gases accumulated around the young Earth to create the primordial atmosphere.
The primitive Earth's atmosphere is hypothesized to have consisted mostly of gases like carbon dioxide, water vapor, nitrogen, and methane. These gases played a key role in shaping the early Earth's climate and environment. Over time, these gases changed through processes like volcanic activity and the emergence of photosynthetic organisms.
It is believed that the early Earth's atmosphere likely consisted of gases like water vapor, carbon dioxide, nitrogen, and methane. Over time, as the Earth cooled and life forms evolved, the composition of the atmosphere changed due to processes like photosynthesis.
Oparin proposed that the Earth's early atmosphere consisted of water vapor, methane, ammonia, and hydrogen. These gases are believed to have played a role in the chemical reactions that led to the formation of organic molecules necessary for life.
The first atmosphere of Earth is thought to have consisted mainly of hydrogen and helium, with smaller amounts of methane and ammonia. Over time, volcanic activity released gases such as carbon dioxide and water vapor, altering the composition of the atmosphere.
The main component of Earth's original atmosphere was likely hydrogen and helium. Over time, these gases were largely lost to space, and the atmosphere evolved to primarily consist of nitrogen and oxygen as a result of volcanic outgassing and the development of life on Earth.
Oparin's hypothesis suggested that early Earth's atmosphere lacked free oxygen. Instead, it consisted of gases like methane, ammonia, hydrogen, and water vapor.