• Use a hose to sprinkle water on the mountain.
• Observe the change in the shape of the mountain.
The experiment most likely demonstrates the interactions between the
1) atmosphere and biosphere
2)biosphere and hydrosphere
3) geosphere and biosphere
4) hydrosphere and geosphere
The experiment most likely illustrates how the atmosphere and biosphere interact. As a result, choice (A) is the best way to respond.
A layer (or layers) of gases that encircle a planet and are maintained in place by the gravity of the celestial body is known as an atmosphere.When there is a strong gravitational pull and a cool atmosphere, a planet keeps its atmosphere. The outer region of a star, including the layers above the opaque photosphere, is known as the stellar atmosphere; low-temperature stars may have outer atmospheres with complex molecules.
Nitrogen makes up 78% of the atmosphere of Earth, along with oxygen (21%), argon (0.9%), carbon dioxide (0.04%), and trace gases. The majority of species require oxygen for respiration, whereas plants and algae use carbon dioxide for photosynthesis and lightning and bacteria execute nitrogen fixation to create ammonia, which is used to create nucleotides and amino acids.
Hence, option (A) is accurate.
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Answer: moving continents to geoscience
Explanation:
continents move around on Earth's surface and that they were once joined together as a single supercontinent
The continental drift hypothesis explains how Earth's continents have moved and changed over time.
The continental drift hypothesis illustrates how things change by explaining the movement of Earth's continents over time. This theory suggests that the continents were once joined in a supercontinent called Pangaea and have since moved to their current positions, creating new landforms and changing the shape of Earth's surface. By studying fossils, similarities in rock formations, and the shapes of coastlines, scientists have been able to map the movement of continents and understand how the Earth's surface has changed over millions of years.
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There are different kinds of rocks. Sedimentary rocks found high in the Himalayan Mountains indicate that The Earth's crust that formed these mountains was once covered with an ocean.
The Higher Himalaya is known to be the framework of the Himalayan mountains. It is said to be composed of 10-20 km-thick metamorphic rocks (e.g. schist and gneiss) and granites.
They are found at altitudes of 3000 m to about 8000 m. These rocks are known to be of Proterozoic-Cambrian age called about 2,000-500 Ma.
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Answer: The Earth's crust that formed these mountains was once covered with an ocean
• Avg, winter temperatures: 120°C
• Gravity: 1 m/s2
• Avg summer temperatures: - 100°C
• Atmosphere? No
A Could water exist on this planet? (2 points)
B. Why can or can't water exist? (3 points)
Earth is located in what is known as the habitable zone, which is far enough from the Sun to prevent water loss but not so distant that freezing temperatures force all water on the planet to occur, liquid water, which is essential for life as we know it, continues to exist on its surface.
The distance from a star at which liquid water could exist on the surfaces of circling planets is known as the "habitable zone." Habitable zones are also referred to as Goldilocks zones because they may be just suitable for life, not too hot nor too cold.
For water to continue to be a liquid, the distance at which Earth orbits the Sun is ideal. The habitable zone, sometimes known as the Goldilocks zone, is defined as being this far from the Sun.
Rocky exoplanets located in their stars' habitable zones are better candidates for detection of liquid water on their surfaces.
Up to 16 of the 1,780 extrasolar planets that have been discovered are located in the habitable zone of their star, where the conditions are ideal for supporting life. Size also matters. An atmosphere cannot exist on a planet that is too small, and it cannot exist on a world that is too large.
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Answer:
b
Explanation
no because therer is n atmospheer and the wahter is therer wherer any would evaporate