Final warming during the Late Paleocene led to the warmest climate in the past 65 million years. This rapid warming about 55 million years ago was likely caused by the melting of methane hydrates.
Global temperatures have risen by 5-8°C. The onset of the Paleocene-Eocene thermal maximum is associated with volcanic activity and uplift associated with the North Atlantic magmatic region, causing extreme changes in the global carbon cycle and significant increases in temperature.
A period of severe global warming 55 million years ago was caused by not one but two injections of greenhouse gases into the atmosphere. The rate of increase suggests that ancient warming events could have important lessons for today's climate.
Learn more about Paleocene here: brainly.com/question/10617208
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Your question: What is the layer that is a part of crust and mantle?
Your answer: The crust and the mantle together makes a hard and a strong zone called.....
A Lithosphere!
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The largest mountains on the continents are formed by stress deformation.
This is also know as strain, which is a process that occurs when the intensity of the stress is greater then the internal strength of the rock. This kind of activity, forming of mountains, occurs when to tectonic continental plates with same densities are colliding, so under the pressure, stress, they create, the area of collision is lifting up.
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when the temperature of thy rising air falls below the dew point.
Answer:
Because at those latitudes the jet stream, which is a very high altitude wind, always blows from the West to the East. The planes moving at a constant air speed thus go faster in the West-East direction when they are moving with the wind than in the opposite direction.
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