about 10 and up
The ages of the rocks become older the farther the way they are from the ridges. The closer they are the younger it is. This leaves evidence to the seafloor spreading theory.
The ages of the rocks become older the farther the way they are from the ridges. The closer they are the younger it is. This leaves evidence to the seafloor spreading theory.
Renaissance
The first formal articulation of the theory of glacial ages was in the early 19th century by Swiss geologist Louis Agassiz around the 1840s. He proposed that vast ice sheets had once covered large parts of the Earth during what he termed "Ice Ages."
because
the ages of the rocks become increasingly older in samples obtained farther from the ridge and the younger had just come out the ridge.
it is like pi a never ending number stretching on like the string theory into the infnity of the ages.
The currently accepted theory is that ice ages are caused by changes in Earth's orbit and tilt, known as Milankovitch cycles. These cycles affect the amount of sunlight reaching different parts of the Earth, leading to fluctuations in temperature and the growth and retreat of ice sheets. Other factors, such as volcanic activity and variations in greenhouse gas concentrations, can also influence the climate and contribute to the onset of ice ages.
The ages of the rocks become older the farther the way they are from the ridges. The closer they are the younger it is. This leaves evidence to the seafloor spreading theory.
A. explaining the theory of conic sections developed by Apollonius
A. explaining the theory of conic sections developed by Apollonius
they occur as part of natural climate cycles caused by changes in Earth's orbit, tilt, and precession. These variations affect how sunlight is distributed on Earth's surface, leading to long-term changes in temperature and ice volume. The theory helps explain the periodicity of ice ages over geological time scales.