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Scottish geologist James Hutton, often referred to as the father of modern geology, proposed the theory of uniformitarianism in the late 18th century. He argued that the Earth must be extremely old, as geological processes like erosion and sedimentation had occurred gradually over vast periods of time.

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How old is the the earth and how did scientist know?

The Earth is approximately 4.54 billion years old. Scientists determine the age of the Earth through various methods, including radiometric dating of rocks and meteorites, studying the decay of radioactive isotopes, and analyzing the composition of minerals.


How did scientist find out how old earth was?

Scientists determine the age of the Earth through various methods, including radiometric dating of rocks and meteorites, studying the decay of radioactive isotopes, and analyzing the composition of materials on Earth and in space. These methods provide estimates of Earth's age to be around 4.5 billion years.


How did old earth look like?

Old Earth, also known as "Paleo-Earth," looked very different from the Earth we know today. It had a vastly different climate, with different land formations, vegetation, and animal species. Continents were arranged differently, and there were different geological and environmental conditions.


What terms identifies a viewpoint based on the belief in a very old earth?

The term that identifies a viewpoint based on the belief in a very old earth is "deep time." This concept proposes that geological time spans are immensely long, encompassing billions of years. Scientists use this perspective to explain the gradual changes and processes that have shaped the Earth over its history.


What scientist suggested that the earth is over 6000 years old?

James Hutton, a Scottish geologist, suggested that the Earth is much older than 6000 years in the late 18th century. This concept challenged the prevailing belief in a young Earth based on religious interpretations. His work laid the foundation for modern geology and our understanding of Earth's long history.