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Ice cores drilled through the thickest glaciers at Earth's poles show the layers of snow that were deposited each season kind of like tree rings. The deepest layer in the deepest ice core is the oldest and in Antarctic, continuous ice cores date back at least 750,000 years.

Gases and particles of dust trapped in the snow forming the layers in the cores continuously preserves samples of the atmosphere and these can be analyzed to provide a record of the climate prevailing as each layer was deposited.

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What does a proportional time scale show?

how different parts of earths history compare to the whole world


What can rock fossils and original remains show about earths past?

it can show the futur


What are some reasons to show humans do not cause earths climate change?

Some arguments suggesting that humans do not significantly cause Earth's climate change include natural climate variability, such as changes in solar radiation and volcanic activity, which have historically influenced the climate. Additionally, proponents of this view may cite the Earth’s long climate history, indicating periods of warming and cooling that occurred before industrialization. They may also argue that climate models are unreliable and that the role of greenhouse gases might be overstated compared to other natural factors. Finally, some believe that the current climate policies are economically damaging without effectively addressing the complex nature of climate change.


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Ice cores and rock layers are both used to study Earth's history. Ice cores contain layers of ice formed over time from snowfall, providing information on past climate conditions. Rock layers, on the other hand, are formed from sediments deposited over time and can contain fossils that provide information on past life forms. Both ice cores and rock layers can help scientists understand past environmental conditions and changes.


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Milutin Milankovitch's research demonstrated that variations in Earth's orbital parameters—specifically changes in eccentricity, axial tilt, and precession—can significantly influence the planet's climate over long periods. These cyclical changes, known as Milankovitch cycles, affect the distribution and intensity of sunlight received by Earth, leading to climatic shifts such as glacial and interglacial periods. His work provided a scientific framework for understanding the natural climate changes that have occurred throughout Earth's history.

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