Siple Ice Core Ice cores form from the accumulation of snow and ice over many years which traps air bubbles from previous time periods. Ice cores provide a great deal of information about the previous conditions of atmosphere, climate and geologic events through the capture of the atmosphere in the bubbles as well as through trapping dust and pollen. You will be using data from the Siple core site in Antarctica. Note that the age of the layer get progressively older from the top layer to the bottom layer. New snow accumulates atop older snow and turns into ice due to internal pressure. Click on each layer to reveal the layer’s age and CO 2 composition by volume. Use the data to complete your graph. 320 310 300 290 280 270 260 250 1725 1825 1925 2025 Use the arrows below the core if you need to return to a slide. 3