Seafloor spreading

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    Neotectonics In Australia

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    not uniform across the continent. Geologic Setting The continent of Australian is flank on its southern, eastern and western, edges by oceanic layer, which started to frame at c. 155 – 165 Ma (Stagg et al., 1999; Müller et al., 2000). The spreading of Seafloor stopped at c. 55 Ma, aside from in the south where Australia keeps on moving north far from Antarctica. Toward the north, a Tertiary to Recent active edge is being made by the Australian and Eurasian plate collision at the Timor area,…

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    What Is The Carbon Cycle?

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    Carbon Cycling Internal Achievement Standard Science 90953: Demonstrate understanding of carbon cycling Carbon Cycling Internal What is the Carbon Cycle? Carbon is a key component in all living organisms and can be found in both living and nonliving organisms. Organisms will continue to contain carbon even when they change or decay. Carbon is found in a variety of living things and can exist as a solid e.g coal and diamonds, a liquid e.g crude oil or a gas, for example CO2…

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    Coral Reef Climate Change

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    Our industrialized lifestyle leading to climate change is something we can adapt to, but it’s causing a change that the Coral Reefs are not acclimated to live in.The changes and industrializations we bring affects the climate. This problem has been named and clarified as climate change. Since the industrial revolution our climate has changed drastically. Industrial waste is now a necessary problem that collides with our daily life. This lifestyle can be too much for the fragile ecosystems our…

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