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Angular conformity forms when sedimentary layers are deposited over tilted or folded layers that have been eroded. The newer layers are laid down horizontally on top of the older, slanted strata, creating a distinct angular relationship between the two. This geological feature is often seen in regions where tectonic forces have altered the Earth's crust, resulting in a visible angular discordance between the layers. It serves as important evidence of geological history and processes.

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