Yes, the answer is true. The remains of long-dead organisms have the potential to form fossils. Fossils are the preserved remains or traces of organisms from the past, which are typically formed in sedimentary rocks. The process of fossilization begins when an organism dies and its remains are buried in sediment, such as mud or sand. Over time, the sediments gradually harden into rock, and the organic materials of the organism are gradually replaced by minerals. This process preserves the shape and structure of the organism, creating a fossil. Fossils provide valuable insights into the history of life on Earth and can help scientists understand past environments, behaviors, and evolutionary processes.
