Marine sediment refers to particles that settle and accumulate on the ocean floor. These sediments originate from various sources, including terrestrial processes (like weathering and erosion of rocks on land), biological activity (such as the remains of marine organisms), and chemical precipitation from seawater. Marine sediments can be classified into several types based on their composition and origin: 1. **Terrigenous Sediments**: These sediments are derived from land-based sources and are primarily composed of mineral particles from rocks and soils.
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