Sedimentary rocks are non-interlocking, whereas Igneous and Metamorphic rocks are all interlocking.
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Sedimentary rocks are typically non-interlocking, as they are made up of grains that are laid down and compacted together over time. These grains are usually loosely connected, allowing for easier weathering and erosion compared to interlocking rocks like igneous or metamorphic rocks.
Foliation, which is the alignment of minerals in a preferred orientation, is a common feature in metamorphic rocks but is not typically found in sedimentary rocks. Another feature is the presence of new minerals that form due to the heat and pressure of metamorphism, which are not present in sedimentary rocks. Metamorphic rocks also tend to have a more interlocking crystal structure compared to the more loose and granular structure of sedimentary rocks.
Sedimentary rocks are typically softer than igneous rocks because they are formed from the accumulation of sediments that are often loosely packed together. The grains in sedimentary rocks are not as tightly bonded as the crystals in igneous rocks, which makes them more prone to being weathered and eroded over time. Furthermore, sedimentary rocks often contain minerals that are less resistant to abrasion than the minerals found in igneous rocks.
Rocks formed from broken rocks are known as sedimentary rocks. These rocks are formed from the accumulation and lithification of sediments, which can include fragments of other rocks, minerals, and organic material. Common examples of sedimentary rocks formed from broken rocks include sandstone, conglomerate, and shale.
Sedimentary rocks are formed when sediments are compressed, compacted, and cemented together. Examples include sandstone, shale, and limestone.
Non-interlocking generally refers to a system or arrangement where individual components can operate independently without directly affecting or being affected by other components. In the context of transportation infrastructure, non-interlocking may refer to track segments or signals that do not rely on each other to function. This allows for more flexibility in operations and maintenance.