The Law of _____ states that in horizontal layers of sedimentary rock, each layer is ______ than the layer above it and ______ than the layer below it.

The Law of Superposition states that in horizontal layers of sedimentary rock, each layer is younger than the layer above it and older than the layer below it.

The Law of Superposition states that in horizontal layers of sedimentary rock, each layer is older than the layer above it and younger than the layer below it.

The Law of Superposition states that in horizontal layers of sedimentary rock, each layer is older than the layer above it and younger than the layer below it.

To understand how this law works, we can look at the way sedimentary rocks are formed. Sedimentary rocks are formed through the deposition and accumulation of sediments, such as fragments of rocks, minerals, and organic material, over time. As these sediments settle, they form distinct layers, with each layer representing a different period of deposition.

In order to determine the relative ages of these layers, geologists use the principle of superposition. This principle states that when undisturbed, the oldest rocks are found at the bottom, while the youngest rocks are located at the top of a sequence. This is because as sedimentary layers accumulate, each new layer is deposited on top of the existing layers, causing a stack of layers to form.

To apply the Law of Superposition, geologists need to carefully study the rock layers and make observations. By examining the sequence of layers, they can determine the relative order of their formation. The lowermost layer is the oldest because it was deposited first, while the uppermost layer is the youngest because it was deposited last.

By understanding the Law of Superposition and examining the arrangement of sedimentary rock layers, geologists can reconstruct the geological history of an area and establish a relative timeline of events. This is an important tool in determining the ages of fossils, understanding past environmental changes, and interpreting Earth's geological past.