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How long does it take to form sandstone?

It typically takes millions of years to form sandstone. It is a sedimentary rock formed by the accumulation and cementation of sand grains over time. Factors such as pressure, temperature, and the presence of minerals influence the process.


Observing animal tracks is an example of what observation?

This is an example of indirect observation, where evidence of animal presence is inferred through the tracks left behind rather than directly observing the animals themselves.


Can fish see outside of the aquarium?

Definitely. You can see evidence of this if you watch how fish react when you approach the aquarium. They are often either fearful, or they react by anticipating being fed. In any case, they react to the presence of people near the tank, indicating that they can see out of the tank.


How can a taxonomist use embryo logical evidence in classifying an organism?

A taxonomist can use embryological evidence by examining the developmental stages of organisms to identify similarities and differences in their embryonic forms. This comparative analysis can reveal evolutionary relationships, as closely related species often exhibit similar embryonic development patterns. By assessing features such as the formation of structures, timing of developmental events, and the presence of embryonic layers, taxonomists can refine classifications and understand the evolutionary history of the organisms. Thus, embryological evidence serves as a crucial tool in elucidating phylogenetic relationships among taxa.


How long will it take for a mouses dead body to decompose?

The decomposition of a mouse's dead body can vary based on environmental conditions such as temperature, humidity, and presence of scavengers. In general, it can take a few weeks to a few months for a mouse's body to fully decompose.

Related Questions

What two things do sedimentary rocks record?

Sedimentary rocks can record information about the environment in which they formed, such as the presence of water, wind, or ice. They can also preserve evidence of the organisms that lived in that environment, including fossils.


What is the universal feature of sedimentary rocks?

The presence of layers is the universal feature of all sedimentary rock.


What evidence for the age of the Earth is indicated by the fact that sedimentary rock is found on mountain tops?

The presence of sedimentary rock on mountain tops provides evidence for the Earth's age through the process of plate tectonics and uplift. Sedimentary rocks form from the accumulation of sediments in bodies of water over long periods. When tectonic plates collide, they can push these sedimentary layers upwards, creating mountains. This geological activity, along with the slow processes of erosion and sedimentation, suggests that the Earth has undergone significant changes over millions of years, supporting an ancient Earth timeline.


What condition change igneous sedimentary to metamorphic rock?

The conditions that change igneous or sedimentary rock into metamorphic rock include high temperature, high pressure, and the presence of chemically active fluids. These conditions cause the minerals in the original rock to recrystallize, forming new minerals and textures characteristic of metamorphic rocks.


Which observed feature would provide the evidence of crustal stability?

marine fossils at elevations high above sea level


Geologists can use sedimentary rock to lean about climate in the past?

Geologists can analyze sedimentary rocks to infer past climate conditions by examining features such as grain size, composition, and layering. These rocks often contain fossils and sedimentary structures that indicate environmental conditions at the time of deposition, such as the presence of water or vegetation. For example, coal deposits suggest lush, swampy environments, while desert sandstones indicate arid conditions. By studying these characteristics, geologists can reconstruct historical climate patterns and changes over geological time scales.


Sedimentary rocks record past geological events and what else?

Sedimentary rocks also provide insights into past environmental conditions, such as climate, the presence of water, and the types of organisms that may have lived in that area. Additionally, they can contain important resources such as fossil fuels, minerals, and groundwater.


What are appropriate means for leaving evidence of presence (Select all that apply?

What are appropriate means for leaving evidence of presence? (Select all that apply)


A variety of sunset colors is evidence for a variety of?

A variety of sunset colors is evidence for a variety of atmospheric conditions, such as the presence of different sized particles and gases in the air. These conditions affect how sunlight is scattered, leading to the colorful display we see during sunsets.


When sedimentary rock is buried it may change into metamorphic rock. What causes the change?

The change from sedimentary rock to metamorphic rock occurs due to increased temperature and pressure as the rock is buried deeper in the Earth's crust. These conditions cause physical and chemical changes in the minerals within the rock, resulting in new mineral formations and textures. Additionally, the presence of fluids can facilitate chemical reactions that further contribute to metamorphism. This process can create various types of metamorphic rocks, depending on the original sedimentary rock and the specific conditions it undergoes.


What evidence can you find if it is a sedimentary rock?

Sedimentary rocks can be identified by features such as layering or stratification, which results from the accumulation of sediments over time. Fossils often embedded within these rocks indicate their formation in environments where life existed. Additionally, sedimentary rocks may exhibit grainy textures or contain minerals like calcite or quartz, which are common in sediment deposits. The presence of ripple marks or mud cracks can also suggest deposition in water or terrestrial environments.


Why is siderite important?

Siderite, an iron carbonate mineral, is significant primarily as a source of iron. It is often found in sedimentary iron deposits and can be processed to extract iron for steel production. Additionally, siderite has applications in the fields of geology and mineralogy, providing insights into geological processes and environments. Its presence can also indicate specific conditions of formation in sedimentary basins.