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How do living and nonliving things impact the process of weathering and erosion?
Living things impact weathering and erosion by contributing to the breakdown of rocks through processes like root wedging and burrowing. Nonliving factors such as water, wind, and temperature fluctuations also play a significant role in weathering and erosion by physically breaking down and transporting rocks and sediments. Together, these factors shape the landscape over time.
How do parts of living things become fossilized?
When an organism dies, it can become buried in sediment which helps protect it from decay. Over time, minerals from the surrounding environment can seep into the organism's tissues, gradually replacing them and forming a fossil. The process of fossilization can take millions of years.
Why is cool not considered to be a mineral?
Cool is not considered a mineral because it is not a naturally occurring inorganic solid with a specific chemical composition and crystal structure. Cool is a subjective term used to describe something that is stylish, impressive, or attractive, and does not fit the criteria of a mineral.
What is a rock formed from the remains of living things called?
A rock formed from the remains of living things is called a sedimentary rock. This type of rock is formed through a process known as lithification, where sediments such as dead plants or animals accumulate and become compacted over time. Examples include limestone, coal, and chalk.
What are three things that the sediments in sedimentary rocks may be made of?
Sediments in sedimentary rocks may be made of fragments of other rocks, minerals, and organic material like remains of plants and animals. These sediments are typically transported and deposited by processes such as erosion, weathering, and deposition.
What kind of rock is made when rock minerals and remains of living things are made when these sediments are cemented together?
sedimentary rock
How living things are put together?
living things are put together from cells
Chalk formed from sediments made of skeletons of microscopic living things in the ocean must be a?
Chalk formed from sediments made of skeletions of microscopic living things in the ocean must be a(n) organic rock.
Does the composition of a sedimentary rock depend upon the composition of the rocks and the living things its sediments came from?
It is true that the composition of a sedimentary rock depends upon the composition of the rocks and living things its sediments come from. Sedimentary rocks form through lithification.
How does living and non-living things parts of an ecosystem work together?
An ecosystem is a community of living and non-living things that work together – it consists of abiotic (soil, water, air) and biotic parts (flora, fauna)
How do living and nonliving things impact the process of weathering and erosion?
Living things impact weathering and erosion by contributing to the breakdown of rocks through processes like root wedging and burrowing. Nonliving factors such as water, wind, and temperature fluctuations also play a significant role in weathering and erosion by physically breaking down and transporting rocks and sediments. Together, these factors shape the landscape over time.
What are the living and nonliving things around you called?
Living things are called organisms, while nonliving things are called abiotic components. These components together make up an ecosystem.
Can nonliving things organize?
No, non-living things cannot do things like organize themselves. They may be composed of organized units, such as atoms or molecules, but they don't organize together like living things do.
What are the steps that turn sediment into rock?
Sedimentary rocks are formed by the lithification (cementing, compacting, and hardening) of existing rock or the bones, shells, and pieces of formerly living things. Rocks are weathered and eroded into tiny particles which are then transported and deposited along with other pieces of rock called sediments. Sediments are cemented together and compacted and hardened over time by the weight and pressure of up to thousands of feet of additional sediments above them. Eventually, the sediments are lithified and become solid sedimentary rock. These sediments that come together are known as clastic sediments. Sediments usually sort themselves by the size of the particles during the deposition process so sedimentary rocks tend to contain similarly sized sedimentary particles. An alternative to clastic sediments are chemical sediments which are minerals in solution that harden. The most common chemical sedimentary rock is limestone, which is a biochemical product of calcium carbonate created by the parts of dead creatures. Approximately three-quarters of the earth's bedrock on the continents is sedimentary.
How do living things in an ecosystem interact with each other in an ecosystem?
they stay together
Sediments is another name for these little things?
particles.
What is the term for the reamins of things found in a rock?
Sediments
