Which can be excluded from the list of underground materials that holds water in the Ogallala aquifer?(1 point)
Responses
mineral
mineral
gravel
gravel
silt
silt
sand
1. D.aquifer
2. B. mineral
3. B. subsidence
4. B. It removes water more quickly than it can be replaced.
5. B. It could cause faults to be less stable,resulting in earthquakes.
Connections Academy Science, Unit 2, Lesson 12 Quick Check
Wsp yall for 2024 they changed the question for #2. The new question is: Which can be excluded from the list of underground materials that holds water in the Ogallala aquifer?
silt
gravel
sand
granite
(The answer is granite I just took the quick check) all the other answer from all the other people except question #2 are right.
mineral
Nah "GGs guys". You got to be more specific when you're giving answers. Like, if you're on Connexus or not. Here are the real answers for Connections Academy:
1: C/ Aquifer
2: D/ Mineral
3: A/ Subsidence
4: C/ It removes water more quickly than it can be replaced.
5: C/ It could cause faults to be less stable, resulting in earthquakes.
Well, well, well! It looks like we have a little game of "Guess the Exclusion" here! Out of all the options you mentioned, the one that can be excluded from the list of underground materials that holds water in the Ogallala aquifer is...drum roll, please...gravel! Sorry, gravel, but you're not holding water in this aquifer party. Better luck next time!
C
B
C
D
A
These are right don't trust other guys 🌹🌹
Anonymously is correct and authentic. I got 100%. You guys can trust me and anonymously.
To determine which material can be excluded from the list of underground materials that holds water in the Ogallala aquifer, we need to understand the characteristics of the aquifer and how different materials affect water storage.
The Ogallala aquifer is a vast underground water source located beneath the Great Plains in the United States. It consists of a mixture of different materials, including minerals, gravel, silt, and sand. These materials have varying permeability, which affects their ability to hold and transmit water.
In general, materials with higher porosity and permeability have a greater capacity to store and transmit water. Gravel and sand are known for their high porosity, which allows water to flow through them easily and be stored within their spaces. Silt has intermediate porosity and permeability, offering some potential for water storage. Minerals, on the other hand, typically have low porosity and permeability, making them less suitable for holding water.
Based on this information, we can conclude that the material that can be excluded from the list of underground materials that holds water in the Ogallala aquifer is mineral. Minerals have low porosity and permeability compared to the other options mentioned (gravel, silt, and sand), and thus are less likely to hold water in the aquifer.