Answer:
Potential energy into kinetic energy.
Explanation:
The uplifting of water occurs due to earthquake in the sea floor is refers to potential energy while on the other hand, the movement of water to the land in the form of waves is the kinetic energy. So we can see that the transformations of energy occurs from potential energy due to earthquake into kinetic energy occurs due to movement of water in the form of giant waves (tsunami).
liver
stomach
lungs
Answer:
I WOULD SAY
A: BLOOD
IS THE ANSWER
Answer: B The Geological Time Scale
Explanation:
experimental design, be sure to:
• state a hypothesis to be tested
• describe how the control group will be treated differently from the experimental group
• identify the independent variable in the experiment
• identify the type of data that will be collected
Answer
• state a hypothesis to be tested
Development rate increases faster with temperature that growth rate
• describe how the control group will be treated differently from the experimental group
The control group will be raised at 8 different temperatures to assess their size at maturity, and their asymptotic size.
• identify the independent variable in the experiment
3 clonal lines that differ in asymptotic size and growth rate.
• identify the type of data that will be collected
Measurements of the individual length of Daphnia
Explanation
In this experiment, the temperature-size rile(TSR) was utilized where it will be found that responses on temperature size observed at maturity is different from that manifested at asymptotic size. It will be observed that thermal shift in resources allocation may completely or partly result to a thermal plasticity in maturity size. Moreover, it will be seen that thermal plasticity in asymptotic size is controlled by temperature related challenges.
A volcanic eruption can have a significant impact on an ecosystem, disrupting its balance and affecting the various organisms that inhabit it. The exact effects of the eruption on the ecosystem will depend on various factors, such as the size of the eruption, the type of volcano, the location of the eruption, and the surrounding environment.
One of the most immediate and obvious impacts of a volcanic eruption is the destruction of the local vegetation and wildlife. The intense heat, ash, and lava can kill plants and animals directly or destroy their habitats. This can lead to a decline in biodiversity, which can have long-term consequences for the ecosystem.
Volcanic eruptions can also release large amounts of gases and particles into the atmosphere, which can affect air quality and climate patterns. For example, sulfur dioxide and other gases can react with water vapor to form sulfuric acid, which can lead to acid rain. Ash particles can block sunlight and reduce photosynthesis, affecting the growth and survival of plants.
In addition, volcanic eruptions can trigger other environmental hazards, such as landslides, mudflows, and tsunamis. These events can cause further damage to the ecosystem and disrupt the balance of the local environment.
Overall, the impact of a volcanic eruption on an ecosystem can be severe and long-lasting. However, ecosystems are also resilient and can often recover over time, depending on the severity and duration of the eruption, as well as the capacity of the local organisms to adapt and survive.
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