What happens when Victor goes out in a boat to dispose of the female creature's remains? Where does he end up? What happens when helands?

Answers

Answer 1

When Victor goes out in a boat to dispose of the female creature's remains, he ends up in the middle of the ocean. He intends to throw the remains overboard and let them sink to the bottom of the sea, but he is interrupted by the appearance of the creature, who is seeking revenge for Victor's abandonment of her.

The creature confronts Victor and explains that he will not stop pursuing him until he creates a mate for him, as they had previously agreed upon. Victor is initially resistant to the idea, but eventually agrees to create a companion for the creature, fearing for his own safety. This decision sets in motion a series of events that lead to tragic consequences for all involved. Ultimately, Victor's attempt to dispose of the remains of the female creature only serves to further complicate the already fraught relationship between him and the creature.

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Related Questions

the density of seawater increases with ________ temperature and ________ salinity. group of answer choices A. decreasing; decreasing
B. decreasing; increasing
C. increasing; decreasing
D increasing; increasing

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The solution that is right is B. With a drop in temperature and a rise in salinity, seawater becomes denser.

                        The density of seawater is significantly influenced by temperature and salinity. As the temperature rises, seawater expands and becomes less dense. On the other hand, as the temperature drops, seawater contracts and becomes denser. This is the result of the thermal expansion and contraction of water molecules.

                        Salinity, on the other hand, has a different effect on the density of saltwater. As salinity increases, more dissolved salts are present in the water, increasing its density. Higher salinity leads to more dissolved ions and particles, which increases the water's overall mass without significantly changing its volume.

                         The result is a body of water that is denser since seawater's density grows with rising salinity and dropping temperature.

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The density of seawater increases with C) increasing temperature and decreasing salinity. This means that as the temperature of seawater increases, its density also increases, making it heavier.

On the other hand, as the salinity of seawater decreases, its density also decreases, making it lighter. This is because salt in seawater increases its density, while temperature affects the space between water molecules, making it more compact and thus increasing its density. The density of seawater plays a crucial role in ocean currents, as it affects the water's movement and distribution, which in turn affects the climate. It is important to monitor the changes in seawater density, as it can have significant impacts on marine life and ecosystems. Therefore, understanding the relationship between seawater density, temperature, and salinity is vital for scientific research and ocean management.

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an earthquake has just occurred. seismic waves from the earthquake are detected at two recording stations. at recording station a, . at recording station b, . which recording station is farther away from the epicenter?

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To determine which recording station is farther away from the epicenter, we need to understand how seismic waves travel. There are two types of seismic waves: primary waves (P-waves) and secondary waves (S-waves).

P-waves travel faster than S-waves, so they arrive at the recording station first. By measuring the time difference between the arrival of the P-waves and the S-waves at each recording station, we can calculate the distance to the epicenter.
Assuming that both recording stations are equidistant from the epicenter, the station that receives the seismic waves later would be farther away. This is because the waves would have traveled a longer distance to reach that station, resulting in a longer delay between the arrival of the P-waves and the S-waves.
Therefore, we need more information about the arrival times of the seismic waves at each recording station to determine which one is farther away from the epicenter.

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