The string does not experience any force of tension, as it balances two forces acting in the same direction. Hence, the tension is zero.
Explanation:
If tension existed in the string, it would mean that two equal but opposite forces are exerting pull in contrary directions.
When a force of f newtons is applied from the right and another force of f newtons from the left, the resulting action occurs through one force. Because there is action on the same string in opposing directions, the tension in the string can only be equal to the magnitude of the string itself.
Therefore, the string indeed has no tension since it is dealing with two forces acting in the same direction. Thus, the tension is zero.
For many years, paleontologists have maintained that the extinction of dinosaurs was primarily due to climate changes linked to gradual shifts in the arrangement of continents and oceans as a consequence of plate tectonics. Throughout the Cretaceous period, which marked the peak of dinosaur existence, extensive shallow seas intermittently covered vast portions of land. Evidence from various geological sources, such as chemical clues found in ocean floor sediments, suggests that the climate during the Late Cretaceous was warmer and more stable compared to the present. The daytime temperatures were moderate, as were the nighttime chills, with summers and winters being neither excessively hot nor incredibly cold. It is likely that the shallow continental seas helped regulate the air temperature nearby, maintaining a consistent climate.
The density of mercury in its liquid form is

We understand that the equation determining the pressure at the base of a fluid column can be expressed through Stevin's law

where

represents the density of the liquid
g signifies the acceleration due to gravity
h indicates the height of the fluid column
Given that the pressure at the lower section of the beaker is

, we can manipulate the preceding formula to calculate the height of the mercury column
Answer:
4.32 kg.m/s
Explanation:
The 2.4 kg stone moves at a speed of 3.6 m/s with an angle of 30 degrees from the x+ direction towards y+. The momentum's y-component is calculated by multiplying its mass with its velocity in the y-direction.


