Answer:B. Intensity
Explanation:
The Intensity of an earth quake refers to the noticeable and severity effects of damage on man made structures, natural(crops and livestock) and human life at different locations. To measure the intensity of an earthquake, the Modified Mercalli Intensity Scale is used and consists of 12 levels of intensity(in roman numerals) that rank the extent of damage based on observable effects with the higher levels based on structural damage.
A Level I -V1 Intensity on the scale will show slight damages to properties and treatable injuries to people, but going higher on the scale above VI shows total damage and destruction to structures and human life.
Explanation:
A filmmaker spends very long hours making sure the film is being shot in a way that will provide entertainment for the audience and will highlight the actors and actresses' strengths. They will see each film through, from where the film is shot, to how the script will be played out, to what actors and actresses best fit the roles of the characters. The filmmaker also manages the financial end of the production.
Eligibility to become Filmmaker
Candidates who are motivated and have a strong passion for films, theatre and arts can get into the film industry either through talent or by the means of formal education. Aspiring directors/producers can gain experience by assisting renowned directors or by joining school production.
Some producers assist in production houses to build a career. Apart from this a bachelor’s degree in fine arts can enhance one's knowledge and increase their skill set. Depending upon one’s career interest one can go for a bachelor’s degree or for MFA degree courses.
Answer:
D. Subjective information
Explanation:
Answer:
D. Seafloor bedrock is younger near the ridge and older farther away.
Explanation:
In a divergence boundary oceanic plates or continental plates move apart. The plates moves apart causing an uprising of molten magma to form a new crust. The divergent movement of plate is very prevalent in the oceanic plates.
The plates in the oceanic crust moves apart due to the up welling of aesthenosphere materials . These aesthenosphere materials(molten magma) are introduce to the ocean floor through the mid oceanic ridge . As this materials are introduced through cracks and fissures, the plates continue to drift apart. The molten magma later solidified to form a new crust closer to the oceanic ridge. This is why sea floor bedrock closer to the ridge is younger as new rocks are formed here. But as one move farther away from the ridge the rocks become older. This phenomenon provide ample evidence that the seafloor is spreading. The older rocks found father away from the ridge proves the seafloor has been spreading given way for new rocks closer to the ridge.
