Which of the following types of news was not considered sensationalistic?

objective journalism
yellow journalism
the penny press
satirical journalism

Objective journalism is the type of news which is not considered sensationalistic.

Option A

Explanation:

Objective journalism is the type of journalism where the objectives of the journalism are given more importance. The objectives are that the news should be presented by the journalists to the people to make them aware of the events which are happening in the world.

The news should be presented irrespective of the fact that whether the journalists believe in the news or the facts or not. The news presented in this manner are not biased and are presented in a neutral way.

the earth’s crust is broken into separate pieces called tectonic plates (fig. 7.14). recall that the crust is the solid, rocky, outer shell of the planet. it is composed of two distinctly different types of material: the less-dense continental crust and the more-dense oceanic crust. both types of crust rest atop solid, upper mantle material. the upper mantle, in turn, floats on a denser layer of lower mantle that is much like thick molten tar.

each tectonic plate is free-floating and can move independently. earthquakes and volcanoes are the direct result of the movement of tectonic plates at fault lines. the term fault is used to describe the boundary between tectonic plates. most of the earthquakes and volcanoes around the pacific ocean basin—a pattern known as the “ring of fire”—are due to the movement of tectonic plates in this region. other observable results of short-term plate movement include the gradual widening of the great rift lakes in eastern africa and the rising of the himalayan mountain range. the motion of plates can be described in four general patterns:

collision: when two continental plates are shoved together

subduction: when one plate plunges beneath another (fig. 7.15)

spreading: when two plates are pushed apart (fig. 7.15)

transform faulting: when two plates slide past each other (fig. 7.15)

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