Answer:
Ideas, biography or autobiography, personal experiences, and humor.
Explanation:
A non-fiction can be defined as a piece of work that is not based on imagination but rather it is instructional and based on true events or happenings. A non-fiction comprises of real places, people, and events. These texts contain facts.
<u>There are two types of non-fiction: literary nonfiction and informative non-fiction</u>.
The major topics that are used to write any non-fiction are ideas, biography and autobiography, personal experiences, and humor.
Some examples of nonfiction are The Diary of A Young Girl, Unbroken: A World War II Story of Survival, Resilience, and Redemption, etc.
Answer:
Community colleges were often perceived as nothing more than the poor man's path to higher education. That perception diminished the schools' images and is one part of the community college stigma.
Honestly all of them but A is the most valid answer since most of us contribute to the entirety of social media.
An "appositive" can be defined as a noun or a whole noun phrase used to rename or clarify (by giving an explanation) found next to another noun, usually separated by a coma, dash or a bracket. One of the correct answers to the question would be option B, since the noun would be Garage and the appositive would be "the most cluttered room in the house" and it is added correctly because it is separated from the noun by a comma. The other would be option D since the appositive would be "Adam" and the noun phrase would be "Joey's brother", it is correctly added because Adam renames the noun phrase "Joey's brother" and it is next to it separated by a comma.
Option A is not correct because the word spider should have been next to huge insect and option C does not contain an appositive.
Answer:The distribution of earthquakes across the globe is shown in Figure 11.7. It is relatively easy to see the relationships between earthquakes and the plate boundaries. Along divergent boundaries like the mid-Atlantic ridge and the East Pacific Rise, earthquakes are common, but restricted to a narrow zone close to the ridge, and consistently at less than 30 km depth. Shallow earthquakes are also common along transform faults, such as the San Andreas Fault. Along subduction zones, as we saw in Chapter 10, earthquakes are very abundant, and they are increasingly deep on the landward side of the subduction zone.
General distribution of global earthquakes
Figure 11.7 General distribution of global earthquakes of magnitude 4 and greater from 2004 to 2011, colour coded by depth (red: 0-33 km, orange 33-70 km, green: 70-300 km, blue: 300-700 km)
Explanation:
