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In the fantasy manga and anime series, "Oshi no Ko," the character Bojji has a significant impact on the storyline. Bojji is the prince of the kingdom of Boro, but unlike his peers, he is born without the ability to wield magic. His lack of magical powers makes him an outcast and a disappointment to his father, the king. However, despite his apparent disadvantage, Bojji proves himself to be a valuable and resourceful protagonist. The main idea of whether Bojji has his magic removed is a pivotal point in the series. **Although Bojji initially lacks magic, he undergoes a transformation later on that grants him the ability to harness a unique type of magic called "Irumyuui.

Mafic va metal

**Although Bojji initially lacks magic, he undergoes a transformation later on that grants him the ability to harness a unique type of magic called "Irumyuui."** This newfound power allows Bojji to control and manipulate gravity, turning his disability into a strength. With Irumyuui, Bojji gains the strength to protect himself and those he cares about, as well as to combat the numerous obstacles and enemies he encounters throughout the plotline.

felsic and mafic rocks

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Also known as: acid rock, felsite, silicic rock Written and fact-checked by The Editors of Encyclopaedia Britannica

Encyclopaedia Britannica's editors oversee subject areas in which they have extensive knowledge, whether from years of experience gained by working on that content or via study for an advanced degree. They write new content and verify and edit content received from contributors.

The Editors of Encyclopaedia Britannica Last Updated: Article History Table of Contents Category: Science & Tech Related Topics: granite rhyolite dacite granodiorite quartz monzonite . (Show more)

felsic and mafic rocks, division of igneous rocks on the basis of their silica content. Chemical analyses of the most abundant components in rocks usually are presented as oxides of the elements; igneous rocks typically consist of approximately 12 major oxides totaling over 99 percent of the rock. Of the oxides, silica (SiO2) is usually the most abundant. Because of this abundance and because most igneous minerals are silicates, silica content was used as a basis of early classifications; it remains widely accepted today. Within this scheme, rocks are described as felsic, intermediate, mafic, and ultramafic (in order of decreasing silica content).

In a widely accepted silica-content classification scheme, rocks with more than 65 percent silica are called felsic; those with between 55 and 65 percent silica are intermediate; those with between 45 and 55 percent silica are mafic; and those with less than 45 percent are ultramafic. Compilations of many rock analyses show that rhyolite and granite are felsic, with an average silica content of about 72 percent; syenite, diorite, and monzonite are intermediate, with an average silica content of 59 percent; gabbro and basalt are mafic, with an average silica content of 48 percent; and peridotite is an ultramafic rock, with an average of 41 percent silica. Although there are complete gradations between the averages, rocks tend to cluster about the averages. In general, the gradation from felsic to mafic corresponds to an increase in colour index (dark-mineral percentage).

Britannica Quiz (Bed) Rocks and (Flint) Stones

The fine-grained or glassy nature of many volcanic rocks makes a chemical classification such as the felsic-mafic taxonomy very useful in distinguishing the different types. Silica content is especially useful because the density and refractive index of natural glasses have been correlated with silica percentage; this makes identification possible in the absence of chemical data. For similar determinations, glasses can also be prepared in the laboratory from crystalline rocks.

The influence of silica content on the particular minerals that crystallize from a rock magma is a complex interaction of several parameters, and it cannot be assumed that rocks with the same silica content will have the same mineralogy. Silica saturation is a classification of minerals and rocks as oversaturated, saturated, or undersaturated with respect to silica. Felsic rocks are commonly oversaturated and contain free quartz (SiO2), intermediate rocks contain little or no quartz or feldspathoids (undersaturated minerals), and mafic rocks may contain abundant feldspathoids. This broad grouping on the basis of mineralogy related to silica content is used in many modern classification schemes.

This article was most recently revised and updated by John P. Rafferty.

Encyclopaedia Britannica's editors oversee subject areas in which they have extensive knowledge, whether from years of experience gained by working on that content or via study for an advanced degree. They write new content and verify and edit content received from contributors.
Stranger thigs

The removal of Bojji's magic, or lack thereof, is a defining characteristic that shapes his identity and contributes to his growth as a character. **It symbolizes the challenges he faces due to his disability and highlights the importance of determination, perseverance, and inner strength.** Bojji's journey becomes a tale of self-discovery and self-acceptance, as he learns to embrace his differences and find his own path to success. Instead of focusing on his lack of magical powers, Bojji relies on his intelligence, empathy, and determination to overcome obstacles and prove himself worthy of his position as prince. Overall, the topic of whether Bojji has his magic removed plays a significant role in "Oshi no Ko." **While Bojji does not possess conventional magical abilities at the start of the story, he later gains a unique form of magic that sets him apart and allows him to flourish as a character.** The narrative explores themes of identity, self-acceptance, and personal growth as Bojji navigates the challenges associated with his lack of magical powers. Through his journey, Bojji teaches us that strength comes in many forms and that true power lies within oneself..

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stranger thigs

stranger thigs