Antigone's two main faults are her stubbornness and her defiance of authority. Her unwavering commitment to burying her brother Polynices, despite King Creon's edict, illustrates her inability to compromise and adhere to societal laws. This rebellion against Creon's authority ultimately leads to tragic consequences, showcasing the conflicts between individual morality and state laws. Additionally, her pride in her convictions prevents her from recognizing the potential for dialogue and reconciliation.
antigones father
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did you teacher give you that worksheet too.
no husband, only fiancee. she killed herself before she got married. his name was Haemon, Creon's son.
In wanting to bury Polyneices? She wants to have a clean conscience for the afterlife. If she does the right this and buries her brother, she will have a good afterlife.
antigones father
Foreshadowing
Faults are created when tectonic plates are stretching or compressing. There are two types of faults which are normal and reverse faults.
The two types of faults that can result in mountains are thrust faults and normal faults. Thrust faults occur when one tectonic plate is forced up over another, while normal faults occur when the Earth's crust is being pulled apart, causing one block to drop down relative to the other.
bearing faults and circuit connection faults
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A trench between two parallel faults in the earth's crust is called a graben. Grabens are formed by the downward movement of blocks of land between normal faults.
by two normal faults
The two types of faults that can result in mountains are thrust faults and normal faults. Thrust faults occur when older rock is pushed on top of younger rock, causing uplift and mountain formation. Normal faults occur when tensional forces cause one block of rock to drop down relative to another block, creating valleys and mountain ranges.
At convergent boundaries, two tectonic plates move toward each other, leading primarily to two types of faults: thrust faults and reverse faults. Thrust faults occur when one plate is pushed over another, typically resulting in a shortening of the crust. Reverse faults also involve the movement of one block over another but are characterized by a steeper angle. Both types of faults are commonly associated with mountain building and seismic activity.
Three common types of faults are normal faults, reverse (or thrust) faults, and strike-slip faults. Normal faults occur when two blocks of crust move apart, causing one block to drop down relative to the other. Reverse faults happen when compression forces push two blocks together, causing one block to thrust over the other. Strike-slip faults involve horizontal movement of blocks sliding past one another, typically occurring along transform plate boundaries.
No, a fault-block is not typically created by two reverse faults. Reverse faults involve the upward movement of rock layers, and when two reverse faults occur in close proximity, they can create a complex structure but do not directly form a fault-block. Fault-blocks are more commonly associated with normal faults, where blocks of the Earth's crust are pulled apart, resulting in sections that drop down relative to others. In summary, while reverse faults can influence the landscape, they do not create fault-blocks in the same manner as normal faults do.