What happens when jagged edges of rock plates grind past each other
So the answer would be Earthquake! 🌎
Explain the meaning of the metaphor italicized below.
Her hair was a glistening raven’s wing that flowed in dark tresses down her back.
The metaphor here is comparing the woman's hair to a raven's wing. This implies that her hair is black and shiny, just like the feathers of a raven.
Write one to two sentences explaining how an author can reveal character development to the reader.
An author can reveal character development to the reader by showing how they react and respond to different situations and challenges throughout the story. Changes in the character's thoughts, feelings, and actions can also indicate growth and development.
Write three to four sentences explaining the differences between listening to a story, watching a story, and reading a story.
Listening to a story allows a person to use their imagination to create images in their mind. Watching a story provides visuals that gives the viewer no need to imagine character appearances or facial expression. Reading a story allows for the use of imagination and allows the reader to appreciate the author's writing style and choice of words.
Write one to two sentences explaining what should be included in a narrative introduction.
A narrative introduction should set the story's scene, establish the tone and mood, provide background information, and introduce the characters in a way that captivates the reader's attention. This will help to engage readers and create a connection with the story and characters.
When jagged edges of rock plates grind past each other, it results in a geological phenomenon known as faulting. Faulting occurs along the boundaries of tectonic plates, which are large pieces of Earth's crust that float on the semi-fluid asthenosphere below. These plates are always in motion, albeit very slowly, due to the convective currents in the underlying mantle.
Now, to understand what happens during faulting, let's break it down into steps:
1. Tectonic Plates: As mentioned earlier, the Earth's crust is divided into several large and small tectonic plates. These plates constantly move due to the pressure and heat within the Earth's mantle.
2. Plate Boundaries: The edges of these plates are where most of the action happens. There are three main types of plate boundaries: divergent boundaries (moving apart), convergent boundaries (colliding), and transform boundaries (sliding past each other). When it comes to jagged rocks grinding past each other, it refers to transform boundaries.
3. Transform Boundaries: At transform boundaries, two plates slide horizontally past each other. These boundaries are marked by transform faults. When the movement occurs, the jagged sections of the plates get stuck due to friction.
4. Build-up of Stress: As the plates continue to move, the locked sections experience stress and strain, causing the rocks to deform and store elastic energy over time.
5. Release of Energy: Eventually, the stress becomes too much to handle, and the stored elastic energy is released in the form of seismic waves, leading to an earthquake. The sudden release of energy allows the jagged edges of the rock plates to overcome the friction and slide past each other, momentarily reducing the stress along the fault line.
6. Earthquake and Aftershocks: The sliding of rock plates during an earthquake produces vibrations that propagate as seismic waves, causing the ground to shake. These vibrations can travel long distances from the initial epicenter. Aftershocks, which are smaller tremors following the main earthquake, often occur as the surrounding rocks adjust to the newly released stress.
So, when jagged edges of rock plates grind past each other, it usually results in the occurrence of an earthquake, which is the release of built-up energy along a fault line.