Wlop 1-5 Fundamentals - ographygeras’s diary

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Fundamentals - Part 1 of 5. Business planning expert Tim Berry talks about the fundamentals of a business plan, the different forms and uses for a plan, and introduces the idea of the plan as a living document.

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Previous work: (check them out on ). The full size comic GhostBlade. All the 4k&8k images which I created in the current month. The brush set I used in each work.

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40% off on purchasing any product in my Gumroad Store.(You will receive an offer code as reward). 1080p, normal speed process video of all the creations in current month. of the current month (the episode in current month if any. You can also buy the previous tutorials in my with the 40% off offer code). You can get the previous rewards in this tier!.

The full size comic GhostBlade. All the 4k&8k images which I created in the current month. The brush set I used in each work. (used in Photoshop).

Original PSD files of all the images in current month. 40% off on purchasing any product in my Gumroad Store.(You will receive an offer code as reward).

1080p, normal speed process video of all the creations in current month. of the current month. Every month, you can get one of my previous artwork for free(include PSD file, brush set and full video process), just choose your favorite one every month and I'll send it to you! Previous work: (check them out on ).

Earth's Internal StructureKey to understanding plate tectonics is an understanding of Earth’s internal structure, which is illustrated in Figure 1.5.1. Earth’s core consists mostly of iron. The outer core is hot enough for the iron to be liquid.

The inner core, although even hotter, is under so much pressure that it is solid. The mantle is made up of iron and magnesium silicate minerals. The bulk of the mantle, surrounding the outer core, is solid rock, but is plastic enough to be able to flow slowly. Surrounding that part of the mantle is a partially molten layer (the asthenosphere), and the outermost part of the mantle is rigid. The crust — composed mostly of granite on the continents and mostly of basalt beneath the oceans — is also rigid.

The crust and outermost rigid mantle together make up the lithosphere. The lithosphere is divided into about 20 tectonic plates that move in different directions on Earth’s surface.An important property of Earth (and other planets) is that the temperature increases with depth, from close to 0°C at the surface to about 7000°C at the centre of the core. In the crust, the rate of temperature increase is about 30°C/km. This is known as the geothermal gradient.Figure 1.5.1 The structure of Earth’s interior showing the inner and outer core, the different layers of the mantle, and the crust WikipediaHeat is continuously flowing outward from Earth’s interior, and the transfer of heat from the core to the mantle causes convection in the mantle (Figure 1.5.2). This convection is the primary driving force for the movement of tectonic plates.

At places where convection currents in the mantle are moving upward, new lithosphere forms (at ocean ridges), and the plates move apart (diverge). Where two plates are converging (and the convective flow is downward), one plate will be subducted (pushed down) into the mantle beneath the other. Many of Earth’s major earthquakes and volcanoes are associated with convergent boundaries.Figure 1.5.2 A model of convection within Earth’s mantle Earth’s major tectonic plates and the directions and rates at which they are diverging at sea-floor ridges, are shown in Figure 1.5.3. The LibreTexts libraries are and are supported by the Department of Education Open Textbook Pilot Project, the UC Davis Office of the Provost, the UC Davis Library, the California State University Affordable Learning Solutions Program, and Merlot. We also acknowledge previous National Science Foundation support under grant numbers 1246120, 1525057, and 1413739. Unless otherwise noted, LibreTexts content is licensed. Have questions or comments?

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