Solar Eclipse june 2021 LIVE video @ViralVideoLab

ViralVideoLab | Solar Eclipse june 2021 LIVE video @ViralVideoLab | Uploaded 3 years ago | Updated 5 hours ago
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The "ring of fire" solar eclipse is coming up Thursday (June 10) and here's when you can watch the solar eclipse.

The solar eclipse will be visible will be partially visible from the United States, northern Canada, Europe, northern Asia, Russia and Greenland. You can also watch solar eclipse live online with several live solar eclipse webcasts, and if you live in any of the areas where the solar eclipse is visible and it's safe to travel, you can look at it outside — just make sure to wear protection.
Solar eclipses happen when moon passes in front of our sun, from the view of our planet. Total solar eclipses happen when our moon covers the entire sun. A "ring of fire" or annular eclipse happens when the moon is near its farthest point from Earth during an eclipse
The first locations where you can see the partial phase of solar eclipse — where the moon takes a "bite" out of the sun — will happen at 4:13 a.m. EDT (0813 GMT); local time will vary depending on where you are situated. You can see a partial eclipse if you are living north and east of a line running roughly from Edmonton, Alberta, to Des Moines, Iowa, down through Savannah, Georgia.
The annular solar eclipse will start being visible in those northerly regions fortunate enough to see it at 5:48 a.m. EDT (0948 GMT), according to Time and Date. The maximum eclipse will happen at 6:42 a.m. EDT (1042 GMT) in the north polar region, where the annular phase will last roughly 3 minutes and 51 seconds.
Annularity will be best visible in Canada, as the path begins on the north shoreline of Lake Superior and is highly visible in the Canadian Shield of northwest Ontario and the Canadian Arctic tundra. Unfortunately, those living in the United States won't be able to see the "ring of fire" in person because the border to Canada has been closed to non-essential travel due to the pandemic.

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$iPhone 14 Zoom is incredible! Subscribe: https://www.youtube.com/subscription_center?add_user=ViralVideoLab Infinite Mountain Zoom #shorts #short play in auto replay (use right click on the video and then repeat) In mathematics, a fractal is a subset of Euclidean space with a fractal dimension that strictly exceeds its topological dimension. Fractals appear the same at different scales, as illustrated in successive magnifications of the Mandelbrot set. Fractals often exhibit similar patterns at increasingly smaller scales, a property called self-similarity, also known as expanding symmetry or unfolding symmetry; if this replication is exactly the same at every scale, as in the Menger sponge, it is called affine self-similar. Fractal geometry lies within the mathematical branch of measure theory. One way that fractals are different from finite geometric figures is how they scale. Doubling the edge lengths of a polygon multiplies its area by four, which is two (the ratio of the new to the old side length) raised to the power of two (the dimension of the space the polygon resides in). Likewise, if the radius of a sphere is doubled, its volume scales by eight, which is two (the ratio of the new to the old radius) to the power of three (the dimension that the sphere resides in). However, if a fractals one-dimensional lengths are all doubled, the spatial content of the fractal scales by a power that is not necessarily an integer. This power is called the fractal dimension of the fractal, and it usually exceeds the fractals topological dimension.[6] Analytically, most fractals are nowhere differentiable. An infinite fractal curve can be conceived of as winding through space differently from an ordinary line – although it is still topologically 1-dimensional, its fractal dimension indicates that it also resembles a surface. Sierpinski carpet (to level 6), a fractal with a topological dimension of 1 and a Hausdorff dimension of 1.893 Starting in the 17th century with notions of recursion, fractals have moved through increasingly rigorous mathematical treatment to the study of continuous but not differentiable functions in the 19th century by the seminal work of Bernard Bolzano, Bernhard Riemann, and Karl Weierstrass,[8] and on to the coining of the word fractal in the 20th century with a subsequent burgeoning of interest in fractals and computer-based modelling in the 20th century.[9][10] The term fractal was first used by mathematician Benoit Mandelbrot in 1975. Mandelbrot based it on the Latin frāctus, meaning broken or fractured, and used it to extend the concept of theoretical fractional dimensions to geometric patterns in nature. There is some disagreement among mathematicians about how the concept of a fractal should be formally defined. Mandelbrot himself summarized it as beautiful, damn hard, increasingly useful. Thats fractals.[12] More formally, in 1982 Mandelbrot defined fractal as follows: A fractal is by definition a set for which the Hausdorff–Besicovitch dimension strictly exceeds the topological dimension. Later, seeing this as too restrictive, he simplified and expanded the definition to this: A fractal is a shape made of parts similar to the whole in some way.[14] Still later, Mandelbrot proposed to use fractal without a pedantic definition, to use fractal dimension as a generic term applicable to all the variants. The consensus among mathematicians is that theoretical fractals are infinitely self-similar, iterated, and detailed mathematical constructs having fractal dimensions, of which many examples have been formulated and studied. Fractals are not limited to geometric patterns, but can also describe processes in time. Fractal patterns with various degrees of self-similarity have been rendered or studied in visual, physical, and aural media[20] and found in nature, technology, art, architecture and law.Fractals are of particular relevance in the field of chaos theory because the graphs of most chaotic processes are fractals.[34] Many real and model networks have been found to have fractal features such as self similarity.$

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