Editing 1778: Interest Timescales
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Entire trees like the one shown typically last several decades or even centuries before they die - if not felled by humans, most are eventually toppled by the wind as well. The breeze needed for that can be measured on the {{w|Beaufort scale}}, likely above 5. | Entire trees like the one shown typically last several decades or even centuries before they die - if not felled by humans, most are eventually toppled by the wind as well. The breeze needed for that can be measured on the {{w|Beaufort scale}}, likely above 5. | ||
− | Finally, in the case of a mountain, a | + | Finally, in the case of a mountain, a mountains rise fast from the ground due to movement of {{w|tectonic plates}} which result in mountains either via volcanic activity or by simply pressing the ground up through the process of subduction (see [[1388: Subduction License]]). The mountains are then very slowly broken down by natural erosion forces, and the stone particles disperse on the wind. These events are much slower than the others, typically taking tens of millions of years to completely erode away a mountain. |
Additionally, some humor stems from the fact that Cueball acts like the mountain is a {{w|roller coaster}}, even though a mountain may take thousands or millions of years to noticeably change. | Additionally, some humor stems from the fact that Cueball acts like the mountain is a {{w|roller coaster}}, even though a mountain may take thousands or millions of years to noticeably change. |