2242: Ground vs Air - Revision history

Pressforaction: /* Explanation */ "Comprised of" is nonsense...

2023-06-17T08:12:45Z

‎Explanation: "Comprised of" is nonsense...

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2022-10-02T11:01:14Z

‎Explanation: move period into parentheses, it’s a complete sentence in there

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2022-05-26T17:30:09Z

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Davidy22: Reverted edits by Explain xkcd server admin (talk) to last revision by Jacky720

2022-05-21T02:56:20Z

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Explain xkcd server admin at 21:36, 20 May 2022

2022-05-20T21:36:34Z

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Jacky720: rv

2022-05-04T23:30:49Z

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Ex Kay Cee Dee at 23:30, 4 May 2022

2022-05-04T23:30:20Z

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@@ Line 11: / Line 11: @@
 This comic depicts a map of the world using the {{w|Winkel tripel projection}}, comparing the thickness of the ground, which is defined as the {{w|lithosphere}}, to the "thickness" (or height) of the air above it, which refers to the {{w|atmosphere}}.
-In an inserted figure, [[Randall]] defines the thickness using three boundaries. At the top is {{w|space}}, defined by the {{w|Kármán line}} at an altitude of 100 km (≈ 62 mi). (See the [[#Trivia|Trivia]] section below for a discussion of this definition of the beginning of space.) Below that is the atmosphere which goes down to the ground, where [[Cueball]] is standing, or the water. Beneath the surface is the lithosphere, comprised of the Earth's crust along with the rigid upper part of the mantle, and beneath this is the {{w|asthenosphere}}, the partially melted, highly viscous region of the {{w|upper mantle}} just below the lithosphere. The lithosphere is variable in thickness, averaging about 100 km, but the oceanic lithosphere is much thinner than the continental lithosphere (oceanic crust is thinner and denser than continental crust).  The diagram also shows oceanic cross-section to the left-hand side and, though the diagram does not make it explicit, presumably the two measurements used are of the atmosphere down from 'space' to the surface of the ground, if dry, or to the surface of the water covering the ground (which is essentially sea level in the oceans, fluctuating slightly with the tides, but covers a broader range for inland water, from the Dead Sea, at 0.4 km below sea level, to Lake Titicaca, almost 4 km above sea level) and of rock descending from the solid interface down to the asthenosphere, as the sliver of liquid that can intervene between the two spans is referred to as a separate measurement elsewhere.
+In an inserted figure, [[Randall]] defines the thickness using three boundaries. At the top is {{w|space}}, defined by the {{w|Kármán line}} at an altitude of 100 km (≈ 62 mi). (See the [[#Trivia|Trivia]] section below for a discussion of this definition of the beginning of space.) Below that is the atmosphere which goes down to the ground, where [[Cueball]] is standing, or the water. Beneath the surface is the lithosphere, comprising the Earth's crust along with the rigid upper part of the mantle, and beneath this is the {{w|asthenosphere}}, the partially melted, highly viscous region of the {{w|upper mantle}} just below the lithosphere. The lithosphere is variable in thickness, averaging about 100 km, but the oceanic lithosphere is much thinner than the continental lithosphere (oceanic crust is thinner and denser than continental crust).  The diagram also shows oceanic cross-section to the left-hand side and, though the diagram does not make it explicit, presumably the two measurements used are of the atmosphere down from 'space' to the surface of the ground, if dry, or to the surface of the water covering the ground (which is essentially sea level in the oceans, fluctuating slightly with the tides, but covers a broader range for inland water, from the Dead Sea, at 0.4 km below sea level, to Lake Titicaca, almost 4 km above sea level) and of rock descending from the solid interface down to the asthenosphere, as the sliver of liquid that can intervene between the two spans is referred to as a separate measurement elsewhere.
 The map shades in the parts where the thickness of the ground is thicker than the thickness of the air. This almost only occurs directly over continents, and certainly only where the continental crust is located (which can stretch into the near-coast parts of oceans). Oceanic crust is much thinner than continental crust. It is also made of a different material; it is denser. Because it is denser, it floats lower in the liquid asthenosphere, causing it to be below sea level. Some parts of continental crust are also under sea level (the continental shelf). These are the areas on the map that are marked as having thicker ground that appear to be over the ocean (such as Northern Canada, or the Caribbean) - they are actually still continental crust. (There are still some exceptions, such as the Sea of Japan and the Philippines).

@@ Line 11: / Line 11: @@
 This comic depicts a map of the world using the {{w|Winkel tripel projection}}, comparing the thickness of the ground, which is defined as the {{w|lithosphere}}, to the "thickness" (or height) of the air above it, which refers to the {{w|atmosphere}}.
-In an inserted figure, [[Randall]] defines the thickness using three boundaries. At the top is {{w|space}}, defined by the {{w|Kármán line}} at an altitude of 100 km (≈ 62 mi). (See the [[#Trivia|Trivia]] section below for a discussion of this definition of the beginning of space). Below that is the atmosphere which goes down to the ground, where [[Cueball]] is standing, or the water. Beneath the surface is the lithosphere, comprised of the Earth's crust along with the rigid upper part of the mantle, and beneath this is the {{w|asthenosphere}}, the partially melted, highly viscous region of the {{w|upper mantle}} just below the lithosphere. The lithosphere is variable in thickness, averaging about 100 km, but the oceanic lithosphere is much thinner than the continental lithosphere (oceanic crust is thinner and denser than continental crust).  The diagram also shows oceanic cross-section to the left-hand side and, though the diagram does not make it explicit, presumably the two measurements used are of the atmosphere down from 'space' to the surface of the ground, if dry, or to the surface of the water covering the ground (which is essentially sea level in the oceans, fluctuating slightly with the tides, but covers a broader range for inland water, from the Dead Sea, at 0.4 km below sea level, to Lake Titicaca, almost 4 km above sea level) and of rock descending from the solid interface down to the asthenosphere, as the sliver of liquid that can intervene between the two spans is referred to as a separate measurement elsewhere.
+In an inserted figure, [[Randall]] defines the thickness using three boundaries. At the top is {{w|space}}, defined by the {{w|Kármán line}} at an altitude of 100 km (≈ 62 mi). (See the [[#Trivia|Trivia]] section below for a discussion of this definition of the beginning of space.) Below that is the atmosphere which goes down to the ground, where [[Cueball]] is standing, or the water. Beneath the surface is the lithosphere, comprised of the Earth's crust along with the rigid upper part of the mantle, and beneath this is the {{w|asthenosphere}}, the partially melted, highly viscous region of the {{w|upper mantle}} just below the lithosphere. The lithosphere is variable in thickness, averaging about 100 km, but the oceanic lithosphere is much thinner than the continental lithosphere (oceanic crust is thinner and denser than continental crust).  The diagram also shows oceanic cross-section to the left-hand side and, though the diagram does not make it explicit, presumably the two measurements used are of the atmosphere down from 'space' to the surface of the ground, if dry, or to the surface of the water covering the ground (which is essentially sea level in the oceans, fluctuating slightly with the tides, but covers a broader range for inland water, from the Dead Sea, at 0.4 km below sea level, to Lake Titicaca, almost 4 km above sea level) and of rock descending from the solid interface down to the asthenosphere, as the sliver of liquid that can intervene between the two spans is referred to as a separate measurement elsewhere.
 The map shades in the parts where the thickness of the ground is thicker than the thickness of the air. This almost only occurs directly over continents, and certainly only where the continental crust is located (which can stretch into the near-coast parts of oceans). Oceanic crust is much thinner than continental crust. It is also made of a different material; it is denser. Because it is denser, it floats lower in the liquid asthenosphere, causing it to be below sea level. Some parts of continental crust are also under sea level (the continental shelf). These are the areas on the map that are marked as having thicker ground that appear to be over the ocean (such as Northern Canada, or the Caribbean) - they are actually still continental crust. (There are still some exceptions, such as the Sea of Japan and the Philippines).