AY Honors/Geology/Answer Key - Revision history

W126jep at 01:40, 4 January 2023

2023-01-04T01:40:50Z

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2022-07-13T20:57:59Z

+ GetLangSuffix Template

W126jep at 12:59, 28 May 2021

2021-05-28T12:59:18Z

W126jep at 15:46, 13 April 2021

2021-04-13T15:46:37Z

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2021-01-24T10:42:58Z

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2021-01-23T17:10:55Z

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Jomegat bot: Jomegat bot moved page Adventist Youth Honors Answer Book/Nature/Geology to AY Honors/Geology/Answer Key: Bot: Moved page

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Jomegat bot moved page AY Honor Geology to AY Honor Geology Answer Key: Bot: Moved page

Jomegat at 04:50, 6 November 2020

2020-11-06T04:50:44Z

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 <!--{{Honor_Master|honor=Geology|master=Conservation}}-->
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 *[[w:Syncline|Syncline]]
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 *[[w:Stratovolcano|Stratovolcano]]
 *[[w:Syncline|Syncline]]
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 <!--T:33-->
-:C) Substratum: Layer of unconsolidated soil parent material. This layer may accumulate the more soluble compounds that bypass the "B" layer.  </div>
+:C) Substratum: Layer of unconsolidated soil parent material. This layer may accumulate the more soluble compounds that bypass the "B" layer. </div>
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 <gallery>
 Image:Nile River and delta from orbit.jpg|Satellite image of the Nile '''River Delta'''
-Image:Baltic spits.png|The three narrow strips of land shown here are '''spits''' in the Baltic  Sea
+Image:Baltic spits.png|The three narrow strips of land shown here are '''spits''' in the Baltic Sea
 Image:DeadSeaSinkhole.jpg|'''Sinkholes''' near the Dead Sea
 Image:Oxbow lake.jpg|Map of an '''oxbow''' lake
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 [[Image:Skjaldbreidur Herbst 2004.jpg|thumb|300px|"Skjaldbreiður", an Icelandic shield volcano whose name means "broad shield."]]
-A '''shield volcano''' is a large volcano with shallowly-sloping sides.  Shield volcanoes are formed by lava flows of low viscosity — lava that flows easily. Consequently, a volcanic mountain having a broad profile is built up over time by flow after flow of relatively fluid lava issuing from vents or fissures on the surface of the volcano. Many of the largest volcanoes on Earth are shield volcanoes. The largest is Mauna Loa on the Big Island of Hawaii.
+A '''shield volcano''' is a large volcano with shallowly-sloping sides. Shield volcanoes are formed by lava flows of low viscosity — lava that flows easily. Consequently, a volcanic mountain having a broad profile is built up over time by flow after flow of relatively fluid lava issuing from vents or fissures on the surface of the volcano. Many of the largest volcanoes on Earth are shield volcanoes. The largest is Mauna Loa on the Big Island of Hawaii.
 <br style="clear:both">
 <!--T:10-->
-[[Image:Sthelens1.jpg|thumb|300px|Mount St. Helens on May 17, 1980, one day before the devastating eruption.  It is a composite volcano.]]
+[[Image:Sthelens1.jpg|thumb|300px|Mount St. Helens on May 17, 1980, one day before the devastating eruption. It is a composite volcano.]]
 A '''composite volcano''' is a tall, conical volcano composed of many layers of hardened lava, tephra, and volcanic ash. These volcanoes are characterized by a steep profile and periodic, explosive eruptions. The lava that flows from them is viscous, and cools and hardens before spreading very far. Mount St. Helens in Washington, USA, Popocatépetl in Mexico, and Krakatoa in Indonesia are composite volcanos.
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-When water flows over a stream bed, it picks up sediments.  The faster the water flows, the larger particles it can transport.  As the water slows, the particles are dropped, forming a sediment.  Because the water speed slows gradually, the particles are sorted by size as they are dropped.
+When water flows over a stream bed, it picks up sediments. The faster the water flows, the larger particles it can transport. As the water slows, the particles are dropped, forming a sediment. Because the water speed slows gradually, the particles are sorted by size as they are dropped.
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 ====Block or Faultblock Mountains====
 [[Image:Horst graben.jpg|thumb|Horsts and Graben]]
-Block mountains are created when large areas are widely broken up by faults creating large vertical displacements. This occurrence is fairly common.  The uplifted blocks are block mountains or horsts. The intervening dropped blocks are termed graben: these can be small or form extensive rift valley systems. This form of landscape can be seen in East Africa, the Vosges, the Basin and Range province of Western North America and the Rhine valley.<br style="clear:both">
+Block mountains are created when large areas are widely broken up by faults creating large vertical displacements. This occurrence is fairly common. The uplifted blocks are block mountains or horsts. The intervening dropped blocks are termed graben: these can be small or form extensive rift valley systems. This form of landscape can be seen in East Africa, the Vosges, the Basin and Range province of Western North America and the Rhine valley.<br style="clear:both">
 ====Dome Mountains====
 [[Image:Enchanted rock 2006.jpg|thumb|Enchanted Rock, a dome mountain just west of the Hill Country of central Texas in the United States.]]
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-When a river reaches a low-lying plain in its final course to the sea or a lake, it meanders widely. Sediments are deposited on the inside (convex) bank because the current there slows. In contrast, both lateral erosion and undercutting occur on the outside (concave) bank where the stream’s speed is the highest.  The faster current on the outside of a bend is able to pick up sediments and transport them further downstream.
+When a river reaches a low-lying plain in its final course to the sea or a lake, it meanders widely. Sediments are deposited on the inside (convex) bank because the current there slows. In contrast, both lateral erosion and undercutting occur on the outside (concave) bank where the stream’s speed is the highest. The faster current on the outside of a bend is able to pick up sediments and transport them further downstream.
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 [[Image:Graded bed.png|thumb|250px|Normal graded bedding]]
-The size of a particle that a stream can transport depends on the stream's speed as well as the size and density of the particle.  In general, the faster the current, the larger the particle that can be transported.  As a stream slows, it drops the largest particles first.  As it slows more, it continues to drop finer and finer particles.  When the current stops, all sediments are deposited.  In the diagram note how the sediment at the top is much finer than the sediment at the bottom.  This natural sorting mechanism occurs whenever sediments are deposited, and can be used to detect boundaries between sedimentation events.  A normal graded sediment indicates that the sediment layer has not been overturned since it was deposited, while an inverted bed (finer particles at the bottom, larger ones on top) indicates that the sedimentation layer was overturned after its deposition.
+The size of a particle that a stream can transport depends on the stream's speed as well as the size and density of the particle. In general, the faster the current, the larger the particle that can be transported. As a stream slows, it drops the largest particles first. As it slows more, it continues to drop finer and finer particles. When the current stops, all sediments are deposited. In the diagram note how the sediment at the top is much finer than the sediment at the bottom. This natural sorting mechanism occurs whenever sediments are deposited, and can be used to detect boundaries between sedimentation events. A normal graded sediment indicates that the sediment layer has not been overturned since it was deposited, while an inverted bed (finer particles at the bottom, larger ones on top) indicates that the sedimentation layer was overturned after its deposition.
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 [[Image:Sand Norderney.jpg|thumb|300px|Ripple marks in sand]]
-In this photo, the wind was blowing from left to right.  The left sides of the ripples have gentler slopes, while the right sides have steeper slopes.  As the wind breaks over the top of the ripples, it forms eddy currents (circulating wind) which make the lee side steeper than the windward side.
+In this photo, the wind was blowing from left to right. The left sides of the ripples have gentler slopes, while the right sides have steeper slopes. As the wind breaks over the top of the ripples, it forms eddy currents (circulating wind) which make the lee side steeper than the windward side.
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-<div style="float:center; width:550px; border:1px; border-style:solid; padding:2px; text-align:left">    [[Image:Soil profile.png]]
+<div style="float:center; width:550px; border:1px; border-style:solid; padding:2px; text-align:left"> [[Image:Soil profile.png]]
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-:A) Surface soil: Layer of mineral soil with most organic matter accumulation and soil life.  This layer eluviates (is depleted of) iron, clay, aluminum, organic compounds, and other soluble constituents. When eluviation is pronounced, a lighter colored "E" subsurface soil horizon is apparent at the base of the "A" horizon.
+:A) Surface soil: Layer of mineral soil with most organic matter accumulation and soil life. This layer eluviates (is depleted of) iron, clay, aluminum, organic compounds, and other soluble constituents. When eluviation is pronounced, a lighter colored "E" subsurface soil horizon is apparent at the base of the "A" horizon.
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-:C) Substratum: Layer of unconsolidated soil parent material. This layer may accumulate the more soluble compounds that bypass the "B" layer.   </div>
+:C) Substratum: Layer of unconsolidated soil parent material. This layer may accumulate the more soluble compounds that bypass the "B" layer.  </div>
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 ;Igneous: Igneous rock is formed when lava cools and solidifies.
-<!--T:22-->
+===a. Granite ===
-{| border="1" cellspacing="2" cellpadding="5"
+Igneous
-!| Rock
-!| Category
+===b. Sandstone===
-|-
+Sedimentary
-| a. Granite
-| Igneous
+===c. Conglomerate===
-|-
+Sedimentary
-| b. Sandstone
-| Sedimentary
+===d. Slate===
-|-
+Metamorphic
-| c. Conglomerate
-| Sedimentary
+===e. Shale===
-|-
+Sedimentary
-| d. Slate
-| Metamorphic
+===f. Marble===
-|-
+Metamorphic
-| e. Shale
-| Sedimentary
+===g. Lava===
-|-
+Igneous
-| f. Marble
-| Metamorphic
+===h. Limestone===
-|-
+Sedimentary
-| g. Lava
-| Igneous
+===i. Basalt===
-|-
+Igneous
-| h. Limestone
-| Sedimentary
+===j. Gneiss===
-|-
+Metamorphic
 ==4. Take a picture or make a sketch of each of the following geological features:== <!--T:23-->

AY Honors/Geology/Answer Key - Revision history

W126jep at 01:40, 4 January 2023

W126jep: + GetLangSuffix Template

W126jep at 12:59, 28 May 2021

W126jep at 15:46, 13 April 2021

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Jomegat bot: Jomegat bot moved page Adventist Youth Honors Answer Book/Nature/Geology to AY Honors/Geology/Answer Key: Bot: Moved page

Jomegat at 04:50, 6 November 2020

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