Hârn Geology - Revision history

Shealladh: /* Kandáy */

2017-08-26T20:59:40Z

‎Kandáy

Shealladh: /* Kandáy */

2017-08-26T20:57:28Z

‎Kandáy

Shealladh: /* Kandáy */

2017-08-26T14:41:32Z

‎Kandáy

Shealladh: /* Kandáy */

2017-08-26T10:06:23Z

‎Kandáy

Shealladh at 10:00, 26 August 2017

2017-08-26T10:00:53Z

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Shealladh: /* Part Two: Geohistory */

2017-08-26T08:52:38Z

‎Part Two: Geohistory

Shealladh: /* Part Two: Geohistory */

2017-08-26T08:37:23Z

‎Part Two: Geohistory

Shealladh: /* Part One: Geological Units */

2017-08-26T08:32:31Z

‎Part One: Geological Units

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Shealladh: /* Part One: Geological Units */

2017-08-26T08:26:33Z

‎Part One: Geological Units

Shealladh: /* Part One: Geological Units */

2017-08-26T08:25:49Z

‎Part One: Geological Units

@@ Line 638: / Line 638: @@
 * '''Note:''' Colour Highlights: <span style="background:#FCFF19">Yellow</span>
-* Colour LINK Text: '''<span style="color:#006699">Possible Link</span>''' [[H%C3%A2rn_Kandáy_SHIRE_HUNDRED_NAME|NAME]]
+* Colour LINK Text: '''<span style="color:#006699">Possible Link</span>'''
-[[H%C3%A2rn_Kingdom_of_Kandáy|Kandáy]]'s mineral resources derive from two main sources. Southern [[H%C3%A2rn_Kingdom_of_Kandáy|Kandáy]] – from the '''<span style="color:#006699">Eryn River</span>''' to '''<span style="color:#006699">Cape Gemal</span>''' – is dotted with '''<span style="color:#006699">granite</span>''' masses, mostly still covered. These intrusions created '''<span style="color:#006699">tin</span>''', '''<span style="color:#006699">copper</span>''', and '''<span style="color:#006699">lead</span>''' '''<span style="color:#006699">ores</span>''' that are mined in '''<span style="color:#006699">Torenshire</span>''' and '''<span style="color:#006699">Erynashire</span>'''. They also metamorphosed overlying carbonaceous materials, creating the soapstone and marble quarried along the coast.
+'''[[H%C3%A2rn_Kingdom_of_Kandáy|Kandáy]]''''s '''<span style="color:#006699">mineral</span>''' '''<span style="color:#006699">resources</span>''' derive from two main sources. Southern '''[[H%C3%A2rn_Kingdom_of_Kandáy|Kandáy]]''' – from the '''<span style="color:#006699">Eryn River</span>''' to '''<span style="color:#006699">Cape Gemal</span>''' – is dotted with '''<span style="color:#006699">granite</span>''' masses, mostly still covered. These intrusions created '''<span style="color:#006699">tin</span>''', '''<span style="color:#006699">copper</span>''', and '''<span style="color:#006699">lead</span>''' '''<span style="color:#006699">ores</span>''' that are mined in '''<span style="color:#006699">Torenshire</span>''' and '''<span style="color:#006699">Erynashire</span>'''. They also metamorphosed overlying carbonaceous materials, creating the soapstone and marble quarried along the coast.
-The other resource that [[H%C3%A2rn_Kingdom_of_Kandáy|Kandáy]] has in relative abundance is '''<span style="color:#006699">bog iron</span>'''. [[H%C3%A2rn_Kingdom_of_Kandáy|Kandáy]]'s largest source is the ancient '''<span style="color:#006699">bog iron</span>''' easily dug up near '''<span style="color:#006699">Chison</span>'''. Near '''<span style="color:#006699">Hebon</span>''' and '''<span style="color:#006699">Selvos</span>''' are similar deposits created by now-dried up bogs. These '''<span style="color:#006699">lodes</span>''' merely scratch the surface of [[H%C3%A2rn_Kingdom_of_Kandáy|Kandáy]]'s '''<span style="color:#006699">bog iron</span>''' potential. The same process that created them is constantly working to create more '''<span style="color:#006699">iron</span>''' '''<span style="color:#006699">ore</span>''' in the many bogs of western [[H%C3%A2rn_Kingdom_of_Kandáy|Kandáy]].
+The other resource that '''[[H%C3%A2rn_Kingdom_of_Kandáy|Kandáy]]''' has in relative abundance is '''<span style="color:#006699">bog iron</span>'''. '''[[H%C3%A2rn_Kingdom_of_Kandáy|Kandáy]]''''s largest source is the ancient '''<span style="color:#006699">bog iron</span>''' easily dug up near '''<span style="color:#006699">Chison</span>'''. Near '''<span style="color:#006699">Hebon</span>''' and '''<span style="color:#006699">Selvos</span>''' are similar deposits created by now-dried up bogs. These '''<span style="color:#006699">lodes</span>''' merely scratch the surface of '''[[H%C3%A2rn_Kingdom_of_Kandáy|Kandáy]]''''s '''<span style="color:#006699">bog iron</span>''' potential. The same process that created them is constantly working to create more '''<span style="color:#006699">iron</span>''' '''<span style="color:#006699">ore</span>''' in the many bogs of western '''[[H%C3%A2rn_Kingdom_of_Kandáy|Kandáy]]'''.
 === [[H%C3%A2rn_Kingdom_of_Réthem|Réthem]] ===

← Older revision		Revision as of 20:57, 26 August 2017
Line 643:		Line 643:


−	The other resource that [[H%C3%A2rn_Kingdom_of_Kandáy\|Kandáy]] has in relative abundance is bog iron. [[H%C3%A2rn_Kingdom_of_Kandáy\|Kandáy]]'s largest source is the ancient bog iron easily dug up near Chison. Near Hebon and Selvos are similar deposits created by now-dried up bogs. These lodes merely scratch the surface of [[H%C3%A2rn_Kingdom_of_Kandáy\|Kandáy]]'s bog iron potential. The same process that created them is constantly working to create more iron ore in the many bogs of western [[H%C3%A2rn_Kingdom_of_Kandáy\|Kandáy]].	+	The other resource that [[H%C3%A2rn_Kingdom_of_Kandáy\|Kandáy]] has in relative abundance is '''<span style="color:#006699">bog iron</span>'''. [[H%C3%A2rn_Kingdom_of_Kandáy\|Kandáy]]'s largest source is the ancient '''<span style="color:#006699">bog iron</span>''' easily dug up near '''<span style="color:#006699">Chison</span>'''. Near '''<span style="color:#006699">Hebon</span>''' and '''<span style="color:#006699">Selvos</span>''' are similar deposits created by now-dried up bogs. These '''<span style="color:#006699">lodes</span>''' merely scratch the surface of [[H%C3%A2rn_Kingdom_of_Kandáy\|Kandáy]]'s '''<span style="color:#006699">bog iron</span>''' potential. The same process that created them is constantly working to create more '''<span style="color:#006699">iron</span>''' '''<span style="color:#006699">ore</span>''' in the many bogs of western [[H%C3%A2rn_Kingdom_of_Kandáy\|Kandáy]].

	=== [[H%C3%A2rn_Kingdom_of_Réthem\|Réthem]] ===		=== [[H%C3%A2rn_Kingdom_of_Réthem\|Réthem]] ===

@@ Line 635: / Line 635: @@
 === [[H%C3%A2rn_Kingdom_of_Kandáy|Kandáy]] ===
-'''Note:''' '''<span style="color:#FF0000">ADD</span>'''link to [[Hârn_Mines_of_Hârn#Kandáy| Hârn MINES]] Kandáy.
+'''Note:''' '''<span style="color:#FF0000">ADD</span>'''link to '''[[Hârn_Mines_of_Hârn#Kandáy| Hârn MINES]]''' Kandáy.
 * '''Note:''' Colour Highlights: <span style="background:#FCFF19">Yellow</span>

@@ Line 635: / Line 635: @@
 === [[H%C3%A2rn_Kingdom_of_Kandáy|Kandáy]] ===
-'''Note:''' '''<span style="color:#FF0000">ADD</span>'''link to [[H%C3%A2rn_Kandáy_SHIRE_HUNDRED_NAME| Hârn MINES]]
+'''Note:''' '''<span style="color:#FF0000">ADD</span>'''link to [[Hârn_Mines_of_Hârn#Kandáy| Hârn MINES]] Kandáy.
 * '''Note:''' Colour Highlights: <span style="background:#FCFF19">Yellow</span>
 * Colour LINK Text: '''<span style="color:#006699">Possible Link</span>''' [[H%C3%A2rn_Kandáy_SHIRE_HUNDRED_NAME|NAME]]
-[[H%C3%A2rn_Kingdom_of_Kandáy|Kandáy]]'s mineral resources derive from two main sources. Southern [[H%C3%A2rn_Kingdom_of_Kandáy|Kandáy]] – from the '''<span style="color:#006699">Eryn River to</span>''' '''<span style="color:#006699">Cape Gemal</span>''' – is dotted with '''<span style="color:#006699">granite</span>''' masses, mostly still covered. These intrusions created '''<span style="color:#006699">tin</span>''', '''<span style="color:#006699">copper</span>''', and '''<span style="color:#006699">lead</span>''' '''<span style="color:#006699">ores</span>''' that are mined in '''<span style="color:#006699">Torenshire</span>''' and '''<span style="color:#006699">Erynashire</span>'''. They also metamorphosed overlying carbonaceous materials, creating the soapstone and marble quarried along the coast.
+[[H%C3%A2rn_Kingdom_of_Kandáy|Kandáy]]'s mineral resources derive from two main sources. Southern [[H%C3%A2rn_Kingdom_of_Kandáy|Kandáy]] – from the '''<span style="color:#006699">Eryn River</span>''' to '''<span style="color:#006699">Cape Gemal</span>''' – is dotted with '''<span style="color:#006699">granite</span>''' masses, mostly still covered. These intrusions created '''<span style="color:#006699">tin</span>''', '''<span style="color:#006699">copper</span>''', and '''<span style="color:#006699">lead</span>''' '''<span style="color:#006699">ores</span>''' that are mined in '''<span style="color:#006699">Torenshire</span>''' and '''<span style="color:#006699">Erynashire</span>'''. They also metamorphosed overlying carbonaceous materials, creating the soapstone and marble quarried along the coast.
 The other resource that [[H%C3%A2rn_Kingdom_of_Kandáy|Kandáy]] has in relative abundance is bog iron. [[H%C3%A2rn_Kingdom_of_Kandáy|Kandáy]]'s largest source is the ancient bog iron easily dug up near Chison. Near Hebon and Selvos are similar deposits created by now-dried up bogs. These lodes merely scratch the surface of [[H%C3%A2rn_Kingdom_of_Kandáy|Kandáy]]'s bog iron potential. The same process that created them is constantly working to create more iron ore in the many bogs of western [[H%C3%A2rn_Kingdom_of_Kandáy|Kandáy]].
 === [[H%C3%A2rn_Kingdom_of_Réthem|Réthem]] ===

@@ Line 393: / Line 393: @@
 <center>
 {|
-|+ style="caption-side:bottom; color:#000000;"|'''Coat of Arms'''
+|+ style="caption-side:bottom; color:#000000;"|'''Geohistory Early Period'''
-| [[File:Hârn_Geology_Early_Uplift_&_Salt_Formations.png|900px|center|link= ]]
+| [[File:Hârn_Geology_Geohistory_Early_Period.png|900px|center|link= ]]
 |}
 </center>
@@ Line 469: / Line 469: @@
 <center>
 {|
-|+ style="caption-side:bottom; color:#000000;"|'''Coat of Arms'''
+|+ style="caption-side:bottom; color:#000000;"|'''Geohistory Second Period'''
-| [[File:Kandáy_Player_Map.png|900px|center|link= ]]
+| [[File:Hârn_Geology_Geohistory_Second_Period.png|900px|center|link= ]]
 |}
 </center>
@@ Line 513: / Line 513: @@
 <center>
 {|
-|+ style="caption-side:bottom; color:#000000;"|'''Coat of Arms'''
+|+ style="caption-side:bottom; color:#000000;"|'''Geohistory Third Period'''
-| [[File:Kandáy_Player_Map.png|900px|center|link= ]]
+| [[File:Hârn_Geology_Geohistory_Third_Period.png|900px|center|link= ]]
 |}
 </center>
@@ Line 532: / Line 532: @@
 <center>
 {|
-|+ style="caption-side:bottom; color:#000000;"|'''Coat of Arms'''
+|+ style="caption-side:bottom; color:#000000;"|'''Denia Hotspot'''
-| [[File:Kandáy_Player_Map.png|900px|center|link= ]]
+| [[File:Hârn_Geology_Geohistory_Denia_Hotspot.png|center|link= ]]
 |}
 </center>
@@ Line 567: / Line 567: @@
 <center>
 {|
-|+ style="caption-side:bottom; color:#000000;"|'''Coat of Arms'''
+|+ style="caption-side:bottom; color:#000000;"|'''Third Period Glaciation'''
-| [[File:Kandáy_Player_Map.png|900px|center|link= ]]
+| [[File:Hârn_Geology_Geohistory_Third_Period_Glaciation.png|900px|center|link= ]]
 |}
 </center>
@@ Line 586: / Line 586: @@
 <center>
 {|
-|+ style="caption-side:bottom; color:#000000;"|'''Coat of Arms'''
+|+ style="caption-side:bottom; color:#000000;"|'''Peran Impact Event'''
-| [[File:Kandáy_Player_Map.png|900px|center|link= ]]
+| [[File:Hârn_Geology_Geohistory_Peran_Impact_Event.png|center|link= ]]
 |}
 </center>

@@ Line 83: / Line 83: @@
 As with any land mass, Hârn can be divided into a number of geological units. Each unit arose from a different sequence of processes, often from different base materials, and are marked by distinctive minerals and geological formations. The classification detailed here is a relatively coarse analysis. More detailed study might allow finer distinctions, and in turn, allow more units to be identified. Thus the contents of each unit should not be considered completely homogeneous, nor should the borders between them be interpreted as hard and absolute.
 {| "wikitable" style="width: 25px; height: 25px; float:left;"
 |style="background:#4700FB;" align="center"|
 |}
 The largest portion of Hârn consists mostly of sedimentary rocks formed from material eroded from the several mountain zones. While a great amount of variation occurs, in general the sedimentary rock tends to be more finely grained and contain more calcite the farther from the central sources. Areas closer to the center of Hârn have sandier, more quartz-rich stone. Gravel is prevalent in the flood plains of ancient rivers, so gritstones and conglomerates mark the path of the ancient Thârd, Kald, and northwestern rivers.

@@ Line 85: / Line 85: @@
 === Alluvial Sedimentary Units ===
 The largest portion of Hârn consists mostly of sedimentary rocks formed from material eroded from the several mountain zones. While a great amount of variation occurs, in general the sedimentary rock tends to be more finely grained and contain more calcite the farther from the central sources. Areas closer to the center of Hârn have sandier, more quartz-rich stone. Gravel is prevalent in the flood plains of ancient rivers, so gritstones and conglomerates mark the path of the ancient Thârd, Kald, and northwestern rivers.
@@ Line 98: / Line 101: @@
 </center>
 {| "wikitable" style="width: 25px; height: 25px; float:left;"
@@ Line 171: / Line 173: @@
 |style="background:#C72124;" align="center"|
 |}
 === Complex Central Highlands ===