39:
between the peaks of An Eag and Sgurr Cos na
Breachd-laoidh. The river is fed by numerous burns both to north and south, key amongst which are Allt a' Chinn Bhric, Allt a' Choire Ghlais, Allt Coir' an Stangain Mhoir, Allt a' ùRiabhaich and Allt Torrain Dharaich. The waters of the Kingie enter those
99:
There are no public roads within the glen though a private vehicle track extends through the plantation from Glen Garry. An old right of way continues westwards from near the head of this track. Much of the lower part of the glen is planted up as a commercial forestry plantation, contiguous with
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at Kingie Pool. Much of the northern side of the glen is formed by the slopes of 1003m high mountain of
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at its north-eastern end at Kingie. It is drained by the River Kingie which rises at a 650m
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8:
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56:. The more broken southern side is dominated, at least in its upper reaches, by three (
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132:"Geology of Britain viewer | British Geological Survey (BGS)"
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72:. The glen runs through territory formed by
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96:in the middle section of the glen.
13:
201:Valleys of Highland (council area)
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1:
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94:West Highland Granite Gneiss
7:
100:plantations in Glen Garry.
62:Sgurr Cos na Breachd-laoidh
10:
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92:which is intruded by the
84:Glenfinnan Group of the
88:, a thick sequence of
86:Loch Ness Supergroup
52:, both of which are
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90:metamorphosed rocks
25:Northwest Highlands
138:on 2 December 2016
48:and the 919m high
196:Glens of Scotland
31:which opens onto
23:or valley in the
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172:57.031°N 5.240°W
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134:. Archived from
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70:Sgurr Mhurlagain
60:; the 835m high
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177:57.031; -5.240
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68:and the 880m
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66:Fraoch Bheinn
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140:. Retrieved
136:the original
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80:of the late
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15:
175: /
82:Precambrian
64:, the 858m
42:River Garry
17:Glen Kingie
190:Categories
160:57°01′52″N
104:References
33:Glen Garry
163:5°14′24″W
142:9 October
74:psammites
46:Sgurr Mor
58:Corbetts
29:Scotland
78:pelites
50:Gairich
40:of the
118:"Maps"
54:Munros
19:is a
144:2019
76:and
21:glen
37:col
27:of
192::
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120:.
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