Volume contents
- 1 - Various parishes , Page 1 (start)
- 10 - Various parishes , Page 10
- 20 - Various parishes , Page 20
- 30 - Various parishes , Page 30
- 40 - Various parishes , Page 40
- 50 - Various parishes , Page 50
- 60 - Various parishes , Page 60
- 70 - Various parishes , Page 70
- 80 - Various parishes , Page 80
- 90 - Various parishes , Page 90
- 100 - Various parishes , Page 100
- 110 - Various parishes , Page 110
- 120 - Various parishes , Page 120
- 130 - Various parishes , Page 130
- 140 - Various parishes , Page 140
- 150 - Various parishes , Page 150
- 160 - Various parishes , Page 160
- 170 - Various parishes , Page 170
- 180 - Various parishes , Page 180
- 190 - Various parishes , Page 190
- 200 - Various parishes , Page 200
- 210 - Various parishes , Page 210
- 212 - Various parishes , Page 212 (end)
- 213 - Various parishes , Title page
- 214 - Various parishes , Index
| List of names as written | Various modes of spelling | Authorities for spelling | Situation | Description remarks |
|---|---|---|---|---|
| GLEN ROY | [continued from page 160] Ancient Glen Roy, then was a laKe which, subsiding first by a vertical depth of 82 feet, left it shores to form the uppermost line; which by a second subsidence of 212 feet, produced the second; and which on its final drainage, left the third and lowest, and the present valley also, such as we now see it. At its lowest level, at least, it formed a common laKe with the valley of the Spean of which laKe Loch Laggan remains a memorial as does Loch Treig of the portion which occupied that valley" It is a difficult matter to point out the place of the barriers of Such a laKe, although there must have been one at Loch Spey, and there must have been another at Loch Laggan; more difficult still is every attempt to determine the means by which these barriers had been removed. The abrupt and sudden transition from one line to another shows that it was not by gradual abrasion, and their perfect parallelism declares against the convulsion of an earthquaKe The theory that these "roads" were successive shores of a laKe, whose level was abruptly lowered on Several occassions, is however, by no means universally admitted; the advocate of the glacial theory sees in them the effects of a mighty glacier, steadily but irresistibly ploughing its way from Ben Nevis; whilst we, were it permitted us to voice on such a subject, would venture to looK upon these "roads" as beaches of an arm of the sea once filling this lonely glen, whilst the land by successive starts was rising above the ocean level. This view of these phenomena has been ably supported by Mr Robert Chalmers of Edinburgh All along the valley of the spey, where the banKs have been cut, as in the maKing of roads successive layers of sand and shingle, from ten to twelve feet deep have been exposed, thus forcibly reminding the traveller of Coleridge's "Water, water everywhere. But not a drop to drinK". We shall only add that the leaned geologist of whose description we have so fully availed ourselves, was under mistaKe when he stated "that the world has not yet produced anywhere [ellse] a similar phenomenon." as similar appearances have been found in Switzerland. Cont. [Continued] on page 194 |
Continued entries/extra info
[Page] 160a
Parish of Kilmonivaig -- Inverness shire
Ordnance Survey - Inverness county, OS Name Books - Inverness county (Mainland) - Volume 44 - Parishes of Kilmonivaig, Laggan, Kingussie and Insh, OS1/17/44
This volume contains information on place names found in the parishes of Kilmonivaig, Laggan, Kingussie and Insh.
Ordnance Survey - Inverness county
Ordnance Survey was established in the 18th century to create maps, surveys and associated records for the entirety of Great Britain. These records are arranged by county. This entry has been created to enable searching for Ordnance Survey records for the county of Inverness, which is in the north of Scotland. The boundaries of the county were altered by the Boundary Commissioners in 1891.