1000 resultados para Dickson Land


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Map measuring 28 cm. x 24 cm. showing the Walter H. Dickson land along the road from Blenheim, n.d.

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The Dickson Land peninsula is located in central West-Spitsbergen between the NNE branches of Isfjorden. The climatic firn line lying at 500 m causes plateau glaciers with outlet tongues which are characteristic of S-Dickson Land. The distribution of valley glaciers and the variations of the orographic firn line depend on wind direction. In comparing the firn lines established by the methods of LICHTENECKER (1938) and VISSER (1938), to the values calculated by the method of v. HÖFER (1879), differences of up to l07 m are found. These differences may depend on the inclination and distance relationships of the glaciers above and below the real firn lines. During the latest glacial advance, Dickson Land was located on the peripheries of two local glaciation centers. At that time an inland glaciation of West-Spitsbergen did not exist . The formation of a subglacial channel system dates back to the maximum extent of the late glacial phase before 17500 B.P, (+2000/-1375 years). A correlation of postglacial stadia and 14C dated marine terraces (FEYLING-HANSSEN & OLSSON, 1960; FEYLING-HANSSEN, 1965) is possible. Considering isostatic movement and the difference between calculated and real firn lines, a postglacial stadium at about 10400 B. P. can be reconstructed with a firn line lying 265 m above former sea level. On average, the absolute depression below the recent firn line amounted to 246 m. Stagnation at 9650 B.P. coincided with a firn line at 315 m above former sea level and a depression of 173 m. Around 1890 A.D., glacial fluctuations corresponded to a firn line at 415 m (depression: 64 m). To some extent the morphology of the main valleys appears to depend on structure and petrography. Therefore their value as indicators of former glaciations is questionable. The periglacial forms are shown on a large-scale map. At the time of the "Holocene warm interval", between 7000 and 2000 B.P. (FEYLING-HANSSEN, 1955a, 1965), an increase of periglacial activity seems likely. This can be explained by a simultaneous increase in the depth of the active layer in both soil and bedrock.

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Svalbard is a heavily glacier-covered archipelago in the Arctic. Dickson Land (DL), in the central part of the largest island, Spitsbergen, is relatively arid, and as a result, glaciers there are relatively small and restricted mostly to valleys and cirques. This study presents a comprehensive analysis of glacier changes in DL based on inventories compiled from topographic maps and digital elevation models for the Little Ice Age maximum (LIA), the 1960s, 1990 and 2009/11. Total glacier area decreased by ~38 % since the LIA maximum, and front retreat has increased over the study period. Recently, most of the local glaciers have been consistently thinning in all elevation bands, in contrast to larger Svalbard ice masses which remain closer to balance. The mean 1990–2009/11 geodetic mass balance of glaciers in DL is among the most negative from the Svalbard regional means known from the literature.

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Notice of sale of land for taxes to W. H. Dickson. This is a handwritten document. The land consists of 4 acres of Lot no. 12 in the 5th Concession of Wainfleet. This is dated May 23, 1857 [signatures are illegible]. On the back there is a note that Walter Hamilton Dickson has transferred this land to Joseph Augustus Woodruff, Dec. 3, 1861.

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Explanation of the Land Surrendered to the Crown by the Six Nations Indians for Mr. Dickson: 1 handwritten page explaining the Six Nations surrender of land to the Crown in order to allow the Crown to transfer the land to Mr. Dickson to compensate him for legal fees. [This is not an older document. It was possibly written by the Niagara Historical Society], n.d.

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William Dickson (1799-1877) was the son of the prominent Niagara businessman and politician William Dickson (1769-1846). William was educated in Edinburgh, Scotland, and settled in Galt, Ontario, upon his return to Canada. His father had business affairs in Dumfries and Galt, which he left in his sons charge when he retired to Niagara in 1837. William had an older brother, Robert, and younger brother, Walter, both of whom served in the Militia and became involved in politics.

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Indenture of transfer of parcels of land purchased at sales of land for taxes to Joseph A. Woodruff of the Town of Clifton. Transferred by The Honourable Walter Hamilton Dickson of the Town of Niagara. These lands are located in Caistor, Wainfleet, Humberstone, Crowland, Grimsby, Gainsboro and Pelham, Nov. 1, 1861.

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Indenture of deed of quit claim (original copy and memorial of) between Walter H. and Charlotte Dickson of Guelph and Joseph A. Woodruff of Niagara for land in the Town of Clifton, Stamford and Welland, Aug. 10, 1863.

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Certificate that Joseph Kingsmill, sheriff, has sold 3 ½ acres in Lot no. 34 in the 3rd Concession of Wainfleet to W. H. Dickson, May 23, 1857.

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Certificate that Joseph Kingsmill, sheriff, has sold 3 acres in Lot no. 7 [?] in Grimsby to W. H. Dickson, May 23, 1857.

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Certificate that Joseph Kingsmill, sheriff, has sold 6 acres in Lot no. 9 in the 4th Concession of Caistor to W.H. Dickson [originally said S.D. Woodruff, but this was crossed out], May 23, 1857.

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Certificate that Joseph Kingsmill, sheriff, has sold 4 acres in Lot no. 18 in the 4th Concession of Humberland to W.H. Dickson, May 23, 1857.

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Certificate that Joseph Kingsmill, sheriff, has sold 4 acres in Lot no.1 in the 6th Concession of Grimsby to W. H. Dickson, May 23, 1857.

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Certificate that Joseph Kingsmill, sheriff, has sold 4 acres in Lot no.33 in the 4th Concession of Wainfleet to W.H. Dickson, May 23, 1857.

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Certificate that Joseph Kingsmill, sheriff, has sold 7 acres in Lot no. 24 in the 2nd Concession of Caistor to W. H. Dickson, May 23, 1857.