148 resultados para Idaho. Dept. of Lands
Resumo:
Survey map and description of Abraham Neff's land created by The Welland Canal Company. Included is a written description of the land along with a drawing of the land. Noteable features include; line between A. Neff and Jacob Neffs land, line between lots, canal, bridge. The land totals 7 acres The deed for the land is dated October 25, 1836. Surveyor notes are seen in pencil on the map.
Resumo:
Survey map and description of Jacob Neff Js.'s land created by The Welland Canal Company. Included is a written description of the land along with a drawing of the land. Noteable features include; canal, line between Jacob Neff and Jacob Augustine's land. The land totals 14 acres and 1 road. The deed for the land is dated June 24, 1835. Surveyor notes are seen in pencil on the map.
Resumo:
Survey map and description of the land belonging to the Welland Canal Company at Dunnville. Created by The Welland Canal Company. Included is a written description of the land along with a drawing of the land. There are two seperate surveys done for the lands: Survey #1 (Pp. 148-149) noteable features include; the Grand River, the original boundry of the Grand River, marsh overflow, marsh, feeder river, bridge, Broad street, Lock street, Main street, embankment, dam (600 ft.), lines between lots, reserve for the ships yard, reserve for lock and dry dock, lands occupied by the canal and towpath to guard gate. The land totals 9 acres, and 3 roads, including the street. Survey #2 (Pp. 150-151) completed by George Keefer noteable features include; embankment, marsh overflow, original channel of the Grand River, salt spring, bridges, wier, proposed waste wier, Van Riper's home, proposed bridge, sulphur spring, road, Sulphur Creek, division between lots 12-17. The land totals 27 acres, and 2 perches. Surveyors notes can be seen in pencil and red ink on the survey.See also Pp. 148-151
Resumo:
Survey map of the land for the Mill Scibes Grand River Dam. Created by The Welland Canal Company. Included is a drawing of the land. Noteable features include; Sulphur Creek, post, bridge, Grand River, lot divisions, inside face of embankment. Surveyor notes are seen in pencil on the map.
Resumo:
Survey map and description of the land at the cut of the Chippewa or Welland River. Created by The Welland Canal Company. Included is a drawing of the land along with brief surveyors notes. Noteable features include; bridge, Welland River, road, Stone house, J. Cummings Esq. house, military line, military land, Old Fort, old military draw bridge. Surveyor notes are seen in pencil on the map.
Resumo:
Survey map and description of the St. Catharines ditch land created by The Welland Canal Company. Included is a one and a half page written description of the land along with two drawings of the land. For the first drawing (p.156) noteable features include; line between Soper and O. Phelps land, road along the canal, Phelps mill, brewery, lock no. 5. For the second drawing (p.157) noteable features include; aquaduct, wood land, concessions, old distillery, line of company's land. Surveyor notes are seen in pencil on the map.See Pages 154-157
Resumo:
Survey map and description of Oliver Phelp's land created by The Welland Canal Company. Included is a written description of the land along with a drawing of the land. Noteable features include; Vanderburgh's land, hydraulic ditch, locks 15-20, lot divisions. The land totals 50 acres. The deed for the land is dated June 8th, 1832. Surveyor notes are seen in pencil on the map.See also page 161. Please note the measurments listed under "overall dimensions" are for the text only if the text appears on a seperate page from the drawing.
Resumo:
Survey map of the lands of the Welland Canal Company in Thorold. Created by The Welland Canal Company. Noteable features include; Company's land, reservoir, channel of canal, bridge, Pine street, Mullen street, lot divisions. The plan is titled "Plan of Lands belonging to the Welland Canal Company being the West half of lot no. 29 and the East half of lot no.30 in the township of Thorold, adjoining Marlats Reservoir laid out in town lots, November 24th, 1834". Surveyor notes are seen in pencil on the map.
Resumo:
Survey map of the plan of the Village of Marshville, created by The Welland Canal ompany. Included is a two page drawing of the land. Noteable features include; line between 5th and 4th concessions, William Simpson's land, line between 3rd and 4th concessions, feeder, bridges, mill lots, road to Sugarloaf, old stakes, Canby lot 17, lot no.19, lot divisions. The drawing is titled "Plan of the Village of Marshville now Milton, reserveyed September 18th, 1835". Surveyor notes are seen in pencil on the map.See Pages 164-165
Resumo:
Survey map and description of a village lot in Allanburgh. Created by The Welland Canal Company. Included is a written description of the land along with a drawing of the lot. Noteable features include; Holland road, grave land, Niagara street. The land totals 3/4 of an acre. Surveyor notes are seen in pencil on the map.
Resumo:
Survey map and description of the Village of Allanburgh, created by The Welland Canal Company. Included is a drawing of the land. Noteable features include; lot divisions, Welland Canal, Niagara street, Holland road, lock 36 and 37, foundry, Canal street, mill, Canby street, Dover street, Rose street, Helen street, Water street, Falls street, Centre street, Welland street, Hall street, Clifton street, James street, Mary street, Catherine street, J.G. Stockley's land, reservoir, graveyard. Surveyor notes are seen in pencil on the map.
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List (4 pages, handwritten) of lands in the counties of Lincoln and Welland for which the Sherriff has made new deeds, n.d.
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Rocks correlated with the Hough Lake and Quirke Lake Groups of the Huronian Supergroup form part of a northeasterly trending corridor that separates 1750 Ma granitic intrusive rocks of the Chief Lake batholith from the 1850 Ma mafic intrusive rocks of the Sudbury Igneous Complex. This corridor is dissected by two major structural features; the Murray Fault Zone (MFZ) and the Long Lake Fault (LLF). Detailed structural mapping and microstructural analysis indicates that the LLF, which has juxtaposed Huronian rocks of different deformation style and metamorphism grade, was a more significant plane of dislocation than the MFZ. The sense of displacement along the LLF is high angle reverse in which rocks to the southeast have been raised relative to those in the northwest. South of the LLF Huronian rocks underwent ductile defonnation at amphibolite facies conditions. The strain was constrictional, defined by a triaxial strain ellipsoid in which X > Y > z. Calculations of a regional k value were approximately 1.3. Penetrative ductile defonnation resulted in the development of a preferred crystallographic orientation in quartz as well as the elongation of quartz grains to fonn a regional southeast-northwest trending, subvertical lineation. Similar lithologies north of the LLF underwent dominantly brittle deformation under greenschist facies conditions. Deformation north of the LLF is characterized by the thrusting of structural blocks to form angular discordances in bedding orientation which were previously interpreted as folds. Ductile deformation occurred between 1750 and 1238 Ma and is correlated with a regional period of south over north reverse faulting that effected much of the southern Sudbury region. Post dating the reverse faulting event was a period of sedimentation as a conglomerate unit was deposited on vertically bedded Huronian rocks. Rocks in the study area were intruded by both mafic and felsic dykes. The 1238 Ma mafic dykes appear to have been offset during a period of dextral strike slip displacement along the major fault'). Indirect evidence indicates that this event occurred after the thrusting at 950 to 1100 Ma associated with the Grenvillian Orogeny.
Resumo:
Thesis (M. Sc.) - Brock University, 1975.
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Thesis (M.Sc.)--Brock University, 1979.