George Upper collection, 1989, 1995, undated

George Upper is a Niagara area artist. His limited edition prints feature local scenes, many from Port Dalhousie, Ontario.

Indenture between George Upper and Joseph Augustus Woodruff

Indenture (vellum) between George Upper of Niagara to Joseph Augustus Woodruff of Niagara for the sale of the west half of lot no. 20 in the 2nd Concession in Nissouri. This was registered March 17, 1853 - instrument no. 113. December 1, 1852.

Indenture (vellum) between George Upper and Joseph Augustus Woodruff

Indenture (vellum) between George Upper of Niagara to Joseph Augustus Woodruff of Niagara for the sale of the east half of lot no. 28 in the 2nd Concession on Nissouri. This was registered March 17, 1853 in folio 128 - instrument no. 114, December 1, 1852.

Province of Upper Canada Grant to George Upper

Province of Upper Canada Grant (vellum) to George Upper of the Township of Niagara. He was formerly a private in the Lincoln Militia. He is granted 100 acres in the east half of lot no.28 in the 2nd Concession in the Township of Nissouri. This was registered Dec. 1827 – Folio no. 242. This document is extremely stained and torn on the lower half. No effect on the text, Nov. 27, 1827.

Indenture between Isaac Fuller of the Township of Niagara and George Upper of the Township of Niagara

Indenture between Isaac Fuller of the Township of Niagara and George Upper of the Township of Niagara for the west half of Lot no. 29 in the 2nd Concession of the Township of Nissouri, Jan. 29, 1830.

Indenture of quit claim between Thomas Fuller of the Township of Niagara and George Upper of the Township of Niagara

Indenture of quit claim between Thomas Fuller of the Township of Niagara and George Upper of the Township of Niagara for 100 acres in the back half of Lot no. 29 in the 2nd Concession in the Township of Niagara, Oct. 26, 1852.

Indenture of Bargain and Sale (vellum) between Captain George Salmon, formerly of Upper Canada and now of Middlesex, England and Charles Hampden Turner of Surrey, England

Indenture of Bargain and Sale (vellum) between Captain George Salmon, formerly of Upper Canada and now of Middlesex, England and Charles Hampden Turner of Surrey, England for 1,200 acres lying in the Township of Windham in the County of Norfolk in the province of Upper Canada, May 5, 1819.

Summons to Legislative Council of Upper Canada bestowed on William Dickson by George the Third, signed by the Attorney General

Summons to Legislative Council of Upper Canada bestowed on William Dickson by George the Third, signed by the Attorney General. The Crown Seal is faded, but intact, Nov. 16, 1815.

Upper Canada Warrant of Appraisement

Upper Canada warrant of appraisement: warrant of the Surrogate of the District of Niagara to Isaac Hurst, George Bradshaw and Bernard Frey to appraise the goods and chattels of James Fields Deacon. This item is torn and has been taped. There is a hole where the seal has been and there is a stain. This does not affect the text, June 15, 1801.

Dr. George Nogradi

Professor of Rec and Leisure Studies.

Diagenesis and geochemical stratigraphy of Upper Pennsylvanian madera brachiopods, New Mexico

Owing to the fact that low-Mg calcite fossil shells are so important in paleoceanographic research, 249 brachiopod, cement and matrix specimens from two neighboring localities (Jemez Springs and Battleship Rock), of the Upper Pennsylvanian Madera Formation were analyzed. Of which, about 86% of the Madera brachiopods are preserved in their pristine mineralogy, microstructure and geochemistry. Cement and matrix samples, in contrast, have been subjected to complete but variable post-deposition~1 alteration. It is confirmed that the stable isotope data of brachiopods are much better than that of matrix material in defining depositional parameters. Because there is no uniform or constant relationship between the two data bases (e.g., from 0.1 to 3.0%0 for 0180 and from 0.2 to 6.7%0 for 013C in this study), it is not possible to make corrections for the matrix data. Regarding the two stratigraphic sections, elemental and petrographic analyses suggest that Jemez Springs is closer to Penasco Uplift than Battleship Rock. Seawater at Jemez Springs is more aerobic, and the water chemistry is more influenced by continental sources than that at Battleship Rock. In addition, there is a relatively stronger dolomitization in the mid-section of the Battleship Rock. Results further suggest that no significant biogenic fractionation or vital effects occurred during their shell secretion, suggesting that the Madera brachiopods incorporated oxygen and carbon isotopes in equilibrium with the ambient seawater. This conclusion is not only drawn from the temporal and spatial analyses, but also supported by brachiopod inter-generic comparison (Composita and Neospirifer) and statistical analysis ( t-test).

Is technology a threat to education? : the contribution of George Parkin Grant

Thesis (M.Ed.)-- Brock University, 1995.

Patterns of faunal change at an upper Cambrian trilobite extinction event, Nolichucky Formation, Tennessee and Virginia

During the Upper Cambrian there were three mass extinctions, each of which eliminated at least half of the trilobite families living in North American shelf seas. The Nolichucky Formation preserves the record of one of these extinction events at the base of the Steptoean Stage. Sixty-six trilobite collections were made from five sections In Tennessee and Virginia. The lower Steptoean faunas are assigned to one low diversity, Aphelaspis-dominated biofacies, which can be recognized in several other parts of North America. In Tennessee, the underlying upper Marjuman strata contain two higher diversity biofacies, the Coosella-Glaphyraspis Biofacies and the Tricrepicephalus-Norwoodiid Biofacies. At least four different biofacies are present in other parts of North America: the Crepicephalus -Lonchocephalus Biofacies, the Kingstonia Biofacies, the Cedaria Biofacies, and the Uncaspis Biofacies. A new, species-based zonation for the Nolichucky Formation imcludes five zones, three of which are new. These zones are the Crepicephalus Zone, the Coosella perplexa Zone, the Aphelaspis buttsi Zone, the A. walcotti Zone and the A. tarda Zone. The Nolichucky Formation was deposited within a shallow shelf basin and consists largely of subtidal shales with stormgenerated carbonate interbeds. A relative deepening is recorded In the Nolichucky Formation near the extinction, and is indicated In some sections by the appearance of shale-rich, distal storm deposits above a carbonate-rich, more proximal storm deposit sequence. A comparable deepening-upward sequence occurs near the extinction in the Great Basin of southwestern United States and in central Texas, and this suggests a possible eustatic control. In other parts of North America, the extinction IS recorded In a variety of environmental settings that range from near-shore to slope. In shelf environments, there is a marked decrease in diversity, and a sharp reduction in biofacies differentiation. Although extinctions do take place in slope environments, there IS no net reduction in diversity because of the immigration of several new taxa.

Trilobites of the Upper Cambrian (Marjuman) Pika formation of the Southern Canadian Rocky Mountains

The Upper Cambrian Pika Formation in the southern Canadian Rocky Mountains forms a complete lithologic Grand Cycle. The overall pattern of deposition is one of shallowing upwards from a subtidal, muddy, storm-influenced basin to a shallow carbonate bank. The Pika passes gradationally into the overlying inter- to supratidal siliciclastics of the Arctomys Formation. This transition probably reflects a fall in relative sea level. 2 Twenty seven collections from three sections yielded trilobites. The faunas are assigned to two low-diversity biofacies: the Marjumia - Spencella Biofacies and the GZyphaspis - menomoniid Biofacies. In contrast to biofacies of deeper, open-shelf environments, such as the Wheeler and Marjum formations of Utah, the Pika biofacies lack agnostid trilobites. Consequently, agnostid-based zonations defined elsewhere in North America cannot be applied to the Pika and a new sequence of three zones and one informal fauna is proposed for use in inner shelf facies. Eleven species belonging to six genera are described and illustrated. The species Marjumia bagginsi is new. Other genera present are: Bolaspidella, Knechtelia, GZyphaspis and Spencella, in addition to a number of indeterminate forms

Oath of Allegiance to King George III

Transcript (original spelling and grammar retained): We the Commissioned Officers belonging to the Second Regiment of Lincoln Militia - Do sincerely promise and swear that we will be faithful and bear true allegiance to his Majesty King George, and heirs will defend to the utmost of our power against all traitorous conspiracies and attempts whatsoever which shall be made against his Person, Crown or Dignity; and we will do our utmost endeavours to disclose and make them known to his Majesty, His Heirs and successors, all treasons and traitorous conspiracies and attempts, which we shall know to be against Him or them. So help us God. Thomas Clark - Lt. Col. David Secord - Major John Crysler - Capt James Macklin - Capt John [Ross] - [Captain] [Abraham] Bowman - Lieut Gilbert McMicking - Quartmaster John [Misiner] - Ensign Robert Campbell - Capt John [Couke] - Ensign Nicholas Smith - Lieut I certify that the officers who have here [subscribed] the oath took it before me at Chippawa 4 Sept 1812 Thomas Dickson JP