Annual report of the Commissioners of the State Reservation at Niagara, 1906-1907.

Report year irregular.

Annual report of the Commissioners of the State Reservation at Niagara, 1907-1908.

Report year irregular.

Annual report of the Commissioners of the State Reservation at Niagara, 1908-1909.

Report year irregular.

Annual report of the Commissioners of the State Reservation at Niagara, 1909-1910.

Report year irregular.

Annual report of the Commissioners of the State Reservation at Niagara, 1911-1912.

Report year irregular.

Annual report of the Commissioners of the State Reservation at Niagara, 1912-1913.

Report year irregular.

Annual report of the Commissioners of the State Reservation at Niagara.

Report year irregular.

Annual report of the Commissioners of the State Reservation at Niagara, 1915-1916.

Report year irregular.

Annual report of the Commissioners of the State Reservation at Niagara, 1917-1918.

Report year irregular.

Supplemental report of the Commissioners of the State Reservations at Niagara /

"General plan for the improvement of the Niagara reservation", prepared by Frederick Law Olmstead and Calvert Vaux.

Animals without Borders: Farmed Animal Resistance in New York

While billions of farmed animals are immobilized within agribusiness, every year some of these animals manage to break free. This thesis examines the stories of those who flee slaughterhouses and the public response to these individuals. My objective is to understand how animals resist and the role that their stories play in disrupting the ways that humans, particularly as consumers, are distanced from the violence of animal enterprises. Included are six vignettes that allow for an in-depth case study of those who have escaped within New York State. Located in the interdisciplinary field of critical animal studies, my inquiry draws upon new animal geographies, transnational feminisms, and critical discourse analysis. This contribution provides discussion of farmed animal resistance in particular and compares experiences and representations of their resistance from both the “view from below,” which is learned through the animals’ caretakers, and a “view from above,” which is gleaned from their representations in corporate-driven mainstream media.

A roll of non-commissioned Officers, Drummers, & Private men enlisted for the first Battalion of the King’s Royal Regiment of New York, 1781 [photocopy]

The King’s Royal Regiment of New York was a Loyalist regiment that served on the Canadian frontier during the American Revolutionary War. The regiment was commanded by Sir John Johnson, who recruited members from the settlers on his estates in the Mohawk Valley. After the War, the two battalions of the regiment were disbanded. The First Battalion settled on the north shore of the St. Lawrence, while the Second Battalion settled by the Bay of Quinte.

Comparison of the ant assemblages in three phytophysionomies: Rocky field, secondary forest, and riparian forest - A case study in the state park of Ibitipoca, Brazil

Ant assemblages are almost all related with the vegetation composition and so can provide us important information for conservation strategies, which are especially relevant to an environmentally protected area. We sampled the ant fauna in three different phytophysionomies in order to verify if the composition of ant species is different among the areas, especially because one of the areas is a Rocky Field and there is little information about the ant fauna in this habitat. A total of 8730 individuals were registered and an NMDS analysis showed that the ant assemblies are different at the three phytophysionomies (Rocky Field, Riparian Forest, and Secondary Forest). This study shows that the species that compose the ant assemblies in different phytophysionomies are a reflex of the environment, supporting the hypothesis that the vegetational composition results in different compositions in the ant assembly. Vegetal composition is determinant in the formation of the litter and consequently in the occurrence of ant species that depend on this layer of organic matter for nesting and foraging. © 2012 Juliane Floriano Santos Lopes et al.

Chemical composition of Lake George (New York) iron-manganese nodules and underlying sediment

Lake George, New York, is the site of a new discovery of iron-manganese nodules. These nodules occur at a water depth between 21 and 36 m along a stretch of lake extending for about 5 mi north and south of the Narrows, a constricted island-dotted area which separates the north and south Lake George basins. Nodules occur on or within the uppermost 5 cm of a varved glacial clay. Some areas are solidly floored with a carpet of nodules in areas where active currents keep the nodules exposed. The nodules form around nuclei which consist of clay and less commonly of spore capsules, detrital particles, or bark. By their shape we recognize three types of nodules: spherical, discoidal, and lumps. On X-ray examination all nodules show small goethite peaks; in one nodule the manganese mineral birnessite was identified. Manganese and part of the iron appears to be in X-ray amorphous ferromanganese compounds. The Lake George nodules are enriched in iron with respect to marine nodules but are lower in manganese. They have a higher trace element concentration than nodules from other known freshwater lake occurrences, but a lower concentration than marine nodules.

Description and chemical composition of ferromanganese deposits from Oneida Lake, New York

Saucer-shaped iron-manganese crusts occur adjacent to gravel shoal areas in Oneida lake in central New York. The crusts usually have a crude concentric banding owing to an alternation of orange, iron-rich layers and black, iron-poor layers. Materials from both types of layers are x-ray amorphous. The Oneida lake crusts, like most other freshwater manganese nodules, contain about the same Mn concentration as marine manganese nodules, but are usually higher in Fe and lower in trace metals than their marine equivalents. Although Fe and Mn may be precipitating directly from the lake water, it is more likely that the oxidate crusts are the result of precipitation of Fe and Mn when reduced sediment pore water comes in contact with well oxygenated bottom waters. Organisms, particularly bacteria, may play a role in the formation of the crusts, but to date no evidence of this has been found.