The diocese of Western New York, 1897-1931,

"The book is intended to be supplementary to the very excellent 'Diocese of Western New York' published by the Rev. Charles Welles Hayes [1904]"--Pref.

Journal of the ... annual convention, Diocese of Western New York.

Series of published journals begins with those for the primary convention (1838), a special convention in 1839, and the 2nd annual convention (1839).

Date guide to birds of western New York and adjacent Ontario.

"An aid to reporting unusual observations."

Journal of the ... annual convention, Diocese of Western Michigan.

Vol. for 23rd (1897) includes diocesan Constitution and canons.

The diocese of western Michigan; a history /

Bibliography: p. 674.

Settlement in the West : Sketches of Rochester; with incidental notices of western New York.

Microfilm. Ann Arbor, Mich., University Microfilms [n.d.] (American Culture Series, Reel 122.8)

Genealogical and family history of western New York; a record of the achievements of her people in the making of a commonwealth and the building of a nation.

Paged continuously.

From the stage coach to the pulpit, being an autobiographical sketch, with incidents and anecdotes, of Elder H.K. Stimson, the veteran pioneer of western New York, now of Kansas.

Mode of access: Internet.

The centennial history of the Protestant Episcopal church in the diocese of New York, 1785-1885.

"Prepared for the press by a member of the Committee, under its direction."--Pref.

Journal of the ... convention of the Diocese of New York.

Mode of access: Internet.

Debates of the House of deputies in the General convention of the Protestant Episcopal church in the United States of America, held in New York city, October, A. D. 1874,

Mode of access: Internet.

Narrative of events connected with the rise and progress of the Protestant episcopal church in Virginia : to which is added an appendix, containing the journals of the conventions in Virginia from the commencement to the present time.

Mode of access: Internet.

Armor coats, inverse grading, and streambed scour in selected streams of Southern Ontario and Western New York /

Surface size analyses of Twenty and Sixteen Mile Creeks, the Grand and Genesee Rivers and Cazenovia Creek show three distinct types of bed-surface sediment: 1) a "continuous" armor coat which has a mean size of -6.5 phi and coarser, 2) a "discontinuous" armor coat which has a mean size of approximately -6.0 phi and 3) a bed with no armor coat which has a mean surface size of -5.0 phi and finer. The continuous armor coat completely covers and protects the subsurface from the flow. The discontinuous armor coat is composed of intermittently-spaced surface clasts, which provide the subsurface with only limited protection from the flow. The bed with no armor coat allows complete exposure of the subsurface to the flow. The subsurface beneath the continuous armor coats of Twenty and Sixteen Mile Creeks is possibly modified by a "vertical winnowing" process when the armor coat is p«natrat«d. This process results in a welld «v«loped inversely graded sediment sequence.vertical winnowing is reduced beneath the discontinuous armor coats of the Grand and Genesee Rivers. The reduction of vertical winnowing results in a more poorly-developed inverse grading than that found in Twenty and sixteen Mile Creeks. The streambed of Cazenovia Creek normally is not armored resulting in a homogeneous subsurface which shows no modification by vertical winnowing. This streambed forms during waning or moderate flows, suggesting it does not represent the maximum competence of the stream. Each population of grains in the subsurface layers of Twenty and sixteen Mile Creeks has been modified by vertical winnowing and does not represent a mode of transport. Each population in the subsurface layers beneath a discontinuous armor coat may partially reflect a transport mode. These layers are still inversely graded suggesting that each population is affected to some degree by vertical winnowing. The populations for sediment beneath a surface which is not armored are probably indicative of transport modes because such sediment has not been modified by vertical winnowing. Bed photographs taken in each of the five streams before and after the 1982-83 snow-melt show that the probability of movement for the surface clasts is a function of grain size. The greatest probability of of clast movement and scour depth of this study were recorded on Cazenovia Creek in areas where no armor coat is present. The scour depth in the armored beds of Twenty and Sixteen Mile Creeks is related to the probability of movement for a given mean surface size.

Abrasion, transport and distribution of sediment in selected streams of Southern Ontario and Western New York /

The rate of decrease in mean sediment size and weight per square metre along a 54 km reach of the Credit River was found to depend on variations in the channel geometry. The distribution of a specific sediment size consist of: (1) a transport zone; (2) an accumulation zone; and (3) a depletion zone. These zones shift downstream in response to downcurrent decreases in stream competence. Along a .285 km man-made pond, within the Credit River study area, the sediment is also characterized by downstream shifting accumulation zones for each finer clast size. The discharge required to initiate movement of 8 cm and 6 cm blocks in Cazenovia Creek is closely approximated by Baker and Ritter's equation. Incipient motion of blocks in Twenty Mile Creek is best predicted by Yalin's relation which is more efficient in deeper flows. The transport distance of blocks in both streams depends on channel roughness and geometry. Natural abrasion and distribution of clasts may depend on the size of the surrounding sediment and variations in flow competence. The cumulative percent weight loss with distance of laboratory abraded dolostone is defined by a power function. The decrease in weight of dolostone follows a negative exponential. In the abrasion mill, chipping causes the high initial weight loss of dolostone; crushing and grinding produce most of the subsequent weight loss. Clast size was found to have little effect on the abrasion of dolostone within the diameter range considered. Increasing the speed of the mill increased the initial amount of weight loss but decreased the rate of abrasion. The abrasion mill was found to produce more weight loss than stream action. The maximum percent weight loss determined from laboratory and field abrasion data is approximately 40 percent of the weight loss observed along the Credit River. Selective sorting of sediment explains the remaining percentage, not accounted for by abrasion.

The true history regarding alleged connection of the order of ancient, free and accepted Masons: with the abduction and murder of William Morgan in western New York, in 1826... (1886)

Cover title: Masonic light on the abduction and murder of Wm. Morgan.