1993, ISBN: 9781234437077

RareBooksClub. Paperback. New. This item is printed on demand. Paperback. 40 pages. Dimensions: 9.7in. x 7.4in. x 0.1in.This historic book may have numerous typos and missing text. Purc… More...

RareBooksClub. Paperback. New. This item is printed on demand. Paperback. 40 pages. Dimensions: 9.7in. x 7.4in. x 0.1in.This historic book may have numerous typos and missing text. Purchasers can download a free scanned copy of the original book (without typos) from the publisher. Not indexed. Not illustrated. 1885 edition. Excerpt: . . . at Forest Lawn Cemetery next Thursday. Among the invited guests are President Arthur, Governor Cleveland, and the Hon. George Bancroft, the historian; Mayor Scoville, the Common Council, City Clerk Burns and other prominent city officials and citizens; the presidents of all historical societies in the United States and Canada; Professor D. Wilson, the eminent English ethnologist, now of Toronto University, Ont. ; the Hon. Horatio Seymour of Utica, and the Hon. Judge George W. Clinton of Albany, who will deliver the address; Mrs. Harriet Maxwell Converse of New York, whose husband was a noted Indian teacher and historian; Gen. Ely S. Parker of New York, the highest chief in the Seneca Nation, formerly of General Grants staff; the Hon. James G. Blaine of Augusta, Me. , and Mr. W. Furness of Crystal Springs, N. Y. ; Mr. G. A. Shaw, editor of the New York Evening Telegram, and Lieut. Col. J. T. Gilkison, Superintendent and Commissioner of Indians, Brantford, Ont. Besides these the presidents and officers of the Buffalo Young Mens Christian Association, the Buffalo Society of Natural Sciences, the German Young Mens Association, the Young Mens Catholic Association, the Fine Arts Academy, and the Lutheran Young Mens Association have been invited. The Misses Eva and Pauline Johnson, daughters of the late Chief George H. M. Johnson of Chiefswood, near Brantford, Ont. , will be the guests of the family of Judge Sheldon, on Main street. Miss Jessie M. Osborne, of Brantford, a great-granddaughter of the celebrated Mohawk Chieftain, Joseph Brant, will be entertained, together with Chief John Mountpleasant and wife, of the Tuscarora Nation, by the family of William C. Bryant, Esq. These young Indian ladies are well educated and accomplished. About forty. . . This item ships from La Vergne,TN., RareBooksClub, RareBooksClub. Paperback. New. This item is printed on demand. Paperback. 28 pages. Original publisher: Albany, Calif. : U. S. Dept. of Agriculture, Forest Service, Pacific Southwest Research Station, 1993 OCLC Number: (OCoLC)228806949 Subject: Earthworms -- California, Southern. Excerpt: . . . At this stage nothing definitive can be said regarding soil vegetation, which was within 50-100 m of the vernal pools types or soil preferences on the drier sites we sampled. The where the soil depth is generally 20 cm or less. majority of soils were deeper than 35 cm, and textures ranged Several possible explanations emerge. The Diplocardia spe from heavy clays to sands. Soil orders included Mollisols, cies may have restricted and specialized distributions or soil Entisols, Alfisols, Inceptisols, and Vertisols. Most, but not all, depth limitations. Conditions at the time of collecting may not had mollic or umbric epipedons ( diagnostic surface horizons ) have been conducive to finding the species present in the grass-that were darker in color than the subsurface horizons. The forb community on Mesa de Burro. Neither species of predominate soil feature indicative of earthworm activity ( not Diplocardia was found in other chaparral sites, grasslands, or soil preference ) is in the kind and degree of soil structure, riparian areas on the Preserve. However, Lumbricidae and particularly in the surface horizons. Most earthworm-worked Ocnerodrilidae were found in the grassland and riparian habi soils we investigated had some granular or crumb structure to tats of the Preserve. Diplocardia CAI was collected from them; loose single spheroids to aggregated spheriods, ranging numerous grassland sites on the Trabuco and Cleveland Dis from less than 1 mm to greater than 5 mm. We believe tricts of the Cleveland National Forest. earthworm castings are the principal components contributing We repeatedly observed, particularly under oaks, that where to this distinctive type of structure. It should be possible to earthworms, their burrows, and castings were abundant, . . . This item ships from La Vergne,TN., RareBooksClub<

1993, ISBN: 9781234437077

Rarebooksclub.com. Paperback. New. This item is printed on demand. Paperback. 28 pages. Original publisher: Albany, Calif. : U. S. Dept. of Agriculture, Forest Service, Pacific Southwes… More...

Rarebooksclub.com. Paperback. New. This item is printed on demand. Paperback. 28 pages. Original publisher: Albany, Calif. : U. S. Dept. of Agriculture, Forest Service, Pacific Southwest Research Station, 1993 OCLC Number: (OCoLC)228806949 Subject: Earthworms -- California, Southern. Excerpt: . . . At this stage nothing definitive can be said regarding soil vegetation, which was within 50-100 m of the vernal pools types or soil preferences on the drier sites we sampled. The where the soil depth is generally 20 cm or less. majority of soils were deeper than 35 cm, and textures ranged Several possible explanations emerge. The Diplocardia spe from heavy clays to sands. Soil orders included Mollisols, cies may have restricted and specialized distributions or soil Entisols, Alfisols, Inceptisols, and Vertisols. Most, but not all, depth limitations. Conditions at the time of collecting may not had mollic or umbric epipedons ( diagnostic surface horizons ) have been conducive to finding the species present in the grass-that were darker in color than the subsurface horizons. The forb community on Mesa de Burro. Neither species of predominate soil feature indicative of earthworm activity ( not Diplocardia was found in other chaparral sites, grasslands, or soil preference ) is in the kind and degree of soil structure, riparian areas on the Preserve. However, Lumbricidae and particularly in the surface horizons. Most earthworm-worked Ocnerodrilidae were found in the grassland and riparian habi soils we investigated had some granular or crumb structure to tats of the Preserve. Diplocardia CAI was collected from them; loose single spheroids to aggregated spheriods, ranging numerous grassland sites on the Trabuco and Cleveland Dis from less than 1 mm to greater than 5 mm. We believe tricts of the Cleveland National Forest. earthworm castings are the principal components contributing We repeatedly observed, particularly under oaks, that where to this distinctive type of structure. It should be possible to earthworms, their burrows, and castings were abundant, . . . This item ships from La Vergne,TN., Rarebooksclub.com<