Identifier: birdlore151913nati (find matches)
Title: Bird lore
Year: 1899 (1890s)
Authors: National Committee of the Audubon Societies of America National Association of Audubon Societies for the Protection of Wild Birds and Animals National Audubon Society
Subjects: Birds Birds Ornithology
Publisher: New York City : Macmillan Co.
Contributing Library: Smithsonian Institution Libraries
Digitizing Sponsor: Biodiversity Heritage Library

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Text Appearing Before Image:
l. AUDUBON SOCIETIES—EXECUTIVE DEPARTMENT 67 Tmc Dommerich Fund; Feed the Birds; The McLean Bill; Contribution^to the Egret Protection Fund for 1912; New Members; Junior Audu-bon Classes; From a Tennessee Audubon Worker; General News;The Audubon Plumage Law in New York and New Jersey. Manuscripts intended for publication, books, etc., for review and exchanges, should be sentlolheEdiior, at the American Museum of Natural History, 77th St. and 8th Ave., New York City. Notices of changes of addresses, renewals and subscriptions should be sent toBIRD - LORE. HARRISBURG. PA. IMPORTANT NOTICE TO ALL BIRD-LORE SUBSCRIBERS Bird-Lore is published on or near the first days of February, April. June. August. October andDecember. Failure to receive the copy due you should be reported not later than the 15th of themonths above mentioned. We cannot undertake to supply missing numbers after the month inwhich they were issued. Entered as second-class mail matter in the Post Office at Harrisburg, Pa.
Text Appearing After Image:
1. McKays Snow Bunting. Male. Summer 3. Snow Bunting, Female, Summer 2. Snow Bunting, Male, Summer 4. Snow Bunting. Male. Fall 5. Snow Bunting. Male, Spring(One-half Natural Size) A BI-MONTHLY MAGAZINE DEVOTED TO THE STUDY AND PROTECTION OF BIRDS Official Organ of The Audubon Societies Vol. XV January—February, 1913 No. 1 The Duck Hawks of Taughannock Gorge By A. A, ALLEN and H. K. KNIGHT With photographs by H. K. Knight WHEN the glaciers receded from central New York, they left a seriesof long, narrow basins that have come to be known as the FingerLakes. Before the time of the glaciers, these lakes were riverswhose waters poured into a great sea to the north. Tongues of ice, forcingtheir way through the stream beds, gouged them out hundreds of feet in depth,and frequently filled their tributaries with debris. When the ice receded,these tributaries were left stranded, as it were, high above the lake, and wereforced to cut new channels and to drop their waters hundreds of feet to its

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