Shelley memorials: from authentic sources. To which is added an Essay on Christianity,

Mode of access: Internet.

Dollars and cents /

Frontispiece and plates facing p. 96 and 280.

James Fenimore Cooper.

Mode of access: Internet.

Mediterranean pilot.

v. 3. The southeast of Italy, the shores of the Adriatic and Ionian Seas to Cape Matapan -- v. 4. From Cape Matapan (Greece) eastward, the Mediterranean archepelago, and the southern shore of the Mediterranean Sea, eastward to Ras Asjdir(Libia).

Coastal zone management [microform] : hearings before the Subcommittee on Oceanography of the Committee on Merchant Marine and Fisheries, House of Representatives, Ninety-sixth Congress ....

Reuse of record except for individual research requires license from Congressional Information Service, Inc.

Memoir of the Rev. Nathan Parker, D.D., late pastor of the South church and parish in Portsmouth, N.H.

Sabin 101389.

A plain statement of the reasons which led to a dissolution of the connection of the author with the Methodist Episcopal church,

Mode of access: Internet.

New plays from old tales, arranged for boys and girls,

Aucassin and Nicolette.--The birthday of the infants. Wilde.--The princess who hid her shores. Nyblom.--Tamlane. Old ballad.--Pilgrim's progress. Bunyan.--Three Sundays in a week. Poe.--On the old plantation. Prynelle.--Feathertop. Hawthorne.

Thomas Carlyle; a history of his life in London, 1834-1881.

Mode of access: Internet.

Pier at White Lake entrance-to channel-1895

verso: Lake Michigan showing frequent debris from the numerous lumber mills along its shores-years ago

Kernsynthesen mit Hulfe von [3,5]-Dichlorsalicylsaurechlorid /

Thesis (doctoral)--Rheinische Friedrich-Wilhelms-Universitat zu Bonn.

Complete works.

v. 1. Drift from two shores.--v. 2. A waif of the plains.--v. 3. A ward of the Golden Gate.--v. 4. Trent's trust.--v.5. Condensed novels.--v.6 Barker's luck.--v. 7. The luck of Roaring Camp.--v. 8. Complete poetical works.--v. 9. Openings in the old trail.--v. 10. Under the redwoods.--v. 11. From sand hill to pine.--v. 12. Mr. Jack Hamlin's mediaton.--v. 13. Stories in light and shadow.--v. 14. Tales of trail and town.--v. 15. Three partners.--v. 16. Tales of the Argonauts.--v. 17. Mrs. Skagg's husbands.--v. 18. Clarence.--v. 19. The bell ringer of angel's.--v. 20. A protegee of Jack Hamlin's.--v. 21. Sally Dows.--v. 22. A first family of Tasajara.--v. 23. Colonel Starbottle's client.--v. 24. Cressy.--v. 25. A sappho of Green Springs.

Outlines of psychology.

Mode of access: Internet.

Hydrogeophysical characterization of anisotropy in the Biscayne Aquifer using geophysical methods

The anisotropy of the Biscayne Aquifer which serves as the source of potable water for Miami-Dade County was investigated by applying geophysical methods. Electrical resistivity imaging, self potential and ground penetration radar techniques were employed in both regional and site specific studies. In the regional study, electrical anisotropy and resistivity variation with depth were investigated with azimuthal square array measurements at 13 sites. The observed coefficient of electrical anisotropy ranged from 1.01 to 1.36. The general direction of measured anisotropy is uniform for most sites and trends W-E or SE-NW irrespective of depth. Measured electrical properties were used to estimate anisotropic component of the secondary porosity and hydraulic anisotropy which ranged from 1 to 11% and 1.18 to 2.83 respectively. 1-D sounding analysis was used to models the variation of formation resistivity with depth. Resistivities decreased from NW (close to the margins of the everglades) to SE on the shores of Biscayne Bay. Porosity calculated from Archie's law, ranged from 18 to 61% with higher values found along the ridge. Higher anisotropy, porosities and hydraulic conductivities were on the Atlantic Coastal Ridge and lower values at low lying areas west of the ridge. The cause of higher anisotropy and porosity is attributed to higher dissolution rates of the oolitic facies of the Miami Formation composing the ridge. The direction of minimum resistivity from this study is similar to the predevelopment groundwater flow direction indicated in published modeling studies. Detailed investigations were carried out to evaluate higher anisotropy at West Perrine Park located on the ridge and Snapper Creek Municipal well field where the anisotropy trend changes with depth. The higher anisotropy is attributed to the presence of solution cavities oriented in the E-SE direction on the ridge. Similarly, the change in hydraulic anisotropy at the well field might be related to solution cavities, the surface canal and groundwater extraction wells.^