The spell of southern shores; or, From sea to sea in Italy,

Mode of access: Internet.

Nights and days on the gypsy trail through Andalusia and on other Mediterranean shores.

First edition.

Echoes from foreign shores : letters from Bible lands for children /

Mode of access: Internet.

Along New England shores,

Mode of access: Internet.

McDonald of Oregon : A tale of two shores /

Mode of access: Internet.

Sketches of naval life with notices of men, manners and scenery on the shores of the Mediterranean in a series of letters from the Brandywine and Constitution frigates.

Mode of access: Internet.

Travels through part of the Russian Empire and the country of Poland; along the southern shores of the Baltic.

Shaw and Shoemaker 37960.

Correspondence of Lord Byron, with a friend : including his letters to his mother, written from Portugal, Spain, Greece, and the shores of the Mediterranean, in 1809, 1810 and 1811 /

Mode of access: Internet.

Submarine slumps in delta-front sandstones of the Upper Cretaceous Blair Formation, Rock Springs uplift, Wyoming : syndepositional slumps on the western shores of the interior Cretaceous sea /

Mode of access: Internet.

A Trip around Buzzard's Bay shores /

Mode of access: Internet.

Intercolonial outing! : along the shores of the lower St. Lawrence and through the provinces by the sea.

"This is the third revision of the original story"--Pref.

Northward over the "great ice" : a narrative of life and work along the shores and upon the interior ice-cap of northern Greenland in the years 1886 and 1891-1897.

Mode of access: Internet.

Flora of New Bedford and the shores of Buzzard's Bay, with a procession of the flowers /

Includes index.

Coral mortality increases wave energy reaching shores protected by reef flats: Examples from the Seychelles

In the granitic Seychelles, many shores and beaches are fringed by coral reef flats which provide protection to shores from erosion by waves. The surfaces of these reef flats support a complex ecology. About 10 years ago their seaward zones were extensively covered by a rich coral growth, which reached approximately to mean low water level, but in 1998 this was largely killed by seawater warming. The resulting large expanses of dead coral skeletons in these locations are now disintegrating, and much of the subsequent modest recovery by new coral recruitment was set back by further mortalities. A mathematical model of wave energy reaching shorelines protected by coral reef flats has been applied to 14 Seychelles reefs. It is derived from equations which predict: (1) the raised water level, or wave set-up, on reef flats resulting from wave breaking, which depends upon offshore wave height and period, depth of still water over the reef flat and the reef crest profile, and (2) the decay of energy from reef edge to shoreline that is affected by width of reef flat, surface roughness, sea level rise and 'pseudo-sea level rise' created by increased depth resulting from disintegration of coral colonies. The model treats each reef as one entity, but because biota and zonation on reef flats are not homogenous, all reefs are divided into four zones. In each, cover by both living and dead biota was estimated for calculation of parameters, and then averaged to obtain input data for the model. All possible biological factors were taken into account, such as the ability of seagrass beds to grow upwards to match expected sea level rise, reduction in height of the reef flat in relation to sea level as zones of dead corals decay, and the observed 'rounding' of reef crests as erosion removes corals from those areas. Estimates were also made of all these factors for a time approximately a decade ago, representing a time before the mass coral mortality, and for approximately a decade in the future when the observed rapid state of dead coral colony disintegration is assumed to have reached an end point. Results of increased energy over the past decade explain observations of erosion in some sites in the Seychelles. Most importantly, it is estimated that the rise in energy reaching shores protected by fringing reefs will now accelerate more rapidly, such that the increase expected over the next decade will be approximately double than that seen over the past decade. (c) 2005 Elsevier Ltd. All rights reserved.