Souvenir Book of Bar Harbor, Me.

Colored, postcard-like images in a souvenir booklet showing scenes around Bar Harbor, Maine, published between 1915 and 1925. Images include the Village Green, Thunder Cave, Duck Brook, Frenchman\u27s Bay, Newport Mountain from Gorge Road, Bar Harbor High School, Balance Rock, Main Street, Shore Path, Bar Harbor from Rodick Island, the Post Office, Jesup Memorial Library and Y.W.C.A., Kebo Street, Profile Rock and a horse drawn buggy driving past Otter Cliff

Wave transformation across a macrotidal shore platform under low to moderate energy conditions

We investigate how waves are transformed across a shore platform as this is a central question in rock coast geomorphology. We present results from deployment of three pressure transducers over four days, across a sloping, wide (~200 m) cliff-backed shore platform in a macrotidal setting, in South Wales, United Kingdom. Cross shore variations in wave heights were evident under the predominantly low to moderate (significant wave height < 1.4 m) energy conditions measured. At the outer transducer 50 m from the seaward edge of the platform (163 m from the cliff) high tide water depths were 8+ m meaning that waves crossed the shore platform without breaking. At the mid platform position water depth was 5 m. Water depth at the inner transducer (6 m from the cliff platform junction) at high tide was 1.4 m. This shallow water depth forced wave breaking, thereby limiting wave heights on the inner platform. Maximum wave height at the middle and inner transducers were 2.41 and 2.39 m respectively and significant wave height 1.35 m and 1.34 m respectively. Inner platform high tide wave heights were generally larger where energy was up to 335% greater than near the seaward edge where waves were smaller. Infragravity energy was less than 13% of the total energy spectra with energy in the swell, wind and capillary frequencies accounting for 87% of the total energy. Wave transformation is thus spatially variable and is strongly modulated by platform elevation and the tidal range. While shore platforms in microtidal environments have been shown to be highly dissipative, in this macro-tidal setting up to 90% of the offshore wave energy reached the landward cliff at high tide, so that the shore platform cliff is much more reflective

The role of mass-movement in shore platform development along the Gisborne coastline, New Zealand

Tidal shore platforms form a conspicuous part of the coastal scenery north of Gisborne, New Zealand. Some of these platforms are being extended landward under present-day conditions. Present widening results primarily from cliff-retreat by mass-movement. The coincidence in distribution of areas of wave convergence, mass-movement and shore platforms suggests a genetic connection between these marine and subaerial process and response elements. Various types of mass-movement are involved in cliff-retreat, notably slumps, flows, debris slides and soil and rock falls. While the products of such mass-movement forms are removed by wave action, extensive boulder fields on some shore platforms indicate that removal is not always complete. Not all of the shore platforms on this coast are being widened at present. Widening has ceased where active mass-movement is not occurring

Ice Age Elephants of the Channel Islands

Of the small company of land mammals native to the Channel Islands of Southern California none reaches large size, and, if we exclude aboriginal man and his dog, the largest is the fox. This interesting creature, once more numerous than it now is, exists under a variety of conditions on the several islands and may be seen occasionally searching for food along the seashore or living in cactus patches, brushy ravines, and on the open slopes of hills to an elevation of more than 2,000 feet. It seems to lead at present a solitary life. The island species was long ago recognized by biologists as a distinctive type, related to the mainland gray fox rather than to the kit fox and red fox. Six races have now been identified, one for each of the principal islands comprising the Channel Island group

Pyroclastic deposits and volcanic history of Mayor Island

The emergent summit of Mayor Island, Bay of Plenty, New Zealand, is a peralkaline rhyolite volcano constructed by: a sequence of lava flows, the Tutaretare Rhyolite Formation new; and pyroclastic deposits, the Oira Pyroclastite Formition (new). These 2 formations constitute the Mayor Island Group new. The pyroclastic deposits mantle most of the outer slopes of the island, in places exceeding 100 m in thickness, and also occur interbedded with lava flows of the main cone. The pyroclastics have been informally assigned on the basis of their compositional, welding and textural, and sedimentary structural characteristics to one or other of 15 lithotypes which may be related to particular modes of eruption and emplacement, of both airfall (phreatic, phreatomagmatic, phreatoplinian, and plinian types) and pyroclastic flow (ignimbrite, nuée ardente, and base surge types origins). A sixteenth lithotype comprises epiclastic deposits formed possibly by catastrophic overspill from an ancestral crater lake. Two new radiocarbon dates on logs from the pyroclastic deposits are recorded: (Wk105) 8000 ± 70 years B.P., and (Wk77) 6340 ± 190 years B.P. Recognition of the calcalkaline Rotoehu and possibly Rotoma Ashes on Mayor Island, together with the new radiocarbon dates, enables definition of 8 phases of major volcanic activity, each separated by relatively quiescent periods with erosion and paleosol formation. Volcanism commenced sometime prior to 42 000 years ago and has continued intermittently up to the eruption of the young dome lavas, possibly less than 1000 years ago. At present, only I Mayor Island-derived tephra has been identified on the mainland of the North Island, namely the Tuhua Tephra dated (Wk77) at source as 6340 ± 190 years B .P. However, the character and magnitude of several of the pyroclastic units on Mayor Island is such that recognition of other peralkaline tephras is anticipated in northern North Island

Volume 25, Number 1 - February 1947

Volume 25, Number 1 – February 1947. 58 pages including covers and advertisements. Editorial Doherty, R.E. The Beast O\u27Brien, John J. On Coffee Eagle, George L. A Stranger in Strasbourg Shanley, Joseph V. Reflections Doherty, R.E. Thoughts on New York Gnys, Edward L. Chaos Morrison, Coleman On Floorwalkers Eagle, George L. Moment of Vision Deasy, John Living History Fortin, Andrew G. Effects of Studying the Essayists Critiqu

Wisconsin Great Lakes Restoration Projects: Producing Results for People, Communities

This report provides updates on 12 Great Lakes restoration projects occurring in Wisconsin