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Prince Edward Island: Prince Edward Islands
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The yearly value of the Prince Edward Island fish catch in the early 1990s was some Can.$60 million, with lobster accounting for the majority of the total. Other sources of income were landings of cod, crab, blue-fin tuna, and redfish. Irish moss, an alga used in food processing, is harvested along the shoreline.
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The Prince Edward Island delegation's interest in Confederation quickly waned at Québec. The delegation suffered from infighting -- hardly surprising, considering the inter-party animosity existing between its members. Coles and Palmer, for instance, had once fought a duel with each other, and Colonel Gray had ousted Palmer from the premiership only the year before. There were ... problems with the agreement that was taking shape; the Island delegation protested the composition of the proposed union government. Perhaps most damaging, however, was the withdrawal of the offer to repurchase land from absentee landlords.
Uninhabited 5 x 10 km wide Prince Edward Island lies opposite Marion Island at the northern end of a submarine plateau on the Antarctic Plate immediately south of the SW Indian Ocean Ridge. The low-angle Prince Edward Island is a remnant of a large shield volcano formerly centered off the current NW shore of the island. Pleistocene and Holocene scoria cones and tuff cones are located throughout the unglaciated 672-m-high island, which was active contemporaneously with nearby Marion Island. Fifteen of the scoria cones and four tuff cones on the coastal plain were active during the Holocene.
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Long ago, Prince Edward Island was covered by a glacier, which left a deep mantle of sandy-red glacial debris. The soils that developed on this mantle are extremely moist, and soluble and valuable salts have been removed by the moisture. The soils are acidic and comparatively low in plant nutrients. However, over large sections where they have been cared for and where humus content has been added, the soils have proved excellent for agriculture.
Long ago, Prince Edward Island was buried under a thick glacier, which left a deep mantle of sandy-red glacial debris. The soils that developed on this mantle, known as podzals, are moist, acidic, and comparatively low in plant nutrients. However, over large sections where they have been cared for and where organic material has been added, the soils support many types of agriculture.
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One cannot drive through the rural districts of Prince Edward Island without seeing that, in spite of the propensity of some to a sea-going life, as a rule the Scotch make good farmers. Through sad experience have they bought their knowledge, for their hands were more accustomed to fishing-lines than to hoes. It is said of one Highland settlement that when the census was first taken there the returns showed twenty-nine bagpipes and five ploughs! To-day... there are no more flourishing farms to be seen than those of the western Highlanders. Snug houses and barns mark their settlements, and many of them hold high places of trust in their native colony. Strangers who visit Prince Edward Island on yachting excursions are struck by the fact that, in entering nearly every harbor, the most prominent object is always the Catholic church, keeping, as it were, the Ave Maris Stella in the hearts of this seafaring people.
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