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Dunedin: buildings and boats VII. Dunedin to Bluff III. Bluff IV. Foveaux Strait V. More Stewart Island photos X. Milford Road: History V. Milford Road: Glory VI. Fox Glacier IV. Glacial Plant Colonisers V. Fox Rain Forest VI. Glacier People IX.

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Gold Town: Hokitika V. New Zealand Beeches IV. Rata and Kamahi V. Pohutukawa Birds and Mammals 11 pages II. Royal Albatross III. Fur Seals IV. Sea Lions V. Buller's Mollymawk VI. Penguins VII.

Geological History of Cape Town - Geology of Cape Town

Shags VIII. Kaka IX. Weka X. Kea XI. Spoonbills XII. Early days: from wool to refrigeration III. Nauru: the phosphate grab IV. Rogering the farmer V. White Gold: the dairy bonanza VI.

Environmental costs VII. The Cape of Good Hope V. Table Mountain IV.

DAY 1: Salt Lake City

The Rhodes Memorial V. Irma Stern Gallery VI. Tamboerskloof VII. Bain's Kloof Pass IX. Cape Peninsula: Geology IV. Cape Peninsula: Flora V. Bontebok National Park VI. Montagu Gorge VII. Constantia III.


Urban Geology

Breede River IV. Labour conditions in the wine and fruit industry V. Fair trade and the wine and fruit trade VI. Land Reform VII. Paper: Not so lucky Laiki II. Notes: Laiki timeline: IV.. The Bailout - Summary V. Background VI. Economic Crisis VII. Russian Connections X. Back in Brussels XI. Germany XII. Bank bailout conclusions XV. Political Fallout XVI. Memorandum XXI. The money laundering audits XXII. De Facto Partition II. Dislocation and displacement III. Water resources V.

Biodiversity challenges VI. Seismic Activity VII.

Western Patagonia; A Grand Geological adventure.

The contemporary church VIII. Neolithic to Roman III. The Cult of Aphrodite IV. Byzantium: Introduction VI. Carob: the Locust Bean IX. Locusts: gone but not forgotten?

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British Rule XI. Oregon can be divided into the following nine geologic provinces, each with outstanding geologic scenery. The heavily vegetated, elongated Coast Range province has a varied geologic history. Its basement was formed by a volcanic island chain that collided with North America about 50 million years ago. This province consists of four north-south-trending belts of metamorphic and igneous rocks that formed in an oceanic setting and subsequently collided with the North American continent about million years ago.

Complexly folded and faulted rocks are bounded by belts of sparsely vegetated bands of serpentinite.

Oregon Caves National Monument lies within an enormous fault-bounded block of marble. Between 14 and 16 million years ago, "fissure" volcanic eruptions in eastern Washington, eastern Oregon, and western Idaho produced enormous volumes of molten Columbia River basalt that flowed like water west into the Deschutes-Columbia Plateau province in eastern Washington and northeastern Oregon, with some lava continuing to flow as far west as the Pacific Ocean via the ancestral Columbia River valley.

As the basalt cooled and congealed, it formed the columnar cliffs that dominate the landscape today. The sediments collected into this basin record multiple Ice Age floods that originated in Montana, poured through the Cascades via the Columbia River , and backed up in the valley before eventually draining to the Pacific Ocean.. This area is made up of separate "exotic terranes," areas that were created elsewhere and scooped up by North America as it moved west toward the Pacific. Fossils found in this province reveal their foreign origins. Placer and lode gold mines were active here in the past, and towns such as John Day and Baker City, together with the Sumpter gold dredge, are vivid reminders of the Blue Mountains gold mining heritage.

Both lie in a region that has been stretched, or extended, almost percent from its original width in the last 10 million years. Evidences of this extension are massive fault block mountains such as Steens and Hart Mountains, with intervening basins containing such features as the Alvord Desert and Lake Abert. Intense volcanic and hot spring activity over millions of years has produced fine-grained gold deposits and jasperoids that are prized by rock hounds.