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Wandoo National Park. / 32.067°S 116.517°E / -32.067; 116.517. Wandoo National Park is a national park in Western Australia, 80 km east of Perth. [2] It was established in 2004, and has an area of 463.68 km 2. [1]
The park is composed of typical Darling Scarp woodland including species of marri, jarrah and wandoo with a diverse understorey including a range of wildflowers. [2]Piesse Brook flows through the park before joining the Helena River, making the park and important catchment area for both the Helena and the Swan Rivers.
Eucalyptus wandoo, commonly known as wandoo, dooto, warrnt or wornt [5] and sometimes as white gum, [6] [7] is a small to medium-sized tree that is endemic to the southwest of Western Australia. [8] It has smooth bark, lance-shaped adult leaves, flower buds in groups of nine to seventeen, white flowers and conical to cylindrical fruit.
Eucalyptus accedens, commonly known as smooth bark wandoo or powderbark wandoo is a species of tree endemic to the south-west of Western Australia. Although the common names suggest it is similar to wandoo, ( Eucalyptus wandoo ), the two species are very different botanically. The bark of E. accedens has talc-like powder, at least on the ...
Jarrah Forest, also known as the Southwest Australia woodlands, is an interim Australian bioregion and ecoregion located in the south west of Western Australia. [2] [3] The name of the bioregion refers to the region's dominant plant community, jarrah forest – a tall, open forest in which the dominant overstory tree is jarrah (Eucalyptus marginata).
Mount St. Helens National Volcanic Monument is a U.S. National Monument that includes the area around Mount St. Helens in Cowlitz and Skamania Counties, Washington. It was established on August 27, 1982, by U.S. President Ronald Reagan, following the 1980 eruption. [2] The 110,000 acre (445 km 2) National Volcanic Monument was set aside for ...
Like other mountains in Glacier National Park, Reynolds Mountain is composed of sedimentary rock laid down during the Precambrian to Jurassic periods. Formed in shallow seas, this sedimentary rock was initially uplifted beginning 170 million years ago when the Lewis Overthrust fault pushed an enormous slab of precambrian rocks 3 mi (4.8 km) thick, 50 miles (80 km) wide and 160 miles (260 km ...
At 2,501.9 metres (8,208 ft) above sea level, Säntis is the highest mountain in the Alpstein massif of northeastern Switzerland. It is also the culminating point of the whole Appenzell Alps, between Lake Walen and Lake Constance. Shared by three cantons, the mountain is a highly visible landmark thanks to its exposed northerly position within ...