Kōkeʻe State Park
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Kōkeʻe State Park
Kōkee State Park is located in northwestern Kauai in the Hawaiian Islands. It includes the Kōkeʻe Museum at the marker on State Road 550, which focuses on the weather, vegetation, and bird life; a lodge which serves food and sells gifts; cabins for rent; and hiking trails. The park is just north of Waimea Canyon State Park at and includes of mountainous terrain. The main attractions of Kōkee State Park trails are the native vegetation, native forest birds, and the scenic cliffside views. Situated on a plateau between , much of Kōkee is a montane (infrequent frost) mesic forest ( annual rainfall with moist soil conditions) dominated by koa (''Acacia koa'') and ōhia lehua (''Metrosideros polymorpha'') trees. The park receives around of rain per year, mostly from October to May. At the end of the state road is a lookout onto the Kalalau Valley, once home to thousands of native Hawaiians. The valley was the backdrop for Jack London's short story ''Koolau the Leper''. In O ...
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Kalalau Valley
The Kalalau Valley is located on the northwest side of the island of Kauai in the state of Hawaii. The valley is located in the Nā Pali Coast State Park and houses the Kalalau Beach. The Nā Pali Coast is rugged and is inaccessible to automobiles. The only legal ways to access the valley are by kayak or by hiking the Kalalau Trail. The valley is surrounded by cliffs more than high. This valley's bottom is broad and relatively flat, with an accessible region about long and wide. The abundant sun and rain provides an ideal environment for flora and fauna. Many native Hawaiians lived in the valley into the 20th century, farming taro from a vast complex of terraced fields. Today, its designation as a state park forbids anyone from residing there. Access to Kalalau Valley Since the Nā Pali Coast is too steep for any motorized vehicles, all access to the valley is by boat or foot, except for emergency helicopter landings. Kayaks are a popular way of visiting the ...
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Canyon Trail Kauai
A canyon (from ; archaic British English spelling: ''cañon''), or gorge, is a deep cleft between escarpments or cliffs resulting from weathering and the erosive activity of a river over geologic time scales. Rivers have a natural tendency to cut through underlying surfaces, eventually wearing away rock layers as sediments are removed downstream. A river bed will gradually reach a baseline elevation, which is the same elevation as the body of water into which the river drains. The processes of weathering and erosion will form canyons when the river's headwaters and estuary are at significantly different elevations, particularly through regions where softer rock layers are intermingled with harder layers more resistant to weathering. A canyon may also refer to a rift between two mountain peaks, such as those in ranges including the Rocky Mountains, the Alps, the Himalayas or the Andes. Usually, a river or stream carves out such splits between mountains. Examples of mountain-type ...
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