Little Mashel River Waterfalls
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Little Mashel River Waterfalls
The Little Mashel River Waterfalls are the 3 waterfalls contained within the gorge of the Little Mashel River, not far above its confluence with the Mashel River. Tom Tom Falls Tom Tom Falls, at , also known as Upper Little Mashel Falls, is the first major waterfall in the main gorge of the Little Mashel River. The river flows over an old dam, an artifact of an old millpond, before narrowing and plunging about 25 feet over a cliff into a pool below. The falls are only 5 feet wide, so they are quite powerful. In high water, a small portion of the river completely bypasses the falls and its cliff, forming a series of cascades and ending at the river roughly downstream. Little Mashel Falls Little Mashel Falls, at , is the largest of the 3 falls along the Little Mashel and is located between Tom Tom Falls and Lower Little Mashel Falls. Little Mashel Falls occurs where the river slides down roughly into a congregation of boulders. In spring when the river is high, the ...
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Little Mashel River
The Little Mashel River is a river in Pierce County, Washington. It is a tributary of the Mashel River, and enters the Mashel just downstream from the Eatonville, Washington, city limits. It is noted for its canyon and the three waterfalls. Course The Little Mashel begins in a small, unnamed lake located about southeast of Eatonville, Washington. Upon exiting the lake, the river, very small at this point, flows northeast for about before turning northwest for about , merging with South Fork Little Mashel River about along the way. There, the river briefly turns southwest, picks up the waters of its only named tributary, Midway Creek, and then turns northwest again. It flows that way for another or so until its confluence with the Mashel. A short canyon that sees the river drop over three large, often visited waterfalls lies about above its mouth. South Fork The South Fork Little Mashel River begins about west of the lake the main fork begins in and flows northwest f ...
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Mashel River
The Mashel River is a river in Pierce County, in the U.S. state of Washington. It is a tributary of the Nisqually River, which it enters about southwest of Eatonville, at Nisqually river mile 39.6. Course The Mashel River’s headwaters are a tiny, unnamed lake about southeast of Mount Beljica. The river starts off as a small stream flowing northwest before turning west then south, where the South Fork Mashel River joins, after which the Mashel turns west. The Mashel River is joined by Busy Wild Creek and then, about 3.5 miles downstream, Beaver Creek. The Mashel continues west for about 2.7 miles then turns southwest, along the southern city limits of Eatonville, which it follows for about 1.7 miles. The river is joined by the Little Mashel River a mere after leaving Eatonville’s city limits. George Smallwood Park, named for one of the former mayors of Eatonville, is located about 0.8 miles above the Little Mashel River confluence. After the Little Mashel confluence ...
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Eatonville, Washington
Eatonville is a town in Pierce County, Washington, United States. It is south of Tacoma. The population was 2,845 at the 2020 census. The town motto is "Better Together". History For centuries, Nisqually people roamed the rivers and streams of the Eatonville area. Leschi, one of the main leaders of Nisqually was born in this area in 1808. In 1889, Indian Henry was one of the Nisqually who guided the town's Euro-American founder, Thomas C. Van Eaton, from Mashell Prairie to the present site of Eatonville. Legend has it that upon arrival Henry declared, "This is a good place. Not much snow." Area white settlers and the accompanying Nisqually were in need of goods, which "T.C." provided at his trading post. Supplies were carried by his stage from Spanaway over a rough trail through dense forest. In 1891, the settlers built the town's first school, which is still in use. For years Eatonville was a waypoint for visitors to Mount Rainier. In 1902, the Tacoma Eastern Railroad a ...
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Millpond
A mill pond (or millpond) is a body of water used as a reservoir for a water-powered mill. Description Mill ponds were often created through the construction of a mill dam or weir (and mill stream) across a waterway. In many places, the common proper name Mill Pond has remained even though the mill has long since gone. It may be fed by a man-made stream, known by several terms including leat and'' mill stream.'' The channel or stream leading from the mill pond is the mill race, which together with weirs, dams, channels and the terrain establishing the mill pond, delivers water to the mill wheel to convert potential and/or kinetic energy of the water to mechanical energy by rotating the mill wheel. The production of mechanical power is the purpose of this civil engineering hydraulic system. The term mill pond is often used colloquially and in literature to refer to a very flat body of water. Witnesses of the loss of RMS Titanic RMS ''Titanic'' was a British passenge ...
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Tannic Acid
Tannic acid is a specific form of tannin, a type of polyphenol. Its weak acidity ( pKa around 6) is due to the numerous phenol groups in the structure. The chemical formula for commercial tannic acid is often given as C76H52O46, which corresponds with decagalloyl glucose, but in fact it is a mixture of polygalloyl glucoses or polygalloyl quinic acid esters with the number of galloyl moieties per molecule ranging from 2 up to 12 depending on the plant source used to extract the tannic acid. Commercial tannic acid is usually extracted from any of the following plant parts: Tara pods (''Caesalpinia spinosa''), gallnuts from '' Rhus semialata'' or ''Quercus infectoria'' or Sicilian sumac leaves (''Rhus coriaria''). According to the definitions provided in external references such as international pharmacopoeia, Food Chemicals Codex and FAO-WHO tannic acid monograph only tannins obtained from the above-mentioned plants can be considered as tannic acid. Sometimes extracts from chestnu ...
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Waterfalls Of Pierce County, Washington
A waterfall is a point in a river or stream where water flows over a vertical drop or a series of steep drops. Waterfalls also occur where meltwater drops over the edge of a tabular iceberg or ice shelf. Waterfalls can be formed in several ways, but the most common method of formation is that a river courses over a top layer of resistant bedrock before falling on to softer rock, which erodes faster, leading to an increasingly high fall. Waterfalls have been studied for their impact on species living in and around them. Humans have had a distinct relationship with waterfalls for years, travelling to see them, exploring and naming them. They can present formidable barriers to navigation along rivers. Waterfalls are religious sites in many cultures. Since the 18th century they have received increased attention as tourist destinations, sources of hydropower, andparticularly since the mid-20th centuryas subjects of research. Definition and terminology A waterfall is general ...
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