From: owner-ammf-digest@smoe.org (alt.music.moxy-fruvous digest) To: ammf-digest@smoe.org Subject: alt.music.moxy-fruvous digest V14 #5374 Reply-To: ammf@fruvous.com Sender: owner-ammf-digest@smoe.org Errors-To: owner-ammf-digest@smoe.org Precedence: bulk alt.music.moxy-fruvous digest Saturday, November 28 2020 Volume 14 : Number 5374 Today's Subjects: ----------------- What IS Happening With This New Health Smartwatch That Is Such A Hit Among American Men? ["Now Popular in USA" Subject: What IS Happening With This New Health Smartwatch That Is Such A Hit Among American Men? What IS Happening With This New Health Smartwatch That Is Such A Hit Among American Men? http://sonicbreads.buzz/yQFebpC0EECxtBK1i8eHSiIbwvVZetPQrxjQgx5No0hSrJkF http://sonicbreads.buzz/PFVtKb1AAOSXOPbWFd1ZwadMVQQgnTkjPX6twoMq7_m62Vfn ountains, through valleys (depressions) or along plains, and can create canyons or gorges. The term upriver (or upstream) refers to the direction towards the source of the river, i.e. against the direction of flow. Likewise, the term downriver (or downstream) describes the direction towards the mouth of the river, in which the current flows. The term left bank refers to the left bank in the direction of flow, right bank to the right. The river channel typically contains a single stream of water, but some rivers flow as several interconnecting streams of water, producing a braided river. Extensive braided rivers are now found in only a few regions worldwide,[citation needed] such as the South Island of New Zealand. They also occur on peneplains and some of the larger river deltas. Anastamosing rivers are similar to braided rivers and are quite rare. They have multiple sinuous channels carrying large volumes of sediment. There are rare cases of river bifurcation in which a river divides and the resultant flows ending in different seas. An example is the bifurcation of Nerodime River in Kosovo. The River Cam from the Green Dragon Bridge, Cambridge (Britain) A river flowing in its channel is a source of energy which acts on the river channel to change its shape and form. In 1757, the German hydrologist Albert Brahms empirically observed that the submerged weight of objects that may be carried away by a river is proportional to the sixth power of the river flow speed. This formulation is also sometimes called Airy's law. Thus, if the speed of flow is doubled, the flow would dislodge objects with 64 times as much submerged weight. In mountainous torrential zones this can be seen as erosion channels through hard rocks and the creation of sands and gravels from the destruction of larger rocks. A river valley that was created from a U-shaped glaciated valley, can often easily be identified by the V-shaped channel that it has carved. In the middle reaches where a river flows over flatter land, meanders may form through erosion of the river banks and deposition on the inside of bends. Sometimes the river will cut off a loop, shortening the channel and forming an oxbo ------------------------------ End of alt.music.moxy-fruvous digest V14 #5374 **********************************************