From: owner-ammf-digest@smoe.org (alt.music.moxy-fruvous digest) To: ammf-digest@smoe.org Subject: alt.music.moxy-fruvous digest V14 #5376 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 5376 Today's Subjects: ----------------- Shocking Video: The Dirty Little Fish Oil Secret (and more) ["Doctor Walt] ---------------------------------------------------------------------- Date: Sat, 28 Nov 2020 07:21:53 -0500 From: "Doctor Walters - PhysioTru" Subject: Shocking Video: The Dirty Little Fish Oil Secret (and more) Shocking Video: The Dirty Little Fish Oil Secret (and more) http://hotground.buzz/FbVkobX7kCJr3xvhWztRAIunLGGWBbVJrtAmOsEoa-UF1Mm1 http://hotground.buzz/i4QFg-mPImtilK-OjfDwMwPXPrJIzyuDtIj2T0eUFSCnJ6KI ers can generally be classified as either alluvial, bedrock, or some mix of the two. Alluvial rivers have channels and floodplains that are self-formed in unconsolidated or weakly consolidated sediments. They erode their banks and deposit material on bars and their floodplains. Bedrock rivers form when the river downcuts through the modern sediments and into the underlying bedrock. This occurs in regions that have experienced some kind of uplift (thereby steepening river gradients) or in which a particular hard lithology causes a river to have a steepened reach that has not been covered in modern alluvium. Bedrock rivers very often contain alluvium on their beds; this material is important in eroding and sculpting the channel. Rivers that go through patches of bedrock and patches of deep alluvial cover are classified as mixed bedrock-alluvial. Alluvial rivers can be further classified by their channel pattern as meandering, braided, wandering, anastomose, or straight. The morphology of an alluvial river reach is controlled by a combination of sediment supply, substrate composition, discharge, vegetation, and bed aggradation. At the start of the 20th century William Morris Davis devised the "cycle of erosion" method of classifying rivers based on their "age". Although Davis's system is still found in many books today, after the 1950s and 1960s it became increasingly criticized and rejected by geomorphologists. His scheme did not produce testable hypotheses and was therefore deemed non-scientific. Examples of Davis's river "ages" include: Youthful river: A river with a steep gradient that has very few tributaries and flows quickly. Its channel ------------------------------ End of alt.music.moxy-fruvous digest V14 #5376 **********************************************