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Meanders are a result of the interaction of water flowing through a curved channel with the underlying river bed. Governing physics Straight channel culminating in a single bend Its modern Turkish name is the Büyük Menderes River. It flows through series of three graben in the Menderes Massif, but has a flood plain much wider than the meander zone in its lower reach. The Meander River is south of Izmir, east of the ancient Greek town of Miletus, now Milet, Turkey. Strabo said: ‘.its course is so exceedingly winding that everything winding is called meandering.’ As a result, even in Classical Greece (and in later Greek thought) the name of the river had become a common noun meaning anything convoluted and winding, such as decorative patterns or speech and ideas, as well as the geomorphological feature. The term derives from the winding river Menderes located in Asia-Minor and known to the Ancient Greeks as Μαίανδρος Maiandros ( Latin: Maeander), characterised by a very convoluted path along the lower reach. Streams or rivers with a single channel and sinuosities of 1.5 or more are defined as meandering streams or rivers. The sinuosity of a watercourse is the ratio of the length of the channel to the straight line down-valley distance. The degree of meandering of the channel of a river, stream, or other watercourse is measured by its sinuosity. Over time, meanders migrate downstream, sometimes in such a short time as to create civil engineering challenges for local municipalities attempting to maintain stable roads and bridges. It typically ranges from 15 to 18 times the width of the channel. The zone within which a meandering stream periodically shifts its channel is known as a meander belt. The result of this coupled erosion and sedimentation is the formation of a sinuous course as the channel migrates back and forth across the axis of a floodplain. It is produced as a watercourse erodes the sediments of an outer, concave bank ( cut bank or river cliff) and deposits sediments on an inner, convex bank which is typically a point bar. Meanders of the Rio Cauto at Guamo Embarcadero, Cuba The Jordan River, near the Dead Sea, 1937Ī meander is one of a series of regular sinuous curves in the channel of a river or other watercourse. Meanders develop, which lengthen the course of the stream, decreasing the gradient. The maximum gradient is along the down-valley axis represented by a hypothetical straight coast channel.
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We can re-size patterns to perfectly complement YOUR quilt.ĬLICK HERE* to download a pdf file with a more complete list and larger images of the patterns.For other uses, see Meander (disambiguation). Many designers have patterns available in both digital and paper format. Keep in mind that we use a computer so the patterns that use are digital and not printed on paper. We probably already have it or will be happy to try and locate it. If you don't see what you are looking for, or have seen a pattern that you like somewhere else, just let us know. Here is a sampling of the hundreds of pantographs that we have available to quilt your quilt top. I have hundreds of patterns in my library to choose from. Some of the more poplular patterns are shown below. You choose the design, or let me choose for you.
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It consists of a repeating design over the entire quilt top, from one edge to the other. The edge to edge style of quilting is very popular and very cost effective. The higher the density of the quilting, the higher the cost for quilting. Our pricing for Pantographs are based on three levels of density. Pantographs are patterns that are quilted from the left edge of the quilt to the right edge and the quilting is completed irregardless of the pattern of the quilt top.
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Pantographs (or Edge to Edge) Quilting Patterns