could someone please tell me what an old sand wedge was called?
968230
Was called a niblick\n\nGene Sarazen, striker of the shot heard 'round the world in the '35 Masters, invented the sandwedge in 1930. He called it the sand iron. Initially, he added lead to the bottom edge of a wedge to keep it from digging into the sand. The sandwedge is not old enough to have a name like niblick.\n\nIn the niblick days, early 1800s, golfers used various clubs in order to escape the sand. Some of them had concave faces so they were called spoons. They were banned by the USGA. The term spoon was also applied to what would now be called a 2 Wood. \n\nA ball mark on the green is also referred to as a pitch mark.
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Depends on the beach\nSouth beach those weird soft shoes\nDaytona Flip flops \nJacksonville soft shoes\n Panama bare feet\n Fort Myers bare feet \nTampa soft shoes \n\neach has different kind of sand
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EBAY: UNDER INDIAN ARTIFACTS 1940 TO PRESENT IF LOOKING FOR ATLATI DART THROWING STICK\n\nhttp://cgi.ebay.com/MAPLE-BLACK-WALNUT-WOOD-ATLATL_W0QQitemZ7772459198QQihZ018QQcategoryZ4714QQssPageNameZWDVWQQrdZ1QQcmdZViewItem\nitem # ebay  7772459198
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It is called the footspot.  It is the center of the footstring, the imaginary line accross the table at the second diamond from the rack end of the table.  The footspot is where the first ball in the rack is placed.\n\nJust fyi, at the other end of the table that line is called the headstring.  This is accross the breaking end of the table from second diamond.  The area inside that line is commonly called "the kitchen".
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There are someting called "Ashinaka" which translated would mean "the middle of the foot."  These were typically made of straw and would only cover the middle portion of the sole with the heels and toes protruding from the front and back.  They were worn to give better traction and gripping power.\n\nBTW...the link works if you take away the last three dots.
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You may be able to find it on one of the posts at the blog called Demolition, Scrap Metal and Salvage News http://www.demolition1.blogspot.com
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It's called a pantheon.  There's an old one in Rome.
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An extinct concept. It was last seen in the 1950's.
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Lattis, or Lattice. I'm not sure of the spelling.
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A sand wedge will commonly have 56 degrees of loft, sometimes 58, but 56 is pretty standard.\n\nA PW loft will likely range from 48 to 52 degrees, depending on how "modern" the lofts are.  If you have an older PW, it might well be 52 degrees; otherwise, i'd bet on 48 or so.\n\nWhy the difference?  Recently, manufacturers, in their quest to have the "longest clubs," strengthened the lofts.  Whereas a PW used to be 52 (or maybe 50, depending), now they tend to be around 48.  And the same goes for all the other clubs in a set--they're stronger lofts.\n\nThe net effect is to leave you a very large gap between your PW and your SW.  As from above, perhaps 8 degrees, which means there are distances in between that require you to hit a partial PW, something many find difficult to do consistently.\n\nTo make up for this, manufacturers have filled the gap between the PW and SW by producing what are called "Gap" wedges--they'll have an A or G on them (A meaning Approach wedge, G meaning Gap wedge).  Guess what loft these are?  Answer:  The same as the old PW!\n\nThose crazy manufacturers!  Leave it to them to create a problem, then sell you something to solve it.\n\nMike (The Club Doctor).
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Sand Castle Central - Sand Sculpture Tips, Tricks and PicsSand sculpture tips and tricks, an updated contest schedule and links to master sculptor sites and other related pages.\nwww.sandcastlecentral.com/ -
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A link:\n\nhttp://www.palaeos.com/Palaeo/lagerstatten.html
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It's called Blazon Gap. It's a natural feature. The ridge is Oyster Ridge.
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I always check wikipedia for stuff like that.  Maybe not the best source.  Its in the link below
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On the  bare earth....they used to be called earth-runners,you see.\nBefore cobbled roads became the vogue -then they were cobble-runners.\nBut nowadays,only tarred roads that stretch for miles will do,thank you very much.
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It's called a Mahogany Calabash.\n\nHope this helps!\n\nAngel
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Is this a question?  I was confused by the lack of a complete sentince.  \n\nHowever, if the strata are flat, there is no special name for it.  It's just a bedding layer.  It's measured by the strike (horizontal direction) and the dip (amount it's sloping down).  If it folds and the youngest material is on the inside, it's a syncline (v shaped), but if the youngest material is on the outside, it's an anticline (A shaped)  Then, if the fold is not level, it's called a plunging anticline/syncline.