Friday, April28, 2017 L-36.com

Decimal Equivalent Fractions



FRACTIONAL INCHES
DECIMAL
INCHES
FRACTIONAL INCHES
DECIMAL
INCHES

 

1/64
............................
.015625
1/32
................
.03125
3/64
............................
.046875
1/16..........
.0625
5/64
............................
.078125
3/32
................
.09375
7/64
............................
.109375
1/8...........
.125
9/64
............................
.140625
5/32
................
.15625
11/64
............................
.171825
3/16..........
.1875
13/64
............................
.203125
7/32
................
.21875
15/64
............................
.234375
1/4...........
.250
17/64
............................
.265625
9/32
................
.28125
19/64
............................
.296875
5/16...........
.3125
21/64
............................
.328125
11/32
................
.34375
23/64
.359375
3/8...........
.375
25/64
............................
.390625
13/32
................
.40625
27/64
............................
.421875
7/16..........
.4375
29/64
............................
.453125
15/32
................
.46875
31/64
............................
.484375
1/2...........
.500

 

33/64
.............................
.515625
17/32
.................. .53125
35/64
.............................
.546875
  9/16........... .5625
37/64
.............................
.578125
19/32
.................. .59375
39/64
.............................
.609375
  5/8............. .625
41/64
.............................
.640625
21/32
.................. .65625
43/64
.............................
.671875
  11/16.......... .6875
45/64
.............................
.703125
23/32
.................. .71875
47/64
.............................
.734375
  3/4............. .750
49/64
.............................
.765625
25/32
.................. .78125
51/64
.............................
.796875
  13/16.......... .8125
53/64
.............................
.828125
27/32
.................. .84375
55/64
.............................
.859375
  7/8............. .8750
57/64
.............................
.890625
29/32
.................. .90625
59/64
.............................
.921875
  15/16.......... .9375
61/64
.............................
.953125
31/32
.................. .96875
63/64
.............................
.984375
1................ 1.0000

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Disclaimer:
The information on this web site has not been checked for accuracy. It is for entertainment purposes only and should be independently verified before using for any other reason. There are five sources. 1) Documents and manuals from a variety of sources. These have not been checked for accuracy and in many cases have not even been read by anyone associated with L-36.com. I have no idea of they are useful or accurate, I leave that to the reader. 2) Articles others have written and submitted. If you have questions on these, please contact the author. 3) Articles that represent my personal opinions. These are intended to promote thought and for entertainment. These are not intended to be fact, they are my opinions. 4) Small programs that generate result presented on a web page. Like any computer program, these may and in some cases do have errors. Almost all of these also make simplifying assumptions so they are not totally accurate even if there are no errors. Please verify all results. 5) Weather information is from numerious of sources and is presented automatically. It is not checked for accuracy either by anyone at L-36.com or by the source which is typically the US Government. See the NOAA web site for their disclaimer. Finally, tide and current data on this site is from 2007 and 2008 data bases, which may contain even older data. Changes in harbors due to building or dredging change tides and currents and for that reason many of the locations presented are no longer supported by newer data bases. For example, there is very little tidal current data in newer data bases so current data is likely wrong to some extent. This data is NOT FOR NAVIGATION. See the XTide disclaimer for details. In addition, tide and current are influenced by storms, river flow, and other factors beyond the ability of any predictive program.