CHESMAYNE
Midi: Across
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Coordinates

The coordinates of a chess MP/mp with respect to,
01 The XY
axis.
02 The acentric
notation (B$A, B,
C, D etc) or, the centric notation.
03 Co-ordinate Notation: a notation in which each
cell has its own unique location and identified by its cell
co-ordinates. The ‘Chesmayne Notation’ is an example of such a
notation. ‘Standard Notation’ and
‘Continental Notation’ are other examples.
There are two versions: full notation, and abbreviated (the departure
cell is given only when necessary) ie,
01A XY Standard Notation: 01A PA5-$E02/E04 -
01B KT2-$B08/C06
01B XY Abbreviated Notation: 01A PA5-E04
- 01B KT2-C06
02A Centric Notation: 01A PA5-C04/A02
- 01B KT2-D21/B10
02B Abbreviated Centric: 01A PA5-A02
- 01B KT2-B10
03A Algebraic Notation: 1 e2-e4 -
N-b8-c6
03B Abbreviated Algebraic: 1 e4
- Nc6
Unique cell
identifiers, made up of a number indicating the rank and a letter
indicating the file.
Russian Cyrillic (Russian
players also use Latin for recording the moves of a game), German and English
have differing ways of representing the moves of the MPs/mps ie,
04A Russian: 1 Cf1:c4 (C = Bishop)
04B Abbreviated Russian: 1 C:c4 (colon indicates capture)
05A German: 1 Lf1-c4 (L = Bishop)
05B Abbreviated German: 1 Lc4
06A English: 1 Bf1xc4 (B = Bishop)
06B Abbreviated English: 1 Bxc4 (x indicates capture)
07A XY Standard Notation: 01A BS2-$F01*C04-PA6
07B XY Abbreviated Notation: 01A BS2*C04 (asterisk indicates capture)
08A Acentric Notation: 01A BS2-D06*B12-PA6
08B Abbreviated Acentric: 01A BS2*B12 (asterisk indicates capture)
In the Algebraic Notation the departure cell is only
given if two MPs/mps of the same type could move to the arrival cell (this
occurs quite often with the KTs, KT1 and KT2 or, RO1
and RO2). In the ‘Centric Notation’
and the XY Notation this anomaly does not arise as each MP/mp is identified by
a number ie, PA1, PA2, PA3, KT1, KT2, BS1, BS2, QU1, QU2 etc.
Astronomers
use co-ordinates corresponding to longitude and latitude on the Earth to locate
astronomical objects. These
co-ordinates relate to the positions of stars instead of
points on our Earth’s surface. The
equivalent of latitude is called declination and is measured, like latitude,
from the equator (0 degrees) north and south to the poles (+ or - 90
degrees). An observer on the Earth’s
equator would see a star with 0 degrees declination pass directly overhead
while one with a declination of +90 degrees would lie due north on the
horizon. At the latitude of the
‘Oirish/British Islands’, say 52 degrees north, an object with a declination of
+52 degrees would pass overhead, and the north pole of the sky is raised to 52
degrees above your northern horizon.