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Section: 060.0451 Missouri coordinate system zones precisely defined. RSMO 60.451


Published: 2015

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Missouri Revised Statutes













Chapter 60

County Surveyors and Land Surveys

←60.441

Section 60.451.1

60.461→

August 28, 2015

Missouri coordinate system zones precisely defined.

60.451. 1. For the purpose of more precisely defining the Missouri

coordinate system of 1927, the following definition by the United States

Coast and Geodetic Survey is adopted:



(1) The Missouri coordinate system of 1927, east zone, is a

transverse Mercator projection of the Clarke spheroid of 1866, having a

central meridian 90 degrees -- 30 minutes west of Greenwich, on which

meridian the scale is set at one part in fifteen thousand too small. The

origin of coordinates is at the intersection of the meridian 90 degrees --

30 minutes west of Greenwich and the parallel 35 degrees -- 50 minutes

north latitude. This origin is given the coordinates: x = 500,000 feet

and y = 0 feet;



(2) The Missouri coordinate system of 1927, central zone, is a

transverse Mercator projection of the Clarke spheroid of 1866, having a

central meridian 92 degrees -- 30 minutes west of Greenwich, on which

meridian the scale is set at one part in fifteen thousand too small. The

origin of coordinates is at the intersection of the meridian 92 degrees --

30 minutes west of Greenwich and the parallel of 35 degrees -- 50 minutes

north latitude. This origin is given the coordinates: x = 500,000 feet

and y = 0 feet;



(3) The Missouri coordinate system of 1927, west zone, is a

transverse Mercator projection of the Clarke spheroid of 1866, having a

central meridian 94 degrees -- 30 minutes west of Greenwich, on which

meridian the scale is set at one part in seventeen thousand too small. The

origin of coordinates is at the intersection of the meridian 94 degrees --

30 minutes west of Greenwich and the parallel 36 degrees -- 10 minutes

north latitude. This origin is given the coordinates: x = 500,000 feet

and y = 0 feet.



2. For purposes of more precisely defining the Missouri coordinate

system of 1983, the following definition by the National Ocean

Survey/National Geodetic Survey is adopted:



(1) The Missouri coordinate system 1983, east zone, is a transverse

Mercator projection of the North American Datum of 1983 having a central

meridian 90 degrees -- 30 minutes west of Greenwich, on which meridian the

scale is set at one part in fifteen thousand too small. The origin of

coordinates is at the intersection of the meridian 90 degrees -- 30 minutes

west of Greenwich and the parallel 35 degrees -- 50 minutes north latitude.

This origin is given the coordinates: x = 250,000 meters and y = 0 meters;



(2) The Missouri coordinate system 1983, central zone, is a

transverse Mercator projection of the North American Datum of 1983 having a

central meridian 92 degrees -- 30 minutes west of Greenwich, on which

meridian the scale is set at one part in fifteen thousand too small. The

origin of coordinates is at the intersection of the meridian 92 degrees --

30 minutes west of Greenwich and the parallel of 35 degrees -- 50 minutes

north latitude. This origin is given the coordinates: x = 500,000 meters

and y = 0 meters;



(3) The Missouri coordinate system 1983, west zone, is a transverse

Mercator projection of the North American Datum of 1983 having a central

meridian 94 degrees -- 30 minutes west of Greenwich, on which meridian the

scale is set at one part in seventeen thousand too small. The origin of

coordinates is at the intersection of the meridian 94 degrees -- 30 minutes

west of Greenwich and the parallel 36 degrees -- 10 minutes north latitude.

This origin is given the coordinates: x = 850,000 meters and y = 0 meters.



3. The position of either Missouri coordinate system shall be as

marked on the ground by horizontal control stations established in

conformity with the standards adopted by the department of agriculture for

first-order and second-order work, whose geodetic positions have been

rigidly adjusted on the appropriate datum and whose coordinates have been

computed on the system defined in this section. Any such station may be

used for establishing a survey connection with the Missouri coordinate

system.



(L. 1984 S.B. 479, A.L. 2013 H.B. 28 merged with H.B. 650)



Effective 8-28-13 (H.B. 28)



10-11-13 (H.B. 650)



*H.B. 650 effective 10-11-13, see § 21.250. H.B. 650 was vetoed July

12, 2013. The veto was overridden on September 11, 2013.





1991



1991



60.451. 1. For the purpose of more precisely defining the Missouri

coordinate system of 1927, the following definition by the United States

Coast and Geodetic Survey is adopted:



(1) The Missouri coordinate system of 1927, east zone, is a transverse

Mercator projection of the Clarke spheroid of 1866, having a central meridian

90 degrees -- 30 minutes west of Greenwich, on which meridian the scale is

set at one part in fifteen thousand too small. The origin of coordinates is

at the intersection of the meridian 90 degrees -- 30 minutes west of Greenwich

and the parallel 35 degrees -- 50 minutes north latitude. This origin is

given the coordinates: x = 500,000 feet and y = 0 feet;



(2) The Missouri coordinate system of 1927, central zone, is a transverse

Mercator projection of the Clarke spheroid of 1866, having a central meridian

92 degrees -- 30 minutes west of Greenwich, on which meridian the scale is

set at one part in fifteen thousand too small. The origin of coordinates is

at the intersection of the meridian 92 degrees -- 30 minutes west of Greenwich

and the parallel of 35 degrees -- 50 minutes north latitude. This origin is

given the coordinates: x = 500,000 feet and y = 0 feet;



(3) The Missouri coordinate system of 1927, west zone, is a transverse

Mercator projection of the Clarke spheroid of 1866, having a central meridian

94 degrees -- 30 minutes west of Greenwich, on which meridian the scale is

set at one part in seventeen thousand too small. The origin of coordinates

is at the intersection of the meridian 94 degrees -- 30 minutes west of

Greenwich and the parallel 36 degrees -- 10 minutes north latitude. This

origin is given the coordinates: x = 500,000 feet and y = 0 feet.



2. For purposes of more precisely defining the Missouri coordinate

system of 1983, the following definition by the National Ocean

Survey/National Geodetic Survey is adopted:



(1) The Missouri coordinate system 1983, east zone, is a transverse

Mercator projection of the North American Datum of 1983 having a central

meridian 90 degrees -- 30 minutes west of Greenwich, on which meridian the

scale is set at one part in fifteen thousand too small. The origin of

coordinates is at the intersection of the meridian 90 degrees -- 30 minutes

west of Greenwich and the parallel 35 degrees -- 50 minutes north latitude.

This origin is given the coordinates: x = 250,000 meters and y = 0 meters;



(2) The Missouri coordinate system 1983, central zone, is a transverse

Mercator projection of the North American Datum of 1983 having a central

meridian 92 degrees -- 30 minutes west of Greenwich, on which meridian the

scale is set at one part in fifteen thousand too small. The origin of

coordinates is at the intersection of the meridian 92 degrees -- 30 minutes

west of Greenwich and the parallel of 35 degrees -- 50 minutes north latitude.

This origin is given the coordinates: x = 500,000 meters and y = 0 meters;



(3) The Missouri coordinate system 1983, west zone, is a transverse

Mercator projection of the North American Datum of 1983 having a central

meridian 94 degrees -- 30 minutes west of Greenwich, on which meridian the

scale is set at one part in seventeen thousand too small. The origin of

coordinates is at the intersection of the meridian 94 degrees -- 30 minutes

west of Greenwich and the parallel 36 degrees -- 10 minutes north latitude.

This origin is given the coordinates: x = 850,000 meters and y = 0 meters.



3. The position of either Missouri coordinate system shall be as marked

on the ground by horizontal control stations established in conformity with

the standards adopted by the department of natural resources for first-order

and second-order work, whose geodetic positions have been rigidly adjusted on

the appropriate datum and whose coordinates have been computed on the system

defined in this section. Any such station may be used for establishing a

survey connection with the Missouri coordinate system.



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