Palestine grid

Last updated
The Palestine Grid PalestineGrid.png
The Palestine Grid

The Palestine grid was the geographic coordinate system used by the Survey Department of Palestine.

Contents

The system was chosen by the Survey Department of the Government of Palestine in 1922. [1] The projection used was the Cassini-Soldner projection. The central meridian (the line of longitude along which there is no local distortion) was chosen as that passing through a marker on the hill of Mar Elias Monastery south of Jerusalem. [1] The false origin (zero point) of the grid was placed 100 km to the south and west of the Ali el-Muntar hill that overlooks Gaza city. [1] The unit length for the grid was the kilometre; the British units were not even considered. [1]

At the time the grid was established, there was no intention of mapping the lower reaches of the Negev Desert, but this did not remain true. [1] Those southern regions having a negative northing coordinate then became a source of confusion, which was solved by adding 1000 to the negative northings, running from about 900 to 1000 and from 0 to 300. [1] For some military purposes, 1000 was added to the northing coordinates of all locations, so that they then ranged from about 900 to about 1300. [1]

Portion of 1941 military map showing intersection of Palestine (blue lines) and Levant (black lines) grids near Majdal Shams Palestine and Levant grids.png
Portion of 1941 military map showing intersection of Palestine (blue lines) and Levant (black lines) grids near Majdal Shams

During World War II, a Military Palestine Grid was used that was similar to the Palestine Grid but used the transverse Mercator projection. [2] The difference between the two projections was only a few metres. [2]

After the establishment of the State of Israel, the Palestine grid continued to be used under the name of the Israel Grid or the Israeli Cassini Soldner (ICS) grid, now called the "Old Israeli Grid", with 1,000 km added to the northing component to make the northing range continuous. It was replaced by the Israeli Transverse Mercator grid in 1994. The Palestine grid is still commonly used to specify locations in the historical and archaeological literature.

Specifying locations

United Nations map showing the 1949 Armistice Agreements, with original map reference points ("MR") on the Palestine grid referenced in the respective agreements. United Nations Palestine map showing Armistice Agreements between Israel & Lebanon, Syria, Jordan & Egypt 1949-1950.jpg
United Nations map showing the 1949 Armistice Agreements, with original map reference points ("MR") on the Palestine grid referenced in the respective agreements.

The basic way of specifying a location on the Palestine grid is to write the east-west coordinate followed by the north-south coordinate using 3 digits each. For example, the Dome of the Rock is at 172132. This specifies the location within one kilometre. If more precision is required, extra digits can be added to each coordinate; for example, 17241317 gives the Dome of the Rock to within 100 metres. Many authors separate the two coordinates with punctuation for readability purposes, for example 172-132 or 172/132. [3]

Related Research Articles

<span class="mw-page-title-main">Latitude</span> Geographic coordinate specifying north–south position

In geography, latitude is a coordinate that specifies the north–south position of a point on the surface of the Earth or another celestial body. Latitude is given as an angle that ranges from −90° at the south pole to 90° at the north pole, with 0° at the Equator. Lines of constant latitude, or parallels, run east–west as circles parallel to the equator. Latitude and longitude are used together as a coordinate pair to specify a location on the surface of the Earth.

<span class="mw-page-title-main">Projected coordinate system</span> Cartesian geographic coordinate system

A projected coordinate system – also called a projected coordinate reference system, planar coordinate system, or grid reference system – is a type of spatial reference system that represents locations on Earth using Cartesian coordinates (x, y) on a planar surface created by a particular map projection. Each projected coordinate system, such as "Universal Transverse Mercator WGS 84 Zone 26N," is defined by a choice of map projection (with specific parameters), a choice of geodetic datum to bind the coordinate system to real locations on the earth, an origin point, and a choice of unit of measure. Hundreds of projected coordinate systems have been specified for various purposes in various regions.

<span class="mw-page-title-main">Ordnance Survey National Grid</span> System of geographic grid references used in Great Britain

The Ordnance Survey National Grid reference system (OSGB), also known as British National Grid (BNG), is a system of geographic grid references used in Great Britain, distinct from latitude and longitude.

<span class="mw-page-title-main">Transverse Mercator projection</span> Adaptation of the standard Mercator projection

The transverse Mercator map projection is an adaptation of the standard Mercator projection. The transverse version is widely used in national and international mapping systems around the world, including the Universal Transverse Mercator. When paired with a suitable geodetic datum, the transverse Mercator delivers high accuracy in zones less than a few degrees in east-west extent.

<span class="mw-page-title-main">Irish grid reference system</span> System of geographic grid references used for mapping in Ireland

The Irish grid reference system is a system of geographic grid references used for paper mapping in Ireland. The Irish grid partially overlaps the British grid, and uses a similar co-ordinate system but with a meridian more suited to its westerly location.

<span class="mw-page-title-main">Military Grid Reference System</span> NATO global coordinate reference system

The Military Grid Reference System (MGRS) is the geocoordinate standard used by NATO militaries for locating points on Earth. The MGRS is derived from the Universal Transverse Mercator (UTM) grid system and the Universal Polar Stereographic (UPS) grid system, but uses a different labeling convention. The MGRS is used as geocode for the entire Earth.

The Swiss coordinate system is a geographic coordinate system used in Switzerland and Liechtenstein for maps and surveying by the Swiss Federal Office of Topography (Swisstopo).

<span class="mw-page-title-main">Universal Transverse Mercator coordinate system</span> Map projection system

The Universal Transverse Mercator (UTM) is a map projection system for assigning coordinates to locations on the surface of the Earth. Like the traditional method of latitude and longitude, it is a horizontal position representation, which means it ignores altitude and treats the earth surface as a perfect ellipsoid. However, it differs from global latitude/longitude in that it divides earth into 60 zones and projects each to the plane as a basis for its coordinates. Specifying a location means specifying the zone and the x, y coordinate in that plane. The projection from spheroid to a UTM zone is some parameterization of the transverse Mercator projection. The parameters vary by nation or region or mapping system.

<span class="mw-page-title-main">Spatial reference system</span> System to specify locations on Earth

A spatial reference system (SRS) or coordinate reference system (CRS) is a framework used to precisely measure locations on the surface of Earth as coordinates. It is thus the application of the abstract mathematics of coordinate systems and analytic geometry to geographic space. A particular SRS specification comprises a choice of Earth ellipsoid, horizontal datum, map projection, origin point, and unit of measure. Thousands of coordinate systems have been specified for use around the world or in specific regions and for various purposes, necessitating transformations between different SRS.

<span class="mw-page-title-main">United States National Grid</span> Multi-purpose grid reference system used in the United States

The United States National Grid (USNG) is a multi-purpose location system of grid references used in the United States. It provides a nationally consistent "language of location", optimized for local applications, in a compact, user friendly format. It is similar in design to the national grid reference systems used in other countries. The USNG was adopted as a national standard by the Federal Geographic Data Committee (FGDC) of the US Government in 2001.

The State Plane Coordinate System (SPCS) is a set of 125 geographic zones or coordinate systems designed for specific regions of the United States. Each U.S. state contains one or more state plane zones, the boundaries of which usually follow county lines. There are 108 zones in the contiguous United States, with 10 more in Alaska, five in Hawaii, one for Puerto Rico and the United States Virgin Islands, and one for Guam. The system is widely used for geographic data by state and local governments. Its popularity is due to at least two factors. First, it uses a simple Cartesian coordinate system to specify locations rather than a more complex spherical coordinate system. By using the Cartesian coordinate system's simple XY coordinates, "plane surveying" methods can be used, speeding up and simplifying calculations. Second, the system is highly accurate within each zone. Outside a specific state plane zone accuracy rapidly declines, thus the system is not useful for regional or national mapping.

<span class="mw-page-title-main">Cassini projection</span> Cylindrical equidistant map projection

The Cassini projection is a map projection first described in an approximate form by César-François Cassini de Thury in 1745. Its precise formulas were found through later analysis by Johann Georg von Soldner around 1810. It is the transverse aspect of the equirectangular projection, in that the globe is first rotated so the central meridian becomes the "equator", and then the normal equirectangular projection is applied. Considering the earth as a sphere, the projection is composed of the operations:

<span class="mw-page-title-main">Irish Transverse Mercator</span> Geographic coordinate system for Ireland

Irish Transverse Mercator (ITM) is the geographic coordinate system for Ireland. It was implemented jointly by the Ordnance Survey Ireland (OSi) and the Ordnance Survey of Northern Ireland (OSNI) in 2001. The name is derived from the Transverse Mercator projection it uses and the fact that it is optimised for the island of Ireland.

<span class="mw-page-title-main">Israeli Transverse Mercator</span> Geographic coordinate system for Israel

Israeli Transverse Mercator (ITM), also known as the New Israel Grid is the new geographic coordinate system for Israel. The name is derived from the transverse Mercator projection it uses and the fact that it is optimized for Israel. ITM has replaced the old coordinate system Israeli Cassini Soldner (ICS), also known as the Old Israel Grid (OIG). It became the official grid for Israel in 1998.

<span class="mw-page-title-main">Israeli Cassini Soldner</span> Historical geographic coordinate system

Israeli Cassini Soldner (ICS), commonly known as the Old Israeli Grid is the old geographic coordinate system for Israel. The name is derived from the Cassini Soldner projection it uses and the fact that it is optimized for Israel. ICS has been mostly replaced by the new coordinate system Israeli Transverse Mercator (ITM), also known as the New Israeli Grid (NIG), but still referenced by older books and navigation software.

The modified transverse Mercator (MTM) coordinate system is a metric grid-based method of specifying locations, similar to the Universal Transverse Mercator coordinate system. MTM uses a transverse Mercator projection with zones spaced 3° of longitude apart.

Transverse Mercator projection has many implementations. Louis Krüger in 1912 developed one of his two implementations that expressed as a power series in the longitude difference from the central meridian. These series were recalculated by Lee in 1946, by Redfearn in 1948, and by Thomas in 1952. They are often referred to as the Redfearn series, or the Thomas series. This implementation is of great importance since it is widely used in the U.S. State Plane Coordinate System, in national and also international mapping systems, including the Universal Transverse Mercator coordinate system (UTM). They are also incorporated into the Geotrans coordinate converter made available by the United States National Geospatial-Intelligence Agency. When paired with a suitable geodetic datum, the series deliver high accuracy in zones less than a few degrees in east-west extent.

The Cassini Grid was a grid coordinate system used on British military maps during the first half of the twentieth century, particularly during World War II. The referencing consists of square grids drawn on a Cassini projection. For a period after the war, the maps were also used by the general public. The system has been superseded by the Ordnance Survey National Grid.

The mapcode system is an open-source geocode system consisting of two groups of letters and digits, separated by a dot. It represents a location on the surface of the Earth, within the context of a separately specified country or territory. For example, the entrance to the elevator of the Eiffel Tower in Paris is “France 4J.Q2”. As with postal addresses, it is often unnecessary to explicitly mention the country.

The Survey of Palestine was the government department responsible for the survey and mapping of Palestine during the British mandate period.

References

  1. 1 2 3 4 5 6 7 Dov Gavish (2005). The Survey of Palestine under the British Mandate, 1920–1948. London and New York: RoutledgeCurzon. pp. 73–75.
  2. 1 2 Dov Gavish (2005). The Survey of Palestine under the British Mandate, 1920–1948. London and New York: RoutledgeCurzon. pp. 219–223.
  3. For example, the location of Khirbet esh Sheik Mohammed is given as 1417.1984 in D. Pringle (1986). The Red Tower (al-Burj al-ahmar): Settlement in the Plain of Sharon at the time of the Crusaders and the Mamluks A.D. 1099–1516. Jerusalem Monograph Series no. 1. London: British School of Archaeology in Jerusalem. p. 71.

Further reading