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>>In general, a CRS is built using a geodetic datum where a geodetic datum is (according to Wikipedia - https://en.wikipedia.org/wiki/Geodetic_datum) a global datum reference or reference frame for unambiguously representing the position of locations on Earth by means of either geodetic coordinates (and related vertical coordinates) or geocentric coordinates.
FYI the “datum” business is more complicated than you might imagine. The US National Spatial Reference System is currently being ‘modernized’ as North American Datum (NAD) 83 and vertical datums such as the North American Vertical Datum (NAVD) 88 are to be replaced with new terrestrial reference frames and a novel geopotential datum. The changes are designed to incorporate a ‘dynamic earth’ i.e. with mobile tectonic plates and time-variant datums.
Also a good reference for geodesy etc is the European Petroleum Survey Group https://EPSG.org and its Geodetic Awareness page https://epsg.org/geodetic_awareness.html.
My 2 cents… The topic is one for specialists. There is a lot of prior art. Also in my humble opinion, RDF is a poor tool for science and engineering. Modeling with RDF quickly becomes idiosyncratic and unintelligible to the domain specialist. Perhaps this is the intent?
I nonetheless very keen to hear of examples of successful RDF modeling in a scientific context.
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My 2 cents
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>>In general, a CRS is built using a geodetic datum where a geodetic datum is (according to Wikipedia - https://en.wikipedia.org/wiki/Geodetic_datum) a global datum reference or reference frame for unambiguously representing the position of locations on Earth by means of either geodetic coordinates (and related vertical coordinates) or geocentric coordinates.
FYI the “datum” business is more complicated than you might imagine. The US National Spatial Reference System is currently being ‘modernized’ as North American Datum (NAD) 83 and vertical datums such as the North American Vertical Datum (NAVD) 88 are to be replaced with new terrestrial reference frames and a novel geopotential datum. The changes are designed to incorporate a ‘dynamic earth’ i.e. with mobile tectonic plates and time-variant datums.
Also a good reference for geodesy etc is the European Petroleum Survey Group https://EPSG.org and its Geodetic Awareness page https://epsg.org/geodetic_awareness.html.
My 2 cents… The topic is one for specialists. There is a lot of prior art. Also in my humble opinion, RDF is a poor tool for science and engineering. Modeling with RDF quickly becomes idiosyncratic and unintelligible to the domain specialist. Perhaps this is the intent?
I nonetheless very keen to hear of examples of successful RDF modeling in a scientific context.
On Feb 6, 2026, at 4:36 AM, Chris Partridge <partri...@gmail.com> wrote:
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Chris,
Examining the definitions of various coordinate systems in various sciences and technologies is a large and painstaking undertaking.
I can only share an application of Hilbert's "coordinate system" approach in Foundations of Geometry.
In my own words, but as close to Hilbert's ideas as possible:
A coordinate system in space, for example on a plane, is a figure consisting of two perpendicular lines, on each of which a point distinct from the intersection point (called the origin and usually denoted by O) is chosen and uniquely named. The traditional names for one of the points are X and for the other, Y. The lines on which they are located are called the X- and Y-axes, respectively. The corresponding rays O-X and O-Y are called the regions of positive coordinates, respectively, the X- and Y-axes.
The segments O-X and O-Y are considered unit segments of their axes and are usually equal in length. Any point on the plane is uniquely associated with its X coordinate: a segment or point labeled X. The segment must also have an attribute: a sign with the values "+" or "-" depending on which direction from O it should be placed: "+" toward X, "-" toward the opposite direction. The same applies to Y.
Thus, to present coordinates, one must specify a pair of correctly attributed segments and points somewhere, perhaps on another plane parallel to the given one.
Hilbert's originality lies in the fact that he doesn't operate with non-geometric entities—real numbers.
Which requires a separate transition.
So, for Hilbert, a coordinate system is a labeled figure like this one.
It would be interesting to gather definitions from various theories and technologies in one place. I'd like to participate.
Alex
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Chris,
The mathematics and physics of WGS 84 are very interesting. I'll have to look into it. I'd start with the South Pole—it's the only place where one of the axes meets solid ground, albeit icy, and it moves 10 meters per year. But they say that even if there were rock at the point where the axis meets solid ground, it would still move. What progress has mathematical usage made!
I would ground mathematical models of spacetime in the corrections of general relativity and special relativity for satellite navigation. But I'm a long way from that.
Best,
Alex
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2.1.2.3 Spatial regionWe recommend that users of BFO:spatial region specify the coordinate frame which they areemploying, for example, when dealing with spatial regions on the surface of the Earth, the coordinateframe of latitude and longitude. Such coordinate frames can be associated with a Newtonian or arelativistic frame of reference. The reference frame might be relative to a moving object such as theearth, in which case the corresponding spatial regions move with the movement of the earth.However, they are at rest relative to their coordinate frame. Lines of latitude and longitude are two dimensional object boundaries which can move; however, they are by definition at rest relative to thecoordinate frame which they determine.Elucidation: A spatial region is, intuitively, a 0-, 1-, 2- or 3-dimensional part of space. Thiselucidation will fall short, however, unless it is understood in a way that conforms with what weknow from the theory of relativity. One step in this direction is to add: a spatial region is the sort ofentity that can be specified by means of a coordinate frame, and is always at rest relative to thiscoordinate frame.Example: The Tropic of Capricorn (with the coordinate frame defined by the lines of latitude andlongitude)Spatial regions have no qualities except shape, size and relative location.Object boundaries and sites are distinguished from the spatial region which they occupy at any giventime in the sense that (1) the former move when their material host moves, and they change shape or size when their material host changes shape or size; (2) the latter must be specifiable in terms of some system of coordinates, and they are by definition at rest relative to this coordinate frame.
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Operationally, it is quite clear how this works. The interesting question is what the position point and position region are."Such as with time in SUMO, we introduce the notions of position point and position region. A position point refers to a point in a coordinate system projected on the physical space. A position region is an abstract region in a coordinate system overlapping the physical spatial region occupied by the object. Both position point and position region are types of position measurement; i.e., ∀p PMeasure(q) ↔ PPoint(q) ∨ PRegion(q) and ∀q PPoint(q) → ¬PRegion(q).Also, it is important to note that all these definitions are synchronic; i.e., they consider only situations like snapshots in time. As such, two objects cannot have the exact same quantitative position; i.e., they can not be located at the same position point.
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Chris,
You've touched on several interesting topics for me. I'm not sure how interesting they are for you, though.
The first topic is defining the meaning of the term.
The term "Null Island" is interesting because, as far as I understand, it's not a standard, so to speak, theoretical term. At least, it's not in the glossary at https://www.iers.org/IERS/EN/Service/Glossary/glossaryStandard. However, there are many things missing there, and this is an interesting follow-up on the system of terms and their definitions in the IERS.
I understand that you use the term as a name for a point in the coordinate system with coordinates are 0°N 0°E. But if we look further in Wikipedia, under the heading "Physical location": "The point on the Earth's surface defined as Null Island is located in international waters in the Atlantic Ocean, roughly 600 kilometres (320 nmi) south of the West African coast in the Gulf of Guinea.[2]"
This means it's a name for a part of the Earth's surface with coordinates 0°N 0°E. This corresponds to the word "location" in the Wikipedia description you provided.
This leaves two different definitions for Null Island, not considering the third—the absence of coordinate values for some object in the database.
It seems to me you're sticking to the definition:
Null Island is a proper name for a point in any coordinate system with coordinates 0°N 0°E, if such coordinates exist.
The system of terms and their definitions in the IERS is the core of the corresponding formal ontology.
Is this an interesting topic?
Alex
On Feb 12, 2026, at 12:23 PM, alex.shkotin <alex.s...@gmail.com> wrote:
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It’s not a feature at all. It has no physical existence. It is part of the conceptual reality created by human society (or some subset thereof – mostly British). It is just like the Prime Meridian and the Equator, namely the intersection of the two. The same goes for the entire coordinate reference system. The challenge is anchoring that conceptual reality to some piece of physical reality – like that island in the North Sea where some guys a long time ago decided they needed a longitudinal reference point for their maritime ambitions. Should have been the western tip of Iceland, not Greenwich, in my opinion. That way the international date line and the Prime Meridian could have been one and the same, and the connection to some physical prominence in physical reality would have been a bit less arbitrary and easier to spot from space.
Another problem is that the Earth isn’t really all that solid. It also wobbles and bulges, making the location of both the Prime Meridian and the Equator a bit problematic with respect to coupling them and the more general coordinate reference system to physical reality.
Hans Polzer
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Joshua,
For me, there are three definitions of the term "Null Island": a name for a coordinate point in some coordinate system, a name for a location on Earth, and a name for invalid or missing geodata.
Since this term is used throughout Chris's post, it's important to understand which one he used.
I'm fairly certain this term isn't in the OGC Abstract Specification glossaries or the corresponding ISO TC211 191nn specifications.
It's a bit funny to me to start with such a term. But that's up to Chris.
You think Chris is sticking to the first definition. I think so too. But it's better to start with a clearly written definition of this term, since the next definition we need is that for the coordinate system Chris writes about and is a much more powerful thing.
Alex
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Mundy, B. (1986). The Physical Content of Minkowski Geometry. The British Journal for the Philosophy of Science, 37(1), 25–54.
… in Einstein's 1905 paper … The actual arguments are entirely concerned with the properties of coordinate systems, and Einstein makes quite explicit statements concerning how the coordinate systems are to be constructed, using rods, clocks, and light rays. If we follow the above suggestion of seeking for the physical subject matter of the theory among the types of physical fact which are involved in the construction of a coordinate system of the type referred to in the ordinary informal presentations, we are led to consider facts concerning rigid bodies, clocks, and light rays. 🔗
Mundy, B. (1986). The Physical Content of Minkowski Geometry. The British Journal for the Philosophy of Science, 37(1), 25–54.
The use of material reference systems in general relativity has a long and noble history. Beginning with the systems of rods and clocks conceived by Einstein [1] and Hilbert [2], material systems have been used as a physical means of specifying events in spacetime and for addressing conceptual questions in classical gravity. That such systems also provide important tools for quantum gravity was pointed out by DeWitt [3], who used them to analyze the implications of the uncertainty principle for measurements of the gravitational field. 🔗
Brown, J. D., & Marolf, D. (1996). On Relativistic Material Reference Systems. Physical Review D, 53(4), 1835–1844.
For this reason non-rigid reference-bodies are used which are as a whole not only moving in any way whatsoever, but which also suffer alterations in form ad lib. during their motion. Clocks, for which the law of motion is any kind, however irregular, serve for the definition of time. We have to imagine each of these clocks fixed at a point on the non-rigid reference-body. These clocks satisfy only the one condition, that the “readings” which are observed simultaneously on adjacent clocks (in space) differ from each other by an indefinitely small amount. This non-rigid reference-body, which might appropriately be termed a “reference-mollusk,” is in the main equivalent to a Gaussian four-dimensional co-ordinate system chosen arbitrarily. That which gives the “mollusk” a certain comprehensibleness as compared with the Gauss co-ordinate system is the (really unqualified) formal retention of the separate existence of the space co-ordinate. Every point on the mollusk is treated as a space-point, and every material point which is at rest relatively to it as at rest, so long as the mollusk is considered as reference-body. The general principle of relativity requires that all these mollusks can be used as reference-bodies with equal right and equal success in the formulation of the general laws of nature; the laws themselves must be quite independent of the choice of mollusk. 🔗
Einstein, A. (1920). Relativity: The Special and the General Theory: A Popular Exposition.
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Hans,
That's right. And one of the things Chris might be referring to is that the coordinate system associated with the Earth moves with it, always remaining at its center of mass and rotating its axes to best match the motion of the Earth's surface.
What location on the Earth's surface 0N oE falls at at a given moment in this coordinate system might be interesting.
But I haven't yet figured out what coordinate system Chris is talking about.
Alex
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On Feb 13, 2026, at 6:22 AM, Chris Partridge <partri...@gmail.com> wrote:
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Chris,
My perspective on coordinate reference systems is that they have no physical existence and are not detectable by physical sensory means unless we humans create phsycal means to do so. An alien UFO approaching Earth from points unknown will have no means to detect a coordinate reference system we create unless they establish some means of communicating with humans or interpreting human artifacts that embody the coordinate reference system in some way, such as the Prime Meridian monument. The UFO pilot will certainly not be able to detect the “null island” feature.
Coordinate reference systems can be anchored to some physical entity by convention/agreement among those who want to use such a coordinate reference system to facilitate communicating relative locations of physical or conceptual entities (e.g, school zones, congressional districts, etc). That’s what the British did when they created the Prime Meridian and associated monument. Of course, continental drift, tidal forces, and other internal semifluidic movements inside the earth make that monument a bit of a moving target with respect to other objects on the surface of the earth or in space around the earth.
Alex points out that one could instead use some center of mass of the earth as the center of the coordinate reference system, presumably calculated by using some dynamic physical model of the earth informed periodically or continuously by some battery of sensors, likely space based. That’s probably sufficient for using the coordinate reference system for orbital dynamics, possibly using the sun-earth line as a longitude reference point. But that still leaves the issue of earth’s motion around it’s spin axis and the coupling of the coordinate reference system to surface features if it is to be used to locate objects with respect to each other on Earth’s surface. And many people will still want to locate orbital/near-space objects with respect to points on the Earth’s surface. Some physical surface monument(s) are still required, albeit they might need to be “adjusted” over time like we do with our calendar and clocks to incorporate the vagaries of Earth’s orbit around the sun and it’s varying and slowing spin.
This also points out that there is a lot of coupling between coordinate reference systems and our clocks and time zones, which is why viewing such systems as a 4D construct is good. That’s also why I suggested that the International Dateline and the Prime Meridian should really be one and the same conceptual construct. Of course, pragmatics dictate that such a construct should not bisect an area of significant population density, if at all possible.
Greenwich England doesn't meet that criteria.
I don’t really have a position on coordinate reference systems relationship to spacetime other than to point out the anchoring problem for them to be useful. We naturally use the Earth and the sun as an anchors, but astronomers and astrophysicists have developed other anchors to support galactic and universe level relative location and movement analysis of the entities we see in space.
Hans
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Prime Meridian Monument in Greenwich, England
Josh,
Thanks for elaborating a bit on the geoid and geodetics. I didn’t want to take the time myself to go into all that and left it as “the Earth isn’t really all that solid”. And as you point out, some of the bulging is due to tidal forces, and not just from the moon. I thought you might like the picture above.
Hans
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John,
I concur. I saw your earlier email after I wrote the response below and was tempted to respond, but I think what I wrote pretty much said the same thing, albeit not in so many words. Of course, I was coming at it from a pragmatic application perspective and not from an ontological viewpoint.
Hans
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Chris,
Many interesting topics have been raised, but I'll mention just three:
- "worldline." When you talk about a worldline, you're most likely talking about a geometric representation of the law of motion, for example, of a particle. So, if the motion is one-dimensional, like a cannonball falling, then in a two-dimensional R×T space, its worldline will be a parabola.
- GPS is a complex modern engineering system, and one of the interesting questions is obtaining the geographic coordinates of a receiver based on its measurements. I discussed this with chatGPT – you might find it interesting https://chatgpt.com/s/t_69904996ca488191af08a14c2e203df8
- Referring to the "mollusk" in Einstein's popular work isn't the best approach – it's better to refer to the theory itself, where everything is much more sophisticated. However, I wouldn't delve into general relativity yet – it's a very strong mathematical abstraction of determinism https://chatgpt.com/s/t_69904a5ccc508191936bc4b7d142e176 Sorry, it's in Russian, but I can not translate it right now.
By the way, the links like https://borocvi.atlassian.net/wiki/spaces/4G/pages/6499205137/reference-mollusk you gave are blocked for Russia.
Alex
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Chris,
I don’t think that spacetime itself is a useful coordinate reference system, the key word being “reference”, by its very nature – and the nature of relativity. An entity can “sense” local spacetime curvature by accelerometers, but that tells it nothing about what some other entity is experiencing unless they are collocated or it knows something about the objects that might be causing the local curvature of spacetime. If spacetime is locally “flat” the only useful reference point is the entity itself. Every entity in spacetime is its own coordinate reference system. Other entities can only use that coordinate reference system if they know where they are located in it or vice-versa. That means we naturally gravitate (had to use that) to highly curved space time loci as the bases for coordinate reference systems intended for sharing location information between/among entities.
Of course, we also have lots of systems that use individual entity-based coordinate reference systems such as radars to locate objects with respect to themselves. But for these systems to be useful to others, we need to map/translate these locations to coordinate reference systems that other systems/entities can use. And that typically means we have to use a frame of reference that is shared with and understood by those other entities.
I think it may be useful to consider how general relativity and spacetime concepts impact and inform coordinate reference systems in developing an ontology for them, at least at macroscopic scales. I just have trouble envisioning how spacetime itself could be “the” coordinate reference system. Then again, I don’t pretend to have a deep understanding of general relativity concepts.
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Chris,
I believe the list of coordinate systems you provided meets the description I provided in my previous email: “That means we naturally gravitate (had to use that) to highly curved space time loci as the bases for coordinate reference systems intended for sharing location information between/among entities”. In some cases, they are using sets of such loci, but the basic idea is similar.
It will be interesting to see where your efforts in this area will lead.
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You are welcome, Chris.
By the way, you might want to consider analyzing how the coordinate reference systems you cited differ from each other. What are the attributes/features of each that are not found in the others or where they use different conceptual models. How do they differ in their scope of applicability? In what range of attributes do their implicit assumptions become problematic? What are the signs that one is using the incorrect coordinate reference system for one’s application? How do application attributes relate to the scope of applicability attributes of a given coordinate reference system?
I think of these kinds of questions as being similar to defining/specifying the performance envelope of an airplane or spacecraft. Where, when, and how can I use these different coordinate reference systems? When/where will they cause me to crash or lead me astray in what I am trying to use them for.
How/where do they overlap and how does one map from one to another, and where/when is that possible?
Some of these questions will have binary yes/no answers, while others will have quantitative answers and yet others will have subjective or application-specific answers.
These answers may help your ontology for coordinate reference systems to be more comprehensive and useful to those who have to deal with deciding what coordinate reference systems to use (or possibly develop) and how to work with multiple different coordinate reference systems if their application requires them.
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John,
I agree with your observations. Nonetheless, explicit thinking about the possible variability of coordinate reference systems can make any ontology of coordinate reference systems more useful. It’s OK to have a narrower focus for a particular product or project application. Nothing of consequence is produced without considerable focus. But it can be made more extensible and interoperable if you start with an awareness of the larger world in which it may be asked to work. That’s all that I am suggesting with my “thought experiment” questions. Just realize how narrow your focus actually is before committing a lot of effort into it - instead of being surprised at what you hadn’t considered after you built it.
Hans
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John,
I am simply responding to what Chris wrote about 10 days ago that started this thread:
“We are now revisiting some work on the ontology of coordinate reference systems - and the notion of a ‘spatial object’ - that we started around 15 or so years ago. Now, as we look a little more closely at the details quite a few questions emerge. I’m wondering whether there are people in the community with views on the topic, would be good to hear any thoughts.”
My interest was piqued enough by the “null island” discussion as I have had quite a few real world experiences with multiple different map graphics software packages for digital plotters (before they became commodities) and 0,0 lat/long issues, different map projections, crossing the equator, mapping accuracy at the poles, etc., so I jumped in when Josh Lieberman made his comments about the null island being a “humorous feature”.
I only have what Chris wrote and cited to infer what he envisions an ontology of coordinate reference systems to be, and I am offering up my thoughts to help him better explore what such an ontology might address.
Hans
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Chris,
Just to be clear, I brought up the concept of “performance envelopes” for aircraft and spacecraft to illustrate the notion of a multi-dimensional “utility” or “applicability” space for a given construct, not as potential users of coordinate systems (which, of course, airplanes and spacecraft also are). Aircraft, for example, have lots of different performance dimensions, such as altitude range, stall speed, endurance, top speed, load capacity, fuel economy, cruising speed, distance range (related to cruising speed and endurance), takeoff weight, landing weight, takeoff and landing distances, air turbulence wake size, runway loading , climb rate, air temperature (which affects many of the other dimension points), etc. just to name a few key dimensions. What are the similar performance or applicability context dimensions for coordinate reference systems?
In other words, what is the applicability space of a given coordinate reference system? What are its significant applicability dimensions and what are the appropriate scales for each such dimension, and what are the values along those dimensions where the coordinate system is suitable or performs well? Where are the edges of that multi-dimensional space where the use of the coordinate reference system is questionable or definitely not advised. You can think of it as creating a coordinate reference system for coordinate reference systems, if you like.
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Yes, exactly. And you can see that the number of possible dimensions of the performance/applicability space and associated value sets can be quite large. In the mapping domain, drawing a straight line on a Mercator map does not give you the correct course azimuth from point A to point B. In Lambert Conformal Conic map projection maps it does, which is one reason that projection is used for aeronautical charts. An interesting exercise would be to list how the different coordinate reference systems differ from each other inherently (e.g., radial vs rectilinear) and with respect to common applications of them (e.g., near-earth space tracking, earth surface navigation, inter-stellar research, etc.).
And the different dimensions/attributes may only be “semi-orthogonal” or even closely coupled with each other, such as the altitude and airspeed capability in the airplane performance envelope example.
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Hans,I think we agree about what to do and how to do it.
My point is that the choice of coordinate system depends primarily on the application. The same basic ontology may be used with an open-ended variety of coordinate systems for different kinds of applications.
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