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Everything posted by DaveD

  1. I am very sorry to see this go. Many thanks to so many who have posted great pictures and hand-held positions that I've been able to harvest and improve the quality of tens of thousands of stations in the National Spatial Reference System. I'd like to think that I've made some friends here along the way as well. This has been a great site to help the National Geodetic Survey do a bit of educating about the importance of these data to the country. If anyone has follow-up comments or questions about these marks just drop me a line -- base9geodesy@gmail.com. Peace to all and thanks again -- Dave Doyle owner Base 9 Geodetic Consulting Services NGS chief geodetic surveyor (retired)
  2. It's always best if you owner contact info, but if that's not available for whatever reason than yes submit reports detailing mark conditions. Having an updated recovery does not in any way indicate general right of access on private lands.
  3. Excellent Michaelcycle. I must admit to a certain level of frustration when I see a note posted by a geocacher that they found a bench mark with a scaled position and it was "way off" but then they don't provide the value they got.
  4. I don't specifically remember PG0958, but in general yes that's probably me. In general, I review posts each day to see if someone has posted good quality pictures and/or hand-held values for scaled bench marks. I never post a recovery for a mark found by a geocacher since I did not recover the mark myself. I validate all hand-held positions to ensure that the match the station description. Assuming all of decent quality I can then upload them to the NGS Integrated Database. Having spent years on the NGS datasheet committee I still feel a commitment to do what I can to improve the quality of the reference frames.
  5. These are not in error. All of those are USC&GS bench marks that have relatively accurate horizontal positions that were determined in 1942 by the U.S. Geological Survey. Their values are published on the North American Datum of 1927 (NAD 27). I harvested them and simply transformed the coordinates to NAD 83. They more than satisfy the requirement to be labeled as HD_HELD1. I have performed similar transformations for several thousand scaled marks that had been set by USC&GS and later positioned by USGS. Regrettably the vast majority of horizontal control established by USGS was never formatted and provided to the National Geodetic Survey for inclusion in the National Spatial Reference System.
  6. If you're looking for a great holiday gift for your favorite bench mark hunter, take a look at "Lasting Impressions" from Bernsten International The author, Ronda Rushing is the daughter of the company's founder and until retirement was the company president. It's a great collection of pictures and stories about unique and interesting survey marks across the country.
  7. trmcconn Excellent questions. You are correct that in a 3D Earth Centered Earth Fixed (ECEF) coordinate system, the Z axis is along the rotation axis of the Earth. Since that is constantly changing, geodetic institutions such as the National Geodetic Survey will commonly “fix” that location at some point in time. In the case of the North American Datum of 1983 it was chosen to be January 1, 1984 (1984.0), as was then defined by the Bureau International de ‘Heure (BIH) now incorporated in the International Earth Rotation and Reference System Service (IERS) www.iers.org. It then follows that the X axis is defined as being along the equatorial plane in the orientation of the internationally accepted orientation of 0 longitude which is Greenwich, UK as Bill93 so correctly pointed out and the Y axis is orthogonal east to the X axis. At the time of the development of NAD 83 and the original WGS 84 the only active satellite positioning service was the Navy Transit Doppler https://en.wikipedia.org/wiki/Transit_%28satellite%29. At that time the best we could do was about 1 meter with Doppler consequently the knowledge of the 3D location of Earth geocenter was about 2 m. Today with the mega enhancements of space-based positioning systems and international collaboration we now know the location of geocenter to about .02 m (some say better). Our national datum NAD 83 is still defined to its original geocenter location. Again, as Bill93 indicated that will change with the new datums now scheduled for release in 2025 or 2026. There are several short (1-hr) YouTube videos I did on geodetic datums for the Geospatial Users Group a few years ago that you may find helpful in understanding how these systems have evolved -- https://www.youtube.com/channel/UCG69vYuN1Q61fWKiXffzo9A/videos. I hope this is helpful
  8. Let's be very clear, "NGS support for the database of survey marks" is NOT going away. In fact the agency is actively working on new provisions where surveyors (and others) who want to follow the data submission protocols - called Blue Booking and/or use OPUS Projects and Shared Solutions can easily submit their own data for publication. NGS takes this effort very seriously. What has changed is that these passive marks will no longer define the horizontal and vertical datums of the National Spatial Reference System, that will be performed by the network of Continuously Operating Reference Stations (CORS). Passive marks will continue to play a significant role in land surveying and many engineering and geophysical applications. Information on how to properly set a passive mark can be found in NGS BENCH MARK RESET PROCEDURES beginning on page 14. Bill93 is absolutely correct, you will never be able to meet the accuracy requirements for NGS with a simple cheap code receiver.
  9. The magnetic station in Croydon was set by USC&GS observer W.F. Willis in the fourth quarter of 1901. See page 125 of the USC&GS Superintendent's Annual Report of 1901 Those are great old stations and I'm glad to see it's well preserved and now part of the National Spatial Reference System. Regrettably there is no database of these old stations. Finding data on them can require a certain amount of detective work.
  10. Both USC&GS and USGS set "Meridian Marks," although only USGS had an actual meridian disk for their work . Both agencies had robust magnetic observation programs - now largely combined into activities by USGS. These marks were set to support local land surveyors to be able to determine the magnetic deflection to apply to their compass readings. Long before we were even a country, the vast majority of property boundaries were determined using a compass. Even thought the instruments changed in style, the compass was a critical part of surveying until the advent of GPS. Since any compass reading is highly impacted by local magnetic variations, USC&GS and USGS engaged in programs to set pairs of stations, typically on the grounds of county courthouses, for which they would determine the magnetic direction and "true" (typically astronomic observation) between the pair. In many communities it was a requirement for anyone performing boundary surveyors to go to those stations once a year to compare the readings from their instruments to the values published by the government. This would give them an offset that they could apply to their own measurements to attempt to give the best magnetic direction along any given line they observed. For a range of reason this effort was abandoned by probably the late 1920s. These markers are a great example of the nations surveying and mapping history. A very good example of some restoration efforts was done by the Maryland Society of Surveyors over the pair set at the Fredrick County courthouse https://www.hmdb.org/m.asp?m=89631
  11. USGS stream gage reference marks are not like reference marks for a triangulation station. There is no station mark only the stream gage. They don't typically measure the distance from the RM to the gage but rather perform leveling to determine the height difference. Like Wister6813 and Bill93, I think the coordinates are a typo. USGS has set thousands of these marks across the country and only a very tiny fraction have ever been accurately connected to the National Spatial Reference System maintained by NGS. In some cases the gage has long since been removed but the RM remains.
  12. While I can't speak directly to a line "371" in Indiana, it's highly likely there are more as Bill93 noted. It certainly wasn't normal but there were several instances during my tenure at NGS (72-13) where one or more level lines were set and for a variety of reasons never leveled to.
  13. Correction has been make.
  14. Thanks for the sharp-eyed posting. Since this mark is less than a km from Montana I'm sure it was just a typo when someone entered the recovery. I've sent a note to one of my colleagues still at NGS to review and mark the appropriate correction. The MN DoT surveyors are a great hyper-active bunch but I'm pretty sure they didn't recovery this one.
  15. There are no systematic surveys performed near the polar regions. The U.S. Geological Survey (USGS) has set a survey marker at the South Pole ever year for several decades for the purpose of estimating tectonic motion. Since the polar regions do not belong to any one nation their are no national surveying requirements. Because of the dynamics of ice motions and surface marks would be disturbed/suspect in fairly short order. The use of azimuth marks was started by the U.S. Coast & Geodetic Survey (USC&GS) in the early 1930s (32-33) as a way for local land surveyors who lacked sophisticated geodetic instruments to be able to connect their local surveys to the national coordinate framework. The azimuth from the triangulation station to the azimuth mark (typically about .25-.5 mile away) are always computed with respect the reference ellipsoid used for the coordinate system - either Clarke 1866 for the North American Datum of 1927 (NAD 27) or Geodetic Reference System 1980 (GRS 80) for the North American Datum of 1983. If you are using satellite positioning systems and want to "get things right" then all positions and directions should be computed with respect to a reference ellipsoid -- GRS 80 is the current international standard and likely to be so for many years to come.
  16. That reply from NGS must be from someone relatively new who is doesn't yet know that USGS does not have a database - never will. We tried hard back in the '80s and '90s to work with USGS to automate their data for inclusion in the NGS Integrated Database - lots of talk but not much action. They submitted a bit of their horizontal data in some western states but that was about it - none of their leveling data ever came across.
  17. Pipe marks were common largely because they were very easy to prepare and set. Concrete marks are heavier even if they are prefab and certainly require more time and resources when they were poured in place although they are way more stable. Pipe marks were also very popular with US Government Land Office (USGLO) and the Bureau of Land Management (BLM).
  18. Without more specific information about the marks location my best guess is that the info below published by the U.S. Geological Survey in Bulletin 766-U is the mark you're looking for:
  19. The marker you found is one of many set by the U.S. Geological Survey (USGS) in support of their great effort to create the national series of topographic maps. While the positions and heights they determined for these and their other marks were good enough to support that effort, they were seldom of the quality required by the U.S. Coast & Geodetic Survey (USG&GS), now the National Geodetic Survey (NGS) to be a part of the foundation horizontal and vertical national datums. The vast majority of USGS marks in the NGS database and listed for Benchmarking are individual marks that were observed by USC&GS/NGS as part of their later field efforts. So while PTS 1-5 and likely 7-?? were set only this particular mark was later observed to the highest national standards. Information on the other marks can be obtained by contacting the USGS field office in Rolla, Missouri.
  20. Back in "the day" the U.S. Coast & Geodetic Survey had essential three different survey functions for control marks. 1) General geodesy, set and observed by horizontal and vertical field units at the highest levels of positional accuracy. They are the ones who set Triangulation, Traverse and Bench Mark disks. 2) Airport survey crews responsible for positioning major airports as the foundation for instrument approach procedures and aeronautical charting. In many cases these field teams were small and usually set marks labeled "Topographic" 3) Shoreline crews - generally worked off USC&GS nautical charting ships. The often set "Hydrographic" disks as the support for either shoreline plane table surveys and/or associated photogrammetry surveys. Most control information for these Topographic and Hydrographic marks was managed by the respective USC&GS offices that performed shoreline mapping and aeronautical charting. Since the majority of these stations were not observed to national geodetic standards they remained unpublished for the general public but often used for repeat mapping and charting work. Over the years, from time-to-time some of these marks were connected by the geodetic field teams and their positions upgraded to national standards and are now published by the National Geodetic Survey. Regrettably sometime back in the late '80s or early '90 the paper record of most of these marks were destroyed as they no longer served their original purpose with the advent of GPS.
  21. Bill93 - send a note to Malcolm Archer-Shee -- malcolm.archer-schee@noaa.gov
  22. Azimuth marks were set for most triangulation stations because intersection stations (e.g. church spires, water tanks etc.) were in many cases not visible from the ground (VG) from the triangulation station, and in many, many cases there were no intersection stations anywhere near the triangulation station. For a surveyor to efficiently use the geodetic network it was required to have position coordinates (latitude, longitude and/or State Plane Coordinates) and a corresponding source of azimuth of orientation. The U.S. Coast & Geodetic Survey (USC&GS) started setting AZ Mks in the mid-1930s as increasing numbers of surveyors were being required to use them mostly for government programs such as road construction and local mapping.
  23. NGS started automating all the positional, height and descriptive data for marks that they already had in paper form beginning in the mid-1970's. All of the original data that is now in the database was hand punched on 80 character cards. Over the years the database structure and data entry systems have changed and numerous automated checking routines that did not exist when the DB was first developed. These data, along with a similar cooperative effort by the Canadian Geodetic Survey formed the very first national geodetic control databases anywhere in the world. While the agency did extensive outreach to other federal and state agencies performing geodetic surveys (e.g. USGS, Bureau of Land Management, Corps of Engineers, TVA etc.) only a very modest amount of data was ever received from them.
  24. Both marks you found were set by the U.S. Geological Survey (USGS). The second one DOP 2 1959 is a standard marking they used which includes the initials of the survey team's chief of party. Regrettably the vast majority of the data for marks set by USGS was never submitted to the U.S. Coast & Geodetic Survey (USC&GS), now the National Geodetic Survey (NGS) for inclusion in the national reference systems. You may be able to find some information on these two marks by contacting the USGS office in Rolla, MO -- https://mcmcweb.er.usgs.gov/
  25. The Florida Geospatial Users Group has recently posted several 1-hr videos that describe some of the fundamental concepts in geodesy including; reference surfaces, horizontal and vertical datums and the forthcoming 2022 datums planned by NGS -- https://www.youtube.com/channel/UCG69vYuN1Q61fWKiXffzo9A/videos These may help geocachers better understand the importance of what are generically referenced on this site as "bench marks"
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