Papa Bear said:
The very fact that you could site on Bondcliff would imnply you were not where the cairn/sign are located. The view there is next to nil. Of course it could have been more open in 1981.
I recall the sight was through the trees, but not how open the view was. It is also possible that I was on the east side of the ridge to get a better view.
Though I hate to admit it, I don't run this particular Circus McGurkis.
I'll forgive you this time, just don't let it happen again.
Note that on another thread (
Look Here), the Geocache folks have fixed the location of the cairn/sign at the south bump. Presumably they took a GPS reading when they hid their box there.
Interesting. I just checked the coord--it is the south bump.
(BTW, are geocaches legal in the WMNF? IIRC, they have been forbidden in national parks.)
I think the evidence is accumulating that the cairn/sign are on the south bump. Whether it's higher or lower or the same elevation as the x4025 bump is of course unknown until someone can measure it. Present day hiker technology may preclude that unless the difference is say 15'-20' or more. However the FTFC may decide (or not) that a spot elevation trumps an open contour. Same argument goes for Scar Ridge (where the canister is not on the x3774 bump), no?
I obviously don't know where the sign is since I haven't been there for 24yrs. However, there are some tricks that one can use to make a fairly accurate estimate of the height difference between two locations.
Aneroid altimeters are needed for 2 of the following methods. GPSes with barometric sensors and the auto-calibration turned off will do. Garmin specs 1 ft resolution on their units. (Accuracy of 10 ft with proper calibration (user and/or auto).)
Method 1. Requires 2 aneroid altimeters and 2-way radios. Synchronize the altimeters to the approximate altitude at pt A. Carry 1 altimeter to pt B and compare readings by radio. Might be worth doing twice, with the altimeters switched to minimize the effects of any differences between the altimeters.
Method 2. Requires 1 aneroid altimeter: measure at pt A, then pt B, then back at pt A. (Try to make the travel times equal). Compare altB to the average of altA-1 and altA-2. (The dual measurments at pt A allow you to remove the effects of changes in the atmospheric pressure.) You can do this as many times as you want (or with as many altimeters as you can muster) and use the multiple data points to compute an average and a standard deviation.
Method 3: take a hose long enough to reach between the two locations. Fill it with water (making sure you clear out any air bubbles). Hold both ends up and let the levels settle. The water levels in the ends will be the same and you can compare the local topography to the water levels. (You can drink the water when you are done if you used a clean hose.
)
Of course, you could just trust the map and use the GPS to find pt 4025. Sounds too easy, but it would really be amusing if those coord are obviously not at the top.
My estimates of the location of pt 4025 (WGS-84 datum)
NG TOPO! DRG: ................................... N44 08.636, W071 36.303
Highest point from NG TOPO! DEM: .. N44 08.638, W071 36.305, 4009 ft
Garmin US Topo 24K (DLG): ............... N44 08.642, W071 36.298
(coordinate format: Ndd mm.mmm, Wddd mm.mmm)
(.001 min N = 6 ft, .001 min W = 4 ft)
USGS 24K topo DRGs have an accuracy spec of 90% of the points must be within 40 ft. The DEMs are on a 30m grid.
Just a note: if you are not familiar with the datum, make sure you get it correct. The default for GPSes is WGS-84, USGS topos are labeled--usually NAD-27. (It is settable in the GPS and most mapping software.) I have estimated the difference between the 2 datums in the Whites and came up with 226m.
Maybe we will have to form a VFTT mapping group and actually run an expedition to explore Owl's head summit area...
Doug