The geological survey corps of E.T. Perkins, Jr., is now at Sawtooth. During the past few weeks it has been operating on the headwaters of the various streams tributary to Wood river from the north. The highest of the peaks at the head of East Fork of Wood river has been duly confirmed with the name of “Hyndman Peak,” in‘ honor of Major Hyndman, our fellow-townsman and Mr. Perkins is thoroughly satisfied that it is the highest mountain peak in the state after repeated efforts and tests, having determined its height at 12,072 feet. During the past week Messrs. Goods and Ganuett, chief geologist and topographer from Washington, D. C., visited Mr. Perkins in camp near Galena. This Work is being well and thorougly done by most competent and skillful officials and cannot be too highly commended. Very soon we will have perfectly correct maps of the whole Wood River and Sawtooth regions.
Thomas M. Bannon was also a self-taught mountaineer. Although his name is not widely known in mountaineering circles, during his surveying career from 1889 to 1917 he climbed nearly one thousand summits in the American West. More than two hundred of these summits were in Idaho. Bannon’s cryptic reports, supplemented by the rock Cairns, Wooden triangulation signals, chiseled cross-reference marks; and brass benchmarks that he left behind tell his fascinating story. More than one hundred of his Idaho ascents were probably first ascents. These climbs included many of Idaho’s highest and most famous peaks, including Mount Borah (which he called Beauty), Leatherman Peak, and Invisible Mountain in the Lost River Range; Diamond Peak (which he called Thumb), Bell Mountain (Bannon’s Finger), Lem Peak, and May Mountain (Bannon’s Hi Peak) in the Lemhi Range; Standhope Peak and Smiley Mountain in the Pioneers; Castle Peak in the White Clouds); and Mount McGuire in the Salmon River Mountains. Bannon’s death at 48 cut short an extremely active life.
I spent a good part of the 1990’s investigating pioneer government surveyors in the Idaho and western US mountains. This involved recovering some 100 mountain top triangulation stations placed by Bannon & party in Idaho from 1911-1915. In his career as USGS Topographical Engineer 1894-1917 T.M. Bannon had a hand in making ~50 topographic maps.
Having grown up myself in Maryland, a highpoint was a July 1995 pilgrimage to the Bannon burial plot at St Lawrence Martyr R.C. Church in Jessup. Bannon family monument (like T.M.’s triangulation monuments) occupies a prominent position in the church graveyard.
Photo on right is T.M.B. gravestone. Rick Baugher Photo
Obituary notice from Washington Evening Star, Feb 6, 1917:
THOMAS M. BANNON DIES AFTER A BRIEF ILLNESS
Was Engineer of Topographic Branch Geological Survey- Funeral Thursday at Jessups, Md.
Thomas M. Bannon, engineer of the Topographic Branch of the geological survey and a prominent resident of Anne Arundel county, Md, died Sunday evening at Maryland University Hospital in Baltimore. Mr Bannon had been ill only a short time. [Author’s Note: USGS said field worker deaths at that time often attributed to typhoid fever].
Mr. Bannon had been connected with the geological survey since 1888, the greater portion of his service having been given to topographic and geodetic surveys in different western states.
Prior to the organization of the United States reclamation service, Mr Bannon was detailed to collect the data which that organization used in connection with the development of its projects in Idaho and Utah [Author’s Note: chiefly Bear River drainage].
In 1908 he was detailed to the Porto Rican government and placed in charge of surveys in developing irrigation of the semi-arid portion of the island.
During the last few years Mr Bannon’s efforts had been directed to the extension of geodetic work in western Montana and eastern Idaho and in mapping portions of the national forests in Idaho.
In addition to his official duties with the government Mr Bannon served seven years as a member of the board of governors of the Maryland board of correction and was active in many local and charitable organizations of Anne Arundel county.
Mr Bannon was unmarried, is survived by two sisters, Mary and Francis Key Bannon, and three brothers, James T., Phillip M., and Joseph Bannon.
Final notes: It is believed Bannon thru his mother Evaline was related to Francis Scott Key. Bannon’s federal appointment as an 18 year old was thru Rep. Barnes Compton, also an F.S. Key relative. Survey director John Wesley Powell was chided for hiring “Congressmen’s nephews”. Bannon estate in Jessup was demolished in 1950 to make way for Baltimore Washington Expressway.
On February 26th, 1926, the Sunday Idaho Statesman published the following report by E.S. Crawford describing the origin of the name Appendicitis Mountain, now Appendicitis Hill. Bannon’s extensive surveying contributions to Idaho Surveying are discussed on Pages 14 and 15 of the book.
Appendicitis Case – Responsible for Mountain’s Name
Answering a query of The Statesman several weeks ago as to how “Appendicitis Mountain” acquired its name, E.S. Crawford of Antelope Valley sends the Arco Advertiser the following story which adds a bit to Idaho history:
“What is now known as Appendicitis Mountain forms part of the East Canyon Wall of Antelope Valley, and is one or Antelope’s beauty spots. It is steep and rugged and rises almost from the creek bed. From the top of this mountain looking eastward, Moore and Arco can be seen.”
“In the Spring of 1915, the Hanson brothers (from Lewiston, Idaho) came through this section of the country, building monuments on the highest peaks of the mountain ranges. Among these peaks are Old Smiley, Mount Shelley, what is now known as Appendicitis Mountain and Mount McCaleb.
“During the Summer and Fall of the same year, T. M. Bannon (a geographic surveyor from Washington, D.C.) and his helper, Mr. Tucker (from New Jersey), George Adams (of Challis, Idaho) and another man from Colorado (who acted as cook for the party), camethrough, making maps and prints of the airline distances between these mountains.
“In the early part of September 1915, they camped at the foot of this mountain, in the grove of trees which is on the Crawford Ranch. On the second day of their stay, a trip was made to the mountain top. But as the fog and haze were so thick, they were unable to make the survey and planned on making another trip the following day. This trip, though they did not know it at the time, was never to be made by Mr. Bannon, for that very night he became suddenly ill and passed a night in pain from which morning brought no relief.
Stricken With Appendicitis
“About 8:00AM the next morning, they asked for the best doctor in Mackay and Dr. N. H. Farrell was called. Doctor Farrell pronounced the trouble as appendicitis and advised the removal of Mr. Bannon to the Mackay Hospital. As cars were few in the Antelope Valley, a bed was made in the back of a white-topped buggy and a trip of 20 miles, over not any too smooth roads, was made. This was Doctor Farrell’s first operation case after coming to Mackay, which proved to be a serious as well as a successful operation and Mr. Bannon (in writing to Mr. Crawford after he had recovered returned to his home in Washington, D.C.) wrote very highly of Doctor Farrell and the nurse, MissHendickerson.”
“Although lung trouble set in after the operation and Mr. Bannon had to spend a great deal of time in Ashville, North Carolina, he finally recovered from that and died from some minor ailment in either 1918 or 1919. In one of his letters to Mr. Crawford, he told of naming this mountain and having it put on record in Washington, D.C. as Appendicitis Mountain.”
Mountain climbers and obsessive peak-baggers have a common goal: to stand atop a specific mountain or series of mountains. It is generally accepted that you must stand on the highest point of a mountain to claim a successful ascent. Thankfully, about 95% of the time, there is no dispute as to the mountain top’s exact location (true summit) and its exact elevation (true elevation). But about 5% of the time, things can get murky. Sometimes the location of the true summit is in dispute; sometimes the true elevation (measured in either in feet or meters, or both) is in dispute. This essay attempts to isolate and address these two issues.
Where is the true summit and how is it determined?
To answer this question, we must examine several generic cases (with specific illustrations of Idaho Mountains when possible). We shall start with the easiest case and then progressively handle more complicated cases.
CASE #1
The easiest case is one in which there is one, and only one, highest point. It may be a measured point using a USGS topo map’s figure or it may be the area above the highest contour line on the map (an unmeasured summit). In the latter case, there is only one “highest contour line.” But even in this simple case, you may have to wander around on a summit plateau searching for the “highest point” (measured or unmeasured). Sometimes, it’s just not possible to locate a clear, highest point on a particularly flat summit area. In other instances, some kind soul has built a cairn at what they consider to be the “highest point” and your search is probably unnecessary. In other cases, a surveyor has left a USGS benchmark, or rebar stuck in the ground, or a large cairn with a post in it to indicate exactly where the elusive high point is.
CASE #2
This is the case where a mountain has two measured summits of exactly the same height. THIS IS EXTREMELY UNUSUAL. In Idaho, Peak 8297 fits the bill. This peak is located just off US-93, south of Challis, at Broken Wagon Creek Road. The peak has a narrow summit ridge that stretches from South to North and is over a mile in length. The North Summit is measured at 8,297 feet. The South Summit is measured at 8,297 feet. Which one is the true summit? BOTH ARE. A true peak-bagger will climb both summits to claim this mountain. Doing only one isn’t enough. Why didn’t you climb the other one?
CASE #3
This is the most deceptive case. It is a case in which a measured summit appears to be the true summit, but isn’t. There is an unmeasured summit nearby that sits above a higher contour line than the measured summit. When climbing obscure mountain peaks in Idaho, this case occurs with a much greater frequency than you would think. If you simply look at the USGS topo map, you will be lured into believing that the measured summit IS the true summit.
It is only when you look at the map more closely (or consult an authoritative source on the location and elevation of the true summit of that mountain peak) that you realize that the measured summit is NOT the true summit. The [nearby] unmeasured summit is undeniably higher in elevation (thanks to the higher contour line) and is the true summit. Another way that you will stumble upon Case #3 is when you consult a respected source for peak information and are puzzled as to how they arrived at an elevation for the peak that doesn’t coincide with the measured elevation.
For example, let’s say we have a peak that has a measured summit of 9,995 feet. But your favorite source for peak information lists the peak’s elevation at 10,020 feet. What’s going on here? You examine your source’s map showing the true summit and it turns out to be an unmeasured area above a contour line. In this case, that contour line is at 10,000 feet. The true summit in this case is between 10,000 feet and 10,039 feet (assuming a 40-foot contour interval). Typically, the respected source will use an interpolated estimated of 10,020 feet. 10,020 feet beats 9,995 feet every time. Even if we assume that the unmeasured summit is only 10,000 feet, it still wins and is correctly awarded the honor of being the true summit for this mountain peak. The measured summit of 9,995 feet sits above a [lower] contour line at 9,960 feet.
Here is an Idaho illustration of Case #3. Mores Mountain has an elevation of 7,260 feet and yet the nearby measured summit is 7,237 feet. The higher summit is to the west of Point 7237, but a quick look at the map might fool you into thinking that the elevation of Mores Mountain is 7,237 feet. Page 144 of the book incorrectly shows the elevation of Mores Mountain as 7,237 feet. The true summit is just west of Point 7237 and has a higher contour line than Point 7237. The true summit is measured at 7240+ feet or an interpolated elevation of 7,260 feet.
Be VERY CAREFUL when consulting your map(s) to not make the mistake of bagging the [lower] measured false summit. It is remarkably easy to do because the difference between the measured summit elevation and the “highest” contour line might be slim. And if the two points are separated by enough distance, your visual inspection (if you even do one) might just deceive you. This is a case where a respected authority on determining true summits and true elevations is INVALUABLE. I’m not going to name names, but there is one source in particular that is astonishingly good at determining the true summits of thousands of Idaho’s mountains. It’s really amazing.
CASE #4
This is the case where a mountain has two (or more) unmeasured summits of equal height. An unmeasured summit is one that lacks a specific elevation. It is considered the true summit if it is located above the highest contour line for that mountain. But, in Case #4, we have two (or more) possible true summits since we have two (or more) independent, “highest” contour lines of equal height. In this case, we simply don’t know which one is highest. You must stand on each potential summit and make your own determination—visually or, preferably, with the assistance of a GPS or Altimeter reading. Simply assuming that the “highest” contour line with the greatest land area above the contour line is the true summit is a logical, but not sufficient, assessment.
The closer the potential summits, the easier it is to make a subjective assessment. The farther apart the potential summits (and/or the larger the number of potential summits), the more difficult it is to make such an assessment. Tom Lopez made such an assessment on Idaho’s Triple Peak. I made such assessments on both Triple Top Peak and North Sister. In the case of Triple Peak, the contour line with the largest land area above the “highest” contour line is the true summit. However, in the case of Triple Top Peak, the contour line with the largest land mass above the contour line is NOT the true summit. In the case of North Sister (a peak with four potential summits), it was a tie between the third and fourth summits, both of which have similar land area above the “highest” contour line.
The map only creates a question as to which is the highest point on this peak.
As you can see, determining the true summit can be a tricky endeavor. The best advice is to stand atop all of the potential summits, if possible, just to be sure. If the potential summits are close to each other and you can make a visual determination then a visit to each high point seems unnecessary. A small plastic hand level is an essential tool when the highest point is in question. [The following link discusses the use of a hand level in detail: Tips & Techniques for County Highpointing with Hand Levels]
This level only weighs a few onces and is easy to carry in your summit pack.
CASE #5
This is the case where a mountain has a measured summit and two (or more) unmeasured summits and all of the aforementioned summits share the same, albeit independent, “highest” contour line. This case raises the most complicated and contentious debate. And, unfortunately, it occurs more often than you would think. In Idaho, illustrations include Kinport Peak and Oxford Peak. The easiest way (and the traditional way) of handling these cases is to simply go with the measured summit and ignore the unmeasured summit(s).
Problems arise when you give the unmeasured summit an exact altitude (typically an interpolation between the “highest” contour line and the next higher contour line). An interpolation is simply the mid-point between the “highest” contour line and the next higher contour line. Contour intervals are typically 40 feet but are sometimes 20 feet (with low elevation peaks) and can be measured in meters as well (typically 20 meters, but sometimes 10 meters). An interpolation is simply an estimate. It is not an exact measurement.
Let’s say that we have a peak with a measured summit of 10,415 feet. The highest contour line for this measured summit is 10,400 feet. We also have an unmeasured summit that shares the same, but independent, contour line at 10,400 feet. Tradition says the true summit is located at the measured summit of 10,415 feet. However, some will assign the unmeasured summit an altitude of 10,420 feet (an interpolation based on a 40-foot contour interval). Comparing the 10,420 altitude to the 10,415 altitude, the unmeasured summit wins and is consecrated as the true summit.
But all we know about the unmeasured summit is that it is somewhere in the 10,400 to 10,439-foot range. We simply don’t know its exact elevation. Is it higher or lower than the 10,415-foot measured summit? We just don’t know. We can, however, do a visual inspection of our own, preferably backed up by a GPS or Altimeter measurement of each summit. From that inspection, we can then subjectively determine the true summit. When you mix interpolations (estimates) with actual measurements, the actual measured summit is thrown by the wayside about half of the time. The other half of the time, the measured summit wins. It’s really a crap-shoot. It’s better to either accept the measured summit as the high point (tradition) or to do a subjective, ON SITE assessment.
CASE #6
This is the case where a mountain has a measured summit but has a higher, unmeasured point that shares the SAME, NON-INDEPENDENT, “highest” contour line. In Idaho, such is the case with Black Peak/Black BM (in the Black Pine Mountains) and Wet Peak (in the Lost River Range). In each of these instances, the true summit is not the USGS benchmark (the measured summit) but is a higher point about 100-150 horizontal feet away. The higher point measures at 10 vertical feet higher than the BM in both of these cases.
Tradition dictates to ignore the unmeasured summit and go with the measured summit. Visual, ON SITE inspection may very well warrant a subjective assessment that the nearby unmeasured summit is somewhat higher. Indeed, on Page 351 of Idaho A Climbing Guide, Black Peak is assigned an elevation of 9,395 feet, 10 feet higher than Black BM (9,385 feet) because of observations of climbers who have done their own ON SITE inspection. I concur with that subjective assessment as I did both a visual and altimeter-based assessment of the two humps. My Altimeter determined Black Peak to be 10 feet higher than the nearby Black BM location (the altimeter measures altitude in 5-foot increments).
Once again, your safest bet as a mountain climber/peak-bagger is to stand atop both the measured summit and the unmeasured summit, JUST TO BE SURE. In Case #6, they are likely to be located fairly close to each other, making for an easy assessment. It is a subjective assessment, however. Sources considered to be reliable/authoritative still rely on the measured summit’s altitude, AS THEY SHOULD.
Case #7
This is the case where there is uncertainty about the location of a summit because of an inconsistency in the USGS topo map measurements. Let’s look at Badger Mountain in the South Hills of Idaho:
The measured elevation for Badger Mountain is 7,585 feet. The summit is located at the western end of a wide summit plateau. However, the eastern end of the summit area is on a higher contour line (7,560 feet) than the western end (7,520 feet). How can this be? Did the USGS mapmakers intend to place the measured point at the eastern end, above the 7,560-foot contour line? Or did they forget to include a 7,560-foot contour line at the western end? Or is the 7,585-foot figure a mis-measurement?
Where is the actual high point for Badger Mountain? Based on the contour lines, the western end is lower than the eastern end and can’t possibly have the summit high point there. The eastern end has a higher contour line but a lower interpolated elevation (7,580 feet) than the specific point measurement at the western end (7,585 feet). This is all very confusing thanks to inconsistent map representations on the USGS topo map. I stood on the eastern end of Badger Mountain and, as the contour lines indicate, the high point is there. It is visually obvious and there is a summit cairn there as well. In cases like this, you must investigate the summit area for yourself and make your own determination of the location of the high point, ignoring the USGS topo map’s inconsistencies.
What is the true elevation of a summit and how is it determined?
There are two types of true elevations: actual/measured ones and estimated/unmeasured ones. We will discuss each in turn.
Actual/measured summits
In the process of mapping the Western United States, many mountains were measured by the intrepid surveyors working as part of a U.S. Government-funded project. In more recent times, the United States Geological Survey (USGS) has placed specific altitudes on many mountain peaks as well as USGS benchmarks. Periodically, these altitude assessments are updated, as can be seen with a comparison of an [older] 15-minute USGS topo map to a [more recent] 7.5-minute USGS topo map. Tradition is to ascribe the most recent altitude measurement to be the correct one. If an altitude is no longer given on the latest 7.5-minute map, then the [older] 15-minute map assessment is used. In addition, some sources use North America Vertical Datum of 1988 (NAVD88) measurements as a supplement to the [older] USGS topo map measurements.
Regrettably, there are inconsistencies found on USGS maps, data sheets/maps and BGN pages. Here are two examples:
This graphic shows the discrepancy between a USGS map and the underlying data sheet for the Black Benchmark in Idaho’s Black Pine Mountains..This graphic shows discrepancy between a USGS map and the associated Board of Geographic Names page for Black Pine Peak in the Black Pine Mountains..
In most cases, minor changes (or inconsistencies) in measured altitudes are not terribly important. It can become an issue, however, when comparing two summits of similar height (e.g., Black Pine Peak versus Black Peak/BM) where one peak is a ranked summit and the other is an unranked summit. But, thankfully, that situation is not common. Given the GPS technology that we now have (and perhaps more accurate surveying equipment for ON THE GROUND work), we will probably see some adjustments to specific altitude measurements in the future. And, generally speaking, it’s not a big deal.
Estimated/unmeasured summits
It’s really astonishing how many mountain points and peaks have specific altitude measurements. However, many of the more obscure Idaho peaks lack a specific altitude figure. In these cases, sources rely on the highest contour line as the starting point to make an assessment of a specific altitude for a mountain peak. Typically, an interpolation is used as the specific measure of a peak’s altitude. For example, a peak with a “highest” contour line of 10,400 feet is assigned an altitude of 10,420 feet (assuming a 40-foot contour interval). And, with nothing else to rely on but a topo map with contour lines, such an interpolation is a reasonable estimate. It’s probably more logical than any other estimate. And it’s better than using an ill-defined figure like “10,000+ feet.”
Problems arise when you have a mountain with multiple potential summits (Case #5), one of which is a measured summit. Tradition says to use the measured summit’s altitude and ignore the unmeasured summits entirely. Sources considered to be reliable/authoritative either go with tradition or use the higher of the interpolation and the measured altitude. Others rely on climbers’ ON SITE evaluations.
Given the rather arbitrary nature of comparing interpolations/estimates to actual measured altitudes, I side with tradition on this one. But an ON SITE inspection is not a bad thing. I do it all the time. If you are a purist mountain climber/peak-bagger as I am, you simply must stand on all of the potential high points and make your own determination, if for no other reason than you wish to honestly say that that you stood on the highest point. In cases where a nearby summit is visually [and obviously] lower in altitude, I see no need to stand on the lower summit(s).
That being said, when I stood on the [higher] unmeasured south summit of Kinport Peak and could clearly see that the measured [and accepted] north summit is lower in elevation, I still dropped to a saddle and climbed that northern summit JUST TO BE SURE. And my Altimeter concurred, giving it a 20-foot lower altitude than the [unmeasured, unrecognized] south summit. And I accept the altitude for Kinport Peak as 7,222 feet, even though I know that the actual summit of Kinport Peak is closer to 7,240 feet. Until a recognized, authoritative entity (like the USGS) measures the south summit and confirms my visual (and altimeter-based) assessment, I cannot override the 7,222-foot figure.
Mis-measured summits
This is perhaps the most perplexing case of all and the most difficult to resolve. What is the correct elevation of a mountain peak with a measured altitude that is inconsistent with the USGS map contour lines? Let’s look at Ibex Peak as an illustration. Ibex Peak is an iconic summit located in the South Hills of Idaho. Here is what the USGS topo map shows:
The measured elevation is 7,272 feet and the summit area is pretty small. However, it is impossible for the elevation to be 7,272 feet since the highest contour line is 7,200 feet. Based on the contour lines, the interpolated elevation is 7,220 feet and the maximum elevation is 7,239 feet. Did the USGS mapmakers mis-measure the point elevation (7,272 feet) or fail to include the 7,240-foot contour line? Who knows? The standard convention in this case is to go with the measured elevation of 7,272 feet and ignore the missing contour line(s).
Summary and Conclusions
We can’t always rely on measured estimates of a mountain’s height. Nor can we always be sure that the measured point is the highest point. But neither should we blindly accept interpolations as surrogates for the real thing. We can’t always rely on subjective determinations of where the highest point is (e.g., the contour line with the greatest surface area above it). Sometimes that methodology is correct, sometimes it isn’t.
The best way to deal with all of the possible inaccuracies and estimates is to stand atop every one of the potential high points on a mountain, JUST TO BE SURE. It’s really that simple.
The two most popular websites for climbers are peakbagger.com and ListsofJohn.com. The methodology each of these websites for determining a peak’s elevation is set out below:
Lists of John’s elevation discussion.Peakbagger’s methodology discussion.
Lyman Marden was a member of the USGS team that surveyed the Borah Peak quadrangle. He wrote an article entitled Climbing the Slopes of Mount Borah—the Dean of Idaho Peaksabout the survey. This article appeared in the Idaho Statesman in 1935. In 1950, he wrote the following report for the Boise Public Library.
—An account given to the Boise Public Library on April 15, 1950 by Colonel Lyman Marden, a member of the party that surveyed the Borah Peak quadrangle and placed the benchmark on the top (September 13, 1934).
Located halfway between Mackay and Challis, Idaho. Elevation 12,665 feet above sea level. Highest in the State. Approached via Highway 93 to Challis and Highway 93 toward Mackay or via Highway 20 to Arco, thence to Mackay and toward Challis.
The Challis approach is enriched by the Salmon River country through which Highway 93 runs.
The Arco-Mackay approach is one of great contrast. The Lost River Range, which culminates in Borah Peak, begins as low hills near Arco on the edge of the Snake River Plain. From there, the Range rises to a long series of peaks over 11,300 feet and several over 12,000 feet. See United States Geological Survey, Topographic Map, Borah Peak Quadrangle 1934-35.
A road crosses the mountains just a few miles from Borah Peak through Doublespring Pass and gives access to beautiful country at the headwaters of the Pahsimeroi River, one fork of which rises from the North and East Faces of Borah Peak. These headwaters are scenic with long, grassy slopes called Horse Heaven and at a higher elevation Goat Heaven, and a backdrop of perpendicular mountain faces carved out by glacier action. Small caves may be found at surprising places in the high ridge between the forks of the Pahsimeroi. Good but limited camp spots are available. Obtain Forest Service advice at Challis or Mackay and local ranchers’ advice on springs, streams, wooded areas, etc.
Rivers and creeks in the near vicinity of Borah Peak are of the Lost River type and are apt to lose themselves in the gravel of the valleys for many miles only to reappear. Big Lost River and Little Lost River lose themselves in the Snake River Plain.
The Pahsimeroi River reappears just before emptying into the Salmon River. Fishermen say it is a peculiar shock to run out of water while fishing downstream. There are many interesting phenomena in the general area. Almost certainly some of the peaks have never been climbed. There are castle rocks and pinnacles, hanging lakes, big springs, and distorted and twisted strata. Just north of Borah Peak on the edge of the Pahsimeroi Valley and east of Doublespring is an old volcanic crater containing a crater lake, part of the volcanic action represented by the Craters of the Moon National Monument many miles to the south. It is believed that a large meteor left a wide pockmark in the Pahsimeroi Valley near the upper edge of a distinctive alluvial fan close to the North Face of the Pahsimeroi Mountains. Those who desire to climb Idaho’s highest peak are advised to seek a road to the base of the mountain that leaves the Challis-Mackay Highway 93 quite close to the Dickey Ranch and Post Office. The view of Borah Peak from Dickey will reveal a long, curved ridge ascending to the top. The base of the ridge nearest Dickey is divided by a shallow draw slightly darkened by scrub timber. Ascend the shallow draw and continue along the converged, sharpened ridge to the top.
The Lost River Range as viewed from the summit of Mount Borah by Lyman Marden (USGS 1934).
Lee Morrison was a USGS topographic engineer who led many mapping expeditions in Idaho in the 1920s and 1930s. He announced in 1929 that his calculations had identified an unnamed peak in the Pahsimeroi Mountains of the Lost River Range as being much higher than Mount Hyndman. The peak was soon there after named Borah Peak (aka Mount Borah). In the 1930s, he led the team that mapped the Borah Peak 15-minute quad. Climbers have unofficially named Peak 11367 “Mount Morrison” in honor of his contributions to Idaho.
Lee Morrison at the USGS camp for the Borah survey. Lyman Marden Photo
