ࡱ> AC<=>?@%` ӗbjbjٕ J%       8\z*@"bbb %''''''$\hĽ~K -" --K  bb`ɮɮɮ-T b b%ɮ-%ɮɮ  ɮb ,Vɮd v0ɮB->BɮɮB ݮ zɮ'ۥR KKk^ ----X"\5"\       National Spanish Trails Symposium Southern Utah University, October 2007 Cedar City, Utah SPANISH TRAILS NAVIGATION: THE DOMINGUEZ/ESCALANTE EXPEDITION OF 1776 By: Col Alva Matheson, USAF (R) Master Navigator, Command Space Rating Utah State Director: The Old Spanish Trail Association The end is near and the distance is farwhither shall we walk? Our first discussion in this symposium (PART I) will include a short developmental history of the magnetic compass and methods used by the Dominguez/Escalante expedition of 1776 to resolve compass deviation. It will also address the Franciscan penchant for attempting to apply geomagnetic variation in a relentless pursuit of longitude, and the computation of distance by sidereal methodology. The second presentation in this symposium (PART II) will address the derivation of latitude by celestial observation, and discuss frequent errors in the translation of the diary of Silvestre Velez de Escalante in light of navigational science. It will become evident that the Dominguez/Escalante expedition was never lost. The party knew where they were, they knew where they were going, and only a river and politics stood in their way. alm SPANISH TRAILS NAVIGATION: THE DOMINGUEZ/ESCALANTE EXPEDITION OF 1776 Lecture I: Spanish Land Navigation The Magnetic Compass and Spanish Trails Navigation The magnetic compass has been bane and blessing for a myriad of cultures in preceding centuries. Many countries seeking to extend their influence, whether by commerce or by conquest, learned to depend on the compass, but unfortunately they often did so at some peril. Mysterious and confounding compass irregularities were frequently ignored, sometimes with catastrophic results. Similarly, the ability of land navigators to record and chart topographical information using celestial observations cannot be understated in its importance to Spanish colonization. Yet few historians have chosen to adequately examine either purposes or processes of land navigation. They simply relegate early explorations to the role of being itinerant wanderers in the wilderness. The discovery of the first magnetic compass is often ascribed to one of several ancient Chinese cultures; though that may be more by default than by reasonable investigation. But regardless of those to whom the origin of the compass is commended, it is indisputable that the magnetic compass has always been associated with the advancement of colonial societies... The Spanish Empire was no different. The earliest compass known compass is a box compass, or dry compass as it was sometimes termed, because it was un-damped for either vibration or motion. Basically the box compass was nothing more than a lodestone induced needle on a suspended piece of silk or rice paper, which was conveniently mounted inside of a protective structure. Such a compass facilitated efficient land navigation within a given territory, and it became indispensable for movement and exploration of national and extra-national territories. But it was useless over water, however, because of its inherent instability. As the magnetic compass matured as an instrument to accommodate the reasonable division of property, a science to become known as surveying, its heralded use was not without apparent and inexplicable errors. And though most compass errors could be compensated for at a given location or locale, the errors were seldom understood and the mystical nature of the compass did little to encourage scientific study of its natural aura that was presumed to be the problem? It was not until the advent of maritime trade and the naval movement of military forces across large distances, that the compass was to make its singular contribution to global navigation. It was also here, in movement across large distances that the compass also showed its greatest malediction..., an error now called geomagnetic variation! However insidious the problem of compass error might have been, or how innocently it may have come to the attention of a perceptive user, the significance of geomagnetic variation was most likely to have been recognized in concert with calamity at sea. Being unaware of either the source or solution to geomagnetic variation, even the least conscientious of navigators would have been challenged by unexplained errors in routine observations. Trusting an uncorrected compass for any length of time or distance was always a certain step to an equally certain catastrophe. For local application of compass readings, anomalies could be summarily dismissed as an operator error. But across long distances and in uncharted waters or inclement conditions, those errors would more often result in fatal piloting decisions, and Spanish history tells us there were many of them. So, what is the nature of the beast called Compass Error? Well, compass error actually comes in two forms: Geomagnetic Variation: (sometimes called compass declination by surveyors) is that force created by the magnetic flux field of the earth, in conjunction with the electromagnetic field surrounding the earth. It varies according to the geology and the physical structures of and within the earth, and it varies with the influence of solar storms and electromagnetic disturbances. Variation is never constant. Variation is continually changing in both intensity and location. It is generally observable but not predictable. Compass Deviation: For the purposes of this discussion, compass deviation is construed as the sum total of all non-terrestrial or non-flux induced errors, i.e., the sum total of all cargo, construction, metallic or electromagnetic influences affecting a magnetic compass that are not associated with geomagnetic flux fields.. Geomagnetic variation is manifested and/or charted visibly in the form of isogonic and/or agonic lines on every navigational map. Isogonic lines are lines of constant variation over the surface of the earth; they represent the difference between any given compass direction (one that is free of deviation) and true direction which is a direction in relation to the axial rotation of the earth. An agonic line is a charted region where there is an apparent absence of magnetic variation, a limited region where all forces are balanced and the compass does in fact, point to True North without compensation. Florida is in an area of such agonic influence, much to the consternation of early Spanish navigators and explorers who frequented the region. The earliest known compass in our possession dates from the year 1111 AD. This early compass is of brass and is conspicuous for having both a gnomon and a lubber post for making accurate bearing and time observations. It is also noted for having an engraved mark to correct for local geomagnetic variation, thus allowing the user to establish both an accurate magnetic and true north direction at any given time. It was only when sea faring became common and significant were being traveled that compass error due to variation became a major problem to safe navigation. By the 15th century most geomagnetic anomalies had been charted, compensated for and/or corrected within costal waters by Spanish navigators. Compass deviation would always be a problem for all navigators, depending on such factors as cargo, vessel geometry and the dispersal of metallic armament, fittings throughout the ship. Such errors were routinely compensated for en route with periodic celestial bearings. While the source of geomagnetic variation may have been a total mystery people in the past, the Spanish found that it could be easily corrected for a give location. This was done by simply observing a celestial body (usually the pole star or the sun) or a gnomon and noting the difference between the known true azimuth of the body being observed and that of the north seeking needle of the box compass or binnacle. The difference between the two azimuth bearings was equivalent to total compass error, combining variation and compass deviation for that instant in time through proper alignment at the time of observation. Adjustments were made by moving the compass housing or external metallic compensating bars. The first attempts at long range navigation by the Spanish were hampered by the belief that by charting geomagnetic variation accurately, a vessel could carry its longitude forward with the exploration. In theory, the Spanish navigators hoped to establish their longitude by simply making an isogonal grid of the lines of constant variation, and overlaying that grid on a map of latitude and longitude. In theory this would create a navigational reference that would fix a ships location on the outward journey and ensure a safe return with whatever treasure they sought. Unfortunately, the Spanish navigators and explorers anticipated that geomagnetic variation lines would parallel lines of longitude. Unfortunately they do not, but to test their assertions they needed to find someone brave enough (or crazy enough) to venture a significant distance from port. Enter Christopher Columbus. True, Columbus found a new continent, but he also made equally lasting contributions to the history and science of navigation, including a generous lesson in what doesnt work, at least on the ocean. Typical Astrolabe, Rete and Matre It is well known that Columbus was tutored in every science associated with navigation. He also had access to every navigational instrument known to the Spanish Main. His credentials included the best training of the Jesuits and Franciscans, Abraham Zacutos declination tables, the Al Kamal for known costal locations (including Cadiz, Spain), the astrolabe, the navigators quadrant, and the navigators fore staff. The diaries of Christopher Columbus are replete with the frustrations and inadequacies of his tools, and the difficulty he had in establishing, or even recording, reliable data in the midst of ocean verities. In most cases he simply dispensed with the complexities of attempting some celestial observations with the tools available, but he always carried an accurate compass correction via Polaris. With that information and either observed latitude by Polaris or meridional passage of the Sun--and a good land-fall technique for arrival back in Spain--Columbus was able to make the return voyage with confidence and some alacrity. Successes and failures of Columbus and the early Spanish explorations were not lost on those of the academia left at home. The Jesuits and Franciscans scholars vied with each other in their pursuit of knowledge and refining their technique and mathematical calculations (and the Dominicans were not far behind). It was through their efforts to construct an accurate ephemeris that they were able to record the actual latitude and longitude of Mexico City, Mexico, by coordinating an observation of a predicted eclipse of the moon. Predicted occlusions were conveyed to the outposts of the Spanish empire. Then independent sightings or observations of the altitude of the moon were transmitted back to the motherland and other colonial outposts by courier vessels. The independent calculations and conclusions of Spain were subsequently exchanged with the colonies for comparison and critique. The conclusive information was again exchanged to establish the exact location of various colonies throughout the colonies. For Mexico City, for instance, their calculated mean positional error has been found to be within scant arc minutes of actual earth position! This was a phenomenal achievement for 16th century navigation. But colonial Spain was not through yet. With the information now available to them appropriately charted, they managed to carry their findings, techniques and positions with them as they expanded northward by land from Mexico City to the border lands of what was to eventually become New Mexico. Spanish priests routinely used latitude for a constant line of position, similar to using a Sumner line, crossing it with the league derived longitude carried with them from their point of origin. But the expectation of using geomagnetic variation to eventually carry longitude over land was never lost. ............................................................................................................................................ ........................................................................................................................................... (AUTHORS INCIDENTAL COMMENTARY...) I have observed no lack of either concern or confusion among Old Spanish Trail historians in regard to the Spanish use of the league as a measure of distance? It seems to vary all over the place one associate remarked, while seeking to unravel the mysteries of his Spanish League from interpreted documents. And so it does! As the Spanish Jesuits and Franciscans moved outward from central locations in Mexico and Florida to find and establish missions for the colonies, they were highly schooled in celestial navigation as compared to land navigation. They took their navigational skills regarding observed bodies and the compasses with them, and adapted their seafaring techniques to land uses--with little change and less concern. Dead reckoning and land fall navigation techniques were common practices and techniques, both of which were honed to a high degree of skill. They work equally well in cross country trips, if you know what you are doing, and Fray Dominguez and Silvestre Velez de Escalante, for instance, did know what they were doing! The Spanish system of navigation began with a full knowledge of latitude and longitude, and the calculations associated therewith--including time. Their approach was to first determine the angular separation of longitude, which they divided into sectors of 360 degrees in one 24 hour day. They calculated the circumferential distance of the equator to be 6300 units, which they called leagues (6028.2nm). They knew that lines of longitude were always by definition equal. They also knew that the small circle lines of latitude decreased in circumference with the sine of the latitude (i.e., each latitude decreases from a maximum circumferential distance at the equator to zero at the poles. So, the Spanish navigators simply divided the earths circumference by 360 degrees of rotation (i.e. 6300 leagues/360 degrees per 24 hour day) to determine that one degree of longitude was exactly equal to 17.5 leagues. Knowing that each degree of longitude contained 60 minutes of arc, they then divided that amount by 17.5 leagues per degree to determine that one minute of arc is equal to 3.43 leagues at the equator. They Spanish navigators then calculated the latitudinal distance (east/west along a line of latitude) very precisely to obtain a new length of a different league for each-and-every latitude of the earth. Thus the length of a Spanish League at 30 deg North latitude is the sine of the latitude for 30 deg (sin 30=0.50000) multiplied by the length of the latitude at the equator (17.5 leagues/degree) to arrive at a distance of 8 leagues per degree at 30 deg North. So, yes, a league does vary all over the place! HOWEVER, this approach WAS NOT an encumbrance to navigation. A variable league was a boon to Spanish navigators, since knowing the actual distance, or length of the league between two lines of longitude for any given latitude facilitated many computations and simplified other areas of land fall navigation. Most navigators today still carry a Boditch book of latitudinal distances, albeit in nautical miles rather than leagues, but the principle and practice of the computations has not been altered over time. NOTE: it should be mentioned that outside of celestial navigation as a practice, the Spanish in general (and Dominguez/Escalante in particular) appear to have used a different and more accommodating definition of league in their overland travels. After 1600 AD the nautical league was no longer considered practical as a land unit. The land travel system became associated with... THE DISTANCE IN MILES A MAN ON A HORSE AT NOMINAL GAIT AND WITHOUT INTERFERANCE WOULD EXPECT TO TRAVEL IN ONE HOUR, ACROSS UNFETTERED AND RELATIVELY FLAT TERRAIN!... OR... a distance of 2.63 statute miles per land league! (The length of one Spanish step was equivalent to 32 inches. It was called a vara, by the Spanish. 5000 varas were equivalent to one sito or Spanish walking mile. These were units of survey, however, and NOT units of navigation or travel. (Height was measured in a 65 inch increment or braza. which was roughly eye level increments.) It was the distance of 2.63 miles per hour that is presumed to have been used by the Dominguez/Escalante party to carry forward their longitude by deductive calculation, or DR (deductive reasoning) techniques. ................................................................................................................................................ ................................................................................................................................................ (CONTINUING, POST COMMENTARY) When the Escalante/Dominguez party began their preparations for what would become one of the epic explorations of the American Southwest, it is unlikely they paid even the slightest attention to the tools, techniques or practices they would use in their pending journey. Their training and education would have inculcated a complete acceptance of what, why, and more importantly HOW they were going to find Monterey Mission ...by the sea. The only real mystery to the Dominguez party was the terrain they would cross and the people they would encounter in the process of getting to Monterey, CA. The Dominguez/Escalante exploration party need only use proven techniques of global maritime--navigation, with a known departure point, which was... (Santa Fe, New Mexico N35 deg 41 min by W105 deg 56min) ...to arrive at a known destination point, which was... (Monterey Mission N36 deg 36 min by W121 deg 54 min) Monterey Mission in California had been settled six years prior to the Dominguez expedition, in the year 1770, and Fray Garces with whom Father Silvestre Velez de Escalante had spoken to in preparation for the forthcoming expedition, shared with Escalante what information Garces had on the physical location of Monterey. He and Father Dominguez would have both known that Monterey laid almost exactly 342 leagues (782 nm/900 statute miles) to the west, and less than 60 nm (one degree of latitude) to the north of their departure point of Santa Fe, New Mexico. The expedition was NOT, therefore, a group of wandering adventurers, but they were traveling with the knowledge, means and method to reach their destination. Only politics, religion and a river would stand in the way of them reaching their objective. INVESTIGATION: A bearing is a line of azimuth measured clockwise from north, generally taken with a pylorus or an astrolabe, and usually associated with a magnetic compass or compass correction. An observation is the establishment of the zenith angle or zenith distance of a body above or below the mean horizon to determine latitude or a line of position of the body on a great circle of the earth. Just as their previous tutors had intimated, if variation could be accurately mapped in conjunction with fixed latitude lines of position, the solutions expected of Columbus and more recent seafarers would now be realized. It is likely they blamed the lack of prior success on the instability of ocean going vessels? But over land and traveling from east to West, rather than along a parallel of longitude and with some attention to detail, that should not be a problem, right? Reinforcing the presumption that longitude could be established by reference to magnetic compass variation was the full knowledge that when the De Soto arrived with the Spanish explorers in the gulf-states and Florida, the Spanish found to their amazement that there was no error in their compass at all! With an agonic line as an immediate reference, it seemed only too plausible that as they moved westward the isogonic lines of magnetic variation would be predictable? The observed compass errors had certainly had changed from a compass direction west of true north to a compass direction being east of true north, and the difference was changing at a significantly diminished rate. On land too, the possibility of compass error through the factors of deviation could always be eliminated, in every instance, by comparison to a celestial bearing at any location where a latitude observation was obtained. In this regard, and as a background for further investigation, a connection was made through the National Oceanographic and Atmospheric Administration (NOAA) and the Naval Observatory in Washington, DC. With the kind assistance of Ms Susan McLean of that facility, I was able to encourage a computerized regression analysis of the actual and projected variation for various years beginning with the day and month of the departure of the Dominguez/Escalante party from Santa Fe, New Mexico in July of 1776. Figure 1: Table of Magnetic Variation by Observation and Regression (July, 1776 thru Calendar Year 1990) Location / YearScience Model - D positive eastStandard Model - D positive eastDelta DPueblo, COLat: 38.27355, Long: -104.6209917768.38185013.66190013.2413.1960.044195013.5813.3690.211199010.7210.7110.009Montrose, CO Lat: 38.47941 N, Long: -107.87135177614.09185014.41190014.5114.5070.003195014.6114.611-0.001199012.2112.1960.014Green River, UT Lat: 38.9833 N, Long: -110.150017769.17185014.41190015.4415.484-0.044195015.4915.495-0.005199013.2113.1980.012Saint George, UT Lat: 37.1000, Long: -113.5833 17769.98185014.52190015.4115.536-0.126195015.7215.751-0.031199013.8313.8090.021Provo, UTLat: 40.24715 N, Long: -111.64267177610.56185015.83190016.4816.55-0.07195016.8916.3850.505199014.0714.0690.001Vernal, UTLat: 40.45198 N, Long: -109.53553177610.07185015.6190015.9515.973-0.6195015.9815.785-0.405199013.3413.328-0.729Page, AZ Lat: 36.90425 N, Long: -111.4578217769.51185014.23190014.8414.918-0.078195015.1515.176-0.026199013.1413.1270.013Tuba City, AZ Lat: 36.12498 N, Long: -111.2424617769.25185013.89190014.4514.918-0.468195014.8415.552-0.712199012.8813.127-0.247Zuni Pueblo, NM Lat: 35.07248 N, Long: -108.8499717768.59185013.16190013.4113.434-0.024195013.9313.95-0.02199011.8811.8520.028Albuquerque, NMLat: 35.11721 N, Long: -106.6246317768.59185012.87190012.7912.780.01195013.3213.337-0.017199011.0911.0490.041 NOTE: The above table of variation is an isogonic tabulation (Figure 1) of data relative to the geo-magnetic variation in the American Southwest at selected locations associated with the Dominguez Escalante expedition at that time. The change in local magnetic variation at any given location on the path of the expedition is solely due to the isogonal creep the earths magnetic flux field across the intervening years. It is evident that the change in variation since 1776 approximates nearly 4 degrees of change since that time. In navigational terms, that is 240 nm of angle were it in observed altitude of a celestial body, and 4 full degrees of pylorus error. Either could cause significant cartographic problems. Figure 2: Estimated rates of change of magnetic variation in 1776 for the Spanish Trails, by NOAA geomagnetic data services, US Naval Observatory Pueblo, UT 7' E/year Montrose, UT 7' E/year Green River, UT 11' E/year Saint George, UT 6' E/year Provo, UT 7' E/year Vernal, UT 7' E/year Page, UT 6' E/year Tuba City, AZ 6' E/year Zuni, AZ 6' E/year Note: If you are interested in the rates of change for the present, enter local latitude and longitude desired into the online calculator at  HYPERLINK "http://www.ngdc.noaa.gov/seg/geomag/jsp/Declination.jsp" \t "_blank" http://www.ngdc.noaa.gov/seg/geomag/jsp/Declination.jsp Having ignored the influence and/or positional distortion caused by isogonal creep is but one of several factors that may have induced modern observers to suggest that observations of the Dominguez/Escalante expedition were in error? It may well be that it was not the expeditions observers that were in error, per se, but that todays critics are judging from a perspective that has presumed they are dealing with the same plan-form of the earth that existed in 200 years ago in 1776. One of the seldom recognized benefits of a compensated compass is its use as a chronometer to accurately, if not exactly, determine the local time of day for observing meridional solar passage to establish latitude. Note the following comment recorded by Fray Escalante: September 5, 1776 Tonight we observed the latitude and found ourselves at 40 deg 4 min. Figuring that we had not come up that much since Santa Monica, and fearing some defect in the observation, we decided to make it by the sun the halting at the hour best suited so as not to detain ourselves here where the Sabuaganas might disturb us. Silvestre Velez de Escalante A compass that has been corrected for variation and deviation, usually by a bearing from Polaris at night, can then be used during the daytime to identify high noon. This is done by placing a gnomon in a position where the shadow of the sun will progress to a line paralleling the Lubber Line, the compass needle difference being the total combination of variation and deviation. At the exact instant this occurs, the zenith distance of the sun (HO) is recorded for comparison with declination tables, to arrive at the exact latitude of the observer. The compass process is both more accurate and far less time consuming than attempting to predict noon by shadow, or bisecting two points on either side of noon and regressing the observation. It is also less demanding on ones eyesight and inherently more accurate therefore. The intimation of being in a hurry would suggest this is the procedure they would have used the following day? September 6, 1776 We went down to a little valley through which a small river of good water flows. At its edge, next to the only poplar that there is, and at eleven in the morning, we halted, ordering some companions to keep on going and the loose and loaded animals. The meridian was taken and we found that we were at 41 deg 6 min and 53 sec latitude and there having been no error in last nights observation. Silvestre Velez de Escalante The fact that the Dominguez/Escalante expedition might consider a 65 mile difference in observed position of little concern would suggest that it was not their position that was of concern! If this was the case it would be more likely it was the accuracy of their bearing and of compass deviation that concerned them. But what is evident is that the translation has brought forth an error, this one of some significant consequence. The September 5th observation was actually recorded in the Escalantes diary as 41 degrees, 4 min North latitude, and NOT 40 degrees 4min north latitude as translated. Their actual observations on these two days were less than 2 min of arc apart--scant miles between positions, and a phenomenal example of accurate observation and repetition. It should be remembered from earlier discussion above that one of the elemental purposes and expectations of the Dominguez/Escalante exploration is presumed to include the identification and recording of magnetic variation at various locations during their sojourn. Remember too, the Franciscans would have been heavily influenced by the perception and/or theory that at, least on land, an accurate chart of magnetic variation could be beneficial as a means for estimating the LONGITUDE of any given position during their travel. Again, referring to the journal of Father Silvestre Velez de Escalante: September 14, 1776 On the 14th we made no days march, holding back here so that the horse herd, which was quite weak now, could regain its strength. Before noon the quadrant was set up to check the observation by the sun, and we found no more than 40 deg 59 min 24 sec N. We concluded that this discrepancy could perhaps result because the needle deviated here, and to find this out we left the fixed quadrant set toward the north, or polar star was sighted, the quadrant being on the meridian mentioned, we observed that the needle was swinging northeast. We again took the latitude bearings by the North Star and came up with the same 41 deg 19 min of the previous night. Silvestre Velez de Escalante  Spanish Hand-Hanging Quadrant, With Pinnule: Typical Note: The common translations of the Dominguez-Escalante Journal (by Chavez and Warner), as above, are again in error! They misinterpret a Spanish word, observacione, as bearing, a word with a wholly different meaning than observation and a crucial difference to anyone more schooled in navigational sciences. A bearing yields direction only, not a latitude LOP (Line of Position). Observations yield zenith angle and azimuth. September 14, 1776 Note: 7 days since previous observation On the 14th we made no days march, holding back here so that the horse herd, which was quite weak now, could regain its strength. Before noon the quadrant was set up to check the observation by the sun, and we found no more than 40 deg 59 min 24 sec N. We concluded that this discrepancy could perhaps result because the needle deviated here, and to find this out we left the fixed quadrant set toward the north, along the needles meridian, until night time. As soon as the north or polar star was sighted, the quadrant being on the meridian mentioned, we observed that the needle was swinging northeast. We again took the latitude bearings by the North Star and came up with the same 41 deg 19 min of the previous night. Silvestre Velez de Escalante It is on this date we find the greatest commentary and description of the navigational practices and instruments being used by the Dominguez/Escalante party. Here we learn the following: First: The were using a quadrant, not an astrolabe, staff or back staff Second: The quadrant was being set up and was therefore of a stationary type and not a pinnule or hand-hanging type of instrument. Third: The quadrant used was of large scale, and needed ground support, and it was thus more accurate than any other typical instrument. Fourth: They felt confident they could read the quadrant to within seconds of arc and routinely did so, either directly or by interpolation Fifth: Since the quadrant needed set up is was not likely to have been the same instrument used the preceding day, suggesting that at least some observations could have been made by hanging-hand-hanging quadrant and pinnule as a backup, or quick and easy shooting instrument on a non recorded basis. Sixth: They concluded that part of their error was associated with compass deviation, confirming their use of the resolved compass for meridional passage observations. Seventh: They set the quadrant to the pole star, using the quadrant either as a gnomon for the compass or as a pylorus, to measure variation and eliminate compass deviation. Eighth: They were sensitive enough to the compass and its corrections to suggest they were taking great pains to ensure their variation recordings were accurate for their location on that day, and thus available for later charting of their variation. Ninth: They observed that the compass needle was deviating to the northeast, a clear indication that they were knew they were dealing with east variation and knew the difference. Also implied is the intimation that they knew how to apply it to obtain true directions. Tenth: If the translations were correct, they were taking their bearings by Polaris rather than by solar declination, a simple approach to eliminating deviation. However likely that is, the translation is again incorrect, interpreting the word bearing in lieu of the Spanish word observacione of altitude, which this obviously was. The correct understanding of an otherwise good transliteration is lacking here. Eleventh: The Dominguez/Escalante exploration party was extremely diligent and conscientious in their observations and in ensuring accurate information was confirmed and recorded properly. They may have been itinerant wanderers, but they were never lost! CONCLUSION: Part I To fully appreciate the activities of Spanish trails travelers, diligent historians should acquaint themselves with the rudiments of land navigation, and include some of the more obvious corrections and considerations that are frequently ignored or misapplied to trails records. When these are incorporated, an image of uncommon care and accuracy emerges, along with answers to some of the most nagging questions regarding a variety of decisions, concerns and solutions recorded in the success of the first truly scientific expedition of the American West. In all, seven latitude observations by solar meridian were recorded, another eight by Polaris. Each disclosed a true bearing that would accommodate compass correction for deviation and geomagnetic variation, providing the party with sidereal time, course guidance and positional date in an apparent attempt to chart longitude as a function of isogonic information. Celestial observations ceased or were no longer recorded after the Dominguez/Escalante expedition approached the Colorado River. Their last and only east-bound observation was at the ford of the Rio Colorado, or Crossing of the Fathers (near Page, Utah) on the Colorado River, November 7, 1776. Not only was the expedition in more familiar territory, but they had long since recorded the variation and no longer needed to concern themselves with recording the vagaries navigation Their observed positions, descriptive locations and recorded variation were now treasured commodities which they could share with subsequent borderland travelers.  Father Escalante Discovers Utah Valley Keith Eddington, Pageant in the Wilderness, Utah State Historical Society National Spanish Trails Symposium Southern Utah University, October 2007 Cedar City, Utah SPANISH TRAILS NAVIGATION Lecture II: Ephemeral based Land Navigation REFERENCES AND RESOURCES The Dominguez-Escalante Journal: Their Expedition through Colorado, Utah, Arizona, and New Mexico in 1776. Chavez and Warner. 1976. ISBN 0-8425-0037-5 Without Noise of Arms: The 1776 Dominguez-Escalante Search for a Route from Santa Fe to Monterey, Walter Briggs1976. ISBN 0-87358-141-5 Pageant in the Wilderness: The Story of the Escalante Expedition to the Interior Basin, 1776 Herbert Eugene Bolton, Utah State Historical Society, Salt Lake City, Utah, 1950. (Recommended Resource) Note: For those with a penchant for puzzles and an appreciation for educational challenges in their life (Soduku, stand aside), you can easily learn to calculate the earth position of the Dominguez-Escalante Party for any given observation, and have fun at the same time. Any of the following volumes are useable, new or old. H.O. No. 9 (any volume, any year) American Practical Navigator. Boditch H.O. No. 249, Volume II, (any year) Navigational tables to 45 degrees N. Latitude H.O. No. xxxx (any volume, any year) The Air Almanac, w/ reduction tables Celestial Ephemeris (any volume, any year, any source). (These volumes are available from the US Naval Observatory, Washington D.C.) 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