New Candidate in Arabia for
the Valley of
Lemuel
Refer to Maps 003 and
004 in the Map Room
First
published by the Foundation for Ancient Research and Mormon Studies (FARMS) in
the Journal of Book of Mormon Studies, Volume 8, Number 1, 1999
By George D. Potter
The Discovery[i]
Finding a river of running water in the ancient
land of Midian was not what Craig Thorsted and I had in mind on that day in
May1995. In fact, he and I were searching for one of the Arabian candidates for
Mount Sinai when our journey became one of unexpected discovery.
We had come to the oasis town of al-Bada’a to
explore the Wells of Jethro, the priest of Midian. To obtain authorization to
enter that area, we stopped at the mayor's office. The mayor sent one of his
supervisors to show us the sites and explain their history. The supervisor was
justly proud of the city's history and appealed to the Qur’an to relate the
stories of Moses, Jethro, and the town of al-Bada’a. Complimenting me on my
knowledge of the Qur’an, he said that if we were really interested in Moses, we
should visit the Waters of Musa (Moses) near Maqna. Maqna is a small, isolated
village that lies 20 miles west of al-Bada on the Gulf of Aqaba.
The official in al-Bada’a explained to us that,
according to local tradition, Maqna had been the first camp of Moses after the
Israelites had crossed the Red Sea at the mouth of the Gulf of Aqaba. He said
it was at the Waters of Moses that the Prophet Moses had touched his staff to
the rock and 12 springs gushed forth, one for each tribe (see Qur-an 7:160).
The official feared, however, that the springs might have dried up because in
recent years the government had placed pumps on all the natural wells in Midian.
When we reached Maqna we stopped at a restaurant to inquire about the
springs. Americans must be a rare sight in this remote village, for our truck
was immediately surrounded by curious Arab children who shouted –“Ameriki.”
The supervisor in al-Bada’a had given us the name of a contact man in Maqna who
would show us the Waters. Everyone, it seemed, knew the man. But he was away
from the village.
We decided to inquire at
the first “official" building we could find. We came to a large complex
that turned out to be a Saudi coast guard station. From the gate we were led to
the captain's salon for an interview. After a series of questions, the captain
granted us permission to visit the Waters of Moses. We learned from him that
the place was 12 miles to the north, along a restricted coast guard patrol road.
He gave us written permission and promised a military escort.
(It wasn't until my
fourth trip to the area, 3½ years later, that I finally discovered that the
Waters of Moses we had heard about in al-Bada’a were actually located at Maqna
itself. By a turn of events, the captain had directed us to the wrong spot
farther north along the coast. Some may say that it was by pure luck that we
came, not to the traditional Waters of Moses, but to another source that we
might easily never have seen. I see the experience as providential. By “mistake,”
had we unintentionally stumbled upon the river Laman and the valley of Lemuel?)
As we drove north from
Maqna, the scenery was typical of what I had seen along the shores of the Gulf
of Aqaba of the Red Sea-lifeless sand plains and barren rocky valleys. The
landscape reminded me of Moses' words: “that great and terrible wilderness,
wherein were fiery serpents, and scorpions, and drought, where there was no
water” (Deuteronomy 8:15). Nephi's mention of a river valley, possibly with
fruit trees, seed-bearing plants and grain, seemed totally out of place (see 1
Nephi 2:6; 8:1). Yet, this shoreline is the general area where the valley of
Lemuel should be found.
Eight miles north of
Maqna, we came to our first surprise. the southern end of the mountain range
that here forms the shoreline seemed to drop directly into the waters of the
Gulf of Aqaba. There was just enough room for the coast guard dirt road to pass
between the giant cliffs on the right and the watery gulf on the left. We
followed the narrow road for another four miles, with waves occasionally
breaking over our path. Rounding the base of a cliff, we came upon a truly
spectacular sight. A magnificent narrow canyon just ahead of us ended in a
palm-lined cove. The brilliant blue shades of the clear gulf waters and the sky
framed the scene.
We decided to walk up the
spectacular wadi or canyon. After 3¾ miles it opened into a beautiful oasis
with several wells and three large groves of date palm trees. However, what
caught my interest most was the stream that started in the canyon near its upper end and ran down the
wadi virtually all the way to the sea. (see photograph).
The small desert river appeared to flow
continually night and day, year after year. At the time the Book of Mormon was
first published, the claim that a river ran in arid northwestern Arabia could
not be checked. Western explorers did not venture into this remote area until
well after 1830.[ii] Today it is a different matter. Geologists have
thoroughly explored Arabia in search of oil and water. The Saudi Arabia
Ministry of Agriculture and Water, with the assistance of the U.S. Geological
Survey (USGS), has spent the last 44 years surveying the kingdom's water
resources. Their studies have involved seismic readings, surface and aerial
surveys, and satellite photo analysis. But the findings of the scientists
regarding the possibility of an above-ground river have not been encouraging.
Rather, they concluded that Saudi Arabia “may be the world's largest country
without any perennial rivers or streams."[iii]
Yet Lehi spoke of “a river of water”
that “emptied into the Red Sea” and was “continually running" (1 Nephi
2:6, 9). How could we reconcile Lehi's description and the geologists'
findings? It might be thought that the
climate was wetter in Lehi's time. But that notion runs against both what
little we know about the region from the Bible (e.g., Exodus 3:1) and the known
meteorological history of the Near East.[iv] Scientists say of Arabia: “The past 6000 years
have been marked by... arid conditions, similar to those of the present.”[v] Hugh Nibley also commented, “though
some observers think the area enjoyed a little more rainfall in antiquity than
it does today, all are agreed that the change of climate has not been
considerable since prehistoric times-it was at best almost as bad then as it is
now.”[vi]
What can we reasonably say about the river
Laman from the Book of Mormon? First,
the river was quite surely not a major stream.
Otherwise a permanent settlement, and a name, would have accompanied
it. Second, Lehi gave the river a name,
so it probably had no name that he was aware of (see 1 Nephi 2:8). It is hard
to imagine that any substantial flow of water in the Near East would go unnamed,
implying that the stream did not amount to much and probably was a localized
phenomenon. Third, the river Laman was in the wilderness (see 1 Nephi 2:6), a
place generally devoid of people.
Fourth, the waters of the river Laman emptied into the sea (see 1 Nephi
2:9) in the area where Lehi had camped, which must have been at the north end of the Red Sea, near the Gulf of
Aqaba. Fifth, Nephi described the stream as “continually running” (1 Nephi
2:9). Finally, the river Laman ran
through a geographical feature that Lehi called the valley of Lemuel (see 1
Nephi 2:6-10). Our initial visit
confirmed that the stream in the canyon met at least all of the physical
criteria.
The Hebrew term for river enters into our evaluation of this stream
because of Nephi's account. There are several Hebrew words which Nephi could
have used (see 1 Nephi 2:6; etc.). Most of them refer to any running stream.[vii] These terms for river could mean
seasonal waterways that fill with water only after a storm, such as the
"River of Egypt" (Wadi El-'Arish). They could also refer to large,
continually flowing currents such as the Euphrates River (see Genesis 15:18).[viii]
Whichever word Nephi used that came into English as “river” could
denote a large stream, a small continuously flowing one, or a seasonal flood.
His choice of the phrases “river of water” and “continually running;” however,
seem to point to a stream that flows more or less all the time, at least
throughout the period that they camped nearby.
What were the characteristics of the valley through which the river
Laman flowed? First, Lehi described it as "firm, steadfast, and immovable"
(1 Nephi 2:10), terms that hint at impressive geological features. Second, the
valley was located within three-day's walk or camel ride beyond the northeast
tip of the Red Sea (see 1 Nephi 2:5-6). Finally, the valley of Lemuel reached
the Red Sea for Lehi observed the mouth of the river emptied into the sea (see
1 Nephi 2:8.) So it was not strictly an
interior valley; rather, it reached the seashore.
As with the stream, our first observations were that the valley we had
found met these conditions. The fact that the stream and canyon fulfill the
conditions reported by Nephi for the "river of Laman" and the
"valley of Lemuel" convinced
me that we may well have indeed discovered these Book of Mormon landmarks. Nothing my colleagues and I have learned
subsequently has given us reason to change that view.
Characteristic of the Valley
The grandeur of the valley is difficult to describe in words or even
portray in photographs. It is a narrow
gorge cut through a massive granite mountain.
It consist of three sections; the upper valley (or the Waters of Moses),
the canyon of granite, and the low canyon.
The upper valley constitutes an oasis that lies at the south end of a
twelve-mile long wadi – known locally as Wadi Tayyib al-Ism – that leads down
from the north (see map room). The
upper valley sits like a pleasant jewel, spread out over approximately one
square mile with several hundred palm trees and 12 wells that local residences
call the Waters of Moses.
The upper valley ends as the long, descending wadi veers west and runs
against the eastern granite cliffs of the shoreline mountains. But rather than forming the usual impassable
barrier, the coastal mountains have been breached by a narrow canyon. This deep fracture in the granite mountain
border provides a passage to the sea; I call it the canyon of granite. Tim Sedor, a colleague in the exploration
effort, has surveyed the length of this section of the Wadi Tayyib al-Ism to
the Gulf of Aqaba; he concludes that it is approximately 3 ¾ miles.
Flash floods are a winter-time danger in this part of Arabia. If the family of Lehi and Sariah had camped
here in the hot summer months, they could have stayed in the shade of the
canyon. During the rainy winter months,
however, campers would wisely move out of the canyon up to the much wider oasis
that the upper valley offers.
Climatically the shade provided by the steep walls of the canyon of
granite provides a pleasant environment year round, even during the terrible
heat of an Arabian summer.
Although the trip from Jerusalem was perhaps the least difficult portion
of the trek of Lehi’s group, party members still murmured. Laman and Lemuel thought they would die (see
1 Nephi 2:11). Even in springtime,
temperatures in Arabia reach over 100oF. The murmuring of the sons could well have been caused by exposure
to the stark sunlight and extreme temperatures. A survival expert who advises the Saudi military has offered some
insights into the environmental difficulties that would have faced Lehi and his
family as they crossed this land. Based
on his experience, he advises downed pilots in the desert to first find shelter
from the heat, next to look for water, and only then to seek food. Within hours, he notes, the midday Arabian
sun will kill a person who cannot find shade.
Maximum daily temperatures average between 115oF and 125oF
during the summer months in this part of Arabia.
When considering the cruel climate, one can begin to appreciate just how
difficult the journey from Jerusalem must have been, and seemed. This would have been especially difficult
for city dwellers from Jerusalem, particularly if this was their first exposure
to severe desert conditions in summer.
The canyon of granite would have offered an ideal place in which to wait
out the summer months before continuing.
At the same time it was off the main route southward, in case Nephi’s
part in the death of Laban had become known to pursuers.
The final section of our valley of Lemuel is the lower canyon and the
beach. The granite canyon opens out
into a flat gravel floor just a few feet above sea level. This level area at the mouth of the canyon
is about 3/8 mile long. This is the
most impressive section of the canyon.
Here the height of the canyon walls raises approximately 2,000 feet
straight up from the canyon’s floor.
The lower canyon provides important clues which tend to confirm that
this could be the valley of Lemuel.
First, Lehi found that the stream in the valley “emptied into the Red
Sea,” that is, into the Gulf of Aqaba (1 Nephi 2:8). The walls of our candidate for the valley of Lemuel end within 60
feet of the waters of the gulf.
Second, though the valley carries a stream to the sea, when Lehi first
came into his valley (necessarily from its upper end, not from the coast) he
apparently could not see from his camp that the river emptied into the sea; at
least that is implied by 1 Nephi 2:6 and 9.
Our candidate for the valley is less than four miles long, yet its
towering walls permit seeing the Red Sea only during the last 375 yards as one
descends to the coast. The beautiful
palm-laden beach cove that one finally encounters is a spectacular scene.
It may be worth noting that when Lehi’s party was preparing to leave
their valley, Nephi wrote of the Lord’s gifts to them, including provisions
(see 1 Nephi 16:11). In this spot such
provisions might have included dried fish from the sea, dates and berries,
found primarily in the upper valley, date pits (Arabs today make a coffee
substitute from ground date pits), grain, and of course drinking water from the
river.[ix]
One
may ask how easily a person can reach the canyon and stream when traveling from
the northeast tip of the Red Sea, the direction of Jerusalem, where modern
Aqaba sits. From Nephi’s description,
we know that after his family reached the Red Sea they continued another three
days before making camp (see 1 Nephi 2:5-6).
A reasonable estimate would be that they traveled between 45 and 75
miles during those three days, averaging 15 to 25 miles per day.[x]
The valley
we are describing lies just over 70 miles (on the ground, not in a direct line)
south of Aqaba, clearly within the limits of our estimate on basis of Nephi’s
record.
A
traveler can come to the valley from the north by either of two routes (see
map). The most direct takes a person
south from Aqaba 44 miles along the coast.
Here one reaches a 6,000-foot mountain range that blocks further
coastwise travel. So it is necessary to
turn eastward near Bir Marshah and climb up through an eight-mile long wadi,
finally cresting a ridge at about 1,500 feet elevation. Both people and pack animals can easily
follow this route. From this point, keeping the coastal mountains to the right
(west), a person travels south 20 or so miles into the long valley mentioned earlier,
which leads down to our upper valley and the head of the granite canyon. The distance from Aqaba to the canyon is
almost exactly 74 miles.
Another route, well-traveled in ancient times, follows the modern
highway south from Aqaba. It runs up
Wadi Umm Jurfayn and then south between mountain ranges to the town of
al-Bada’a. About midway through the
long mountain pass, one can turn west and south to reach the long, deep valley
and on to our upper valley. But this
route adds significant distance.
The river Laman might have had some name in Lehi’s time, but it would
have been known only to the local residents.
Brown notes that “in a desert clime all arable land and all water
resources have claimants.”[xi] How might
Lehi have acquired the right to camp in the valley that was likely controlled
by a local tribe? There are several
reasons why this may not have been a serious problem for Lehi. First, Lehi had evidently been a wealthy man
and, though he left his gold and silver in Jerusalem, his family probably
carried among their provisions some items that could be exchanged for temporary
camping privileges. Another possible
scenario is that Lehi’s group appeared small and nonthreatening enough that the
locals required no payment of them. The
hosts may even have pointed out to Lehi where he could find water and a
campsite out of their way in the side canyon whose lower reaches they did not
use themselves. (Nephi did not write
that his family “found” a river, but only that they pitched their tent next to
it; see 1 Nephi 2:6). This latter
possibility is enhanced when we note that Lehi apparently brought no sheep or
goats with him into the wilderness. If
that was so, the local shepherds probably did not consider the Lehites as a
threat to their resources since they had no flocks. In other words, Lehi many have been treated as a welcomed,
noninvasive tenant who, best of all, could pay, even if only nominally. (In order to offer sacrifice, by the way, he
would have needed to buy a lamb or sheep from his host).
A
third possibility is that there were no inhabitants in this valley. That is true today. Except for a stone box constructed in the
earth by Bedouins, evidently for keeping valuables safe, and a few scattered
remains, whose date is not determined, there is little sign that a valley has seen
long-term residents. [ruins of campsite
subsequent to this article, we found had been dated to late Iron Age – well
within Lehi’s time period] The soil
appears unfavorable for farming.
Besides, the narrowness of the river valley severely limits its use for
agriculture since the area of land available to cultivate is not enough to
support a significant resident population.
If the area was empty of people except for nomadic Bedouins, then Lehi
was in no way beholden to locals.
The question we posed while standing in the canyon of granite was: Does this desert river flow “continually” as
1 Nephi 2:9 says? Does it flow night
and day, 365 days a year?[xii]
I could
answer affirmatively only after our third excursion to the valley in November
1996. It had just rained for six
straight days before our arrival – a freak storm, the heaviest in years. But this storm provided a reverse key of
sorts.
On our first and second visits we witnessed the river during and just
after the winter rainy season. But in
November 1996, after a seven-month dry spell, we were finally able to ascertain
that the stream does flow constantly.
The key came not from the flow at the moment we were there, which could
have come from the recent rains, but from the flora in and around the
river. We had earlier discovered the
river’s source to be a spring some 600 feet down the canyon of granite from the
upper valley. On our prior two visits,
the grass, weeds and herbs surrounding the springhead had been a lush
green. On our third visit, they were
still green even after seven months of no rain. This vegetation could not have survived those seven months unless
the spring were feeding the river “continually.”
I
have now visited the valley in the months of April, May, November, December and
most recently, January. Colleagues have
visited in July and August. We have
observed that the volume of water in the river seems rather constant throughout
the year (even though from 1995 to 1999 the volume seems to be decreased
perhaps 50 percent due to the continued effects of pumping the water in the
upper valley). We have also observed
throughout the year that vegetation flourishes in the canyon where the river
runs, and moss and algae line the banks of the stream.
The spring that feeds the river comes from an underground reservoir
system. Dr. Wes Garner,[xiii] our consulting geologist, painted the following
picture of the system: When the
occasional rains fall in the long wadi to the north, they are trapped in the
sands. This watershed of sand runs
southward for 20 miles until its downward course to the sea is blocked by the
granite underpinnings of the towering cliffs to the west. (Richard Wellington, my writing and
exploring companion, has estimated the size of the watershed to be
approximately 105 square miles). This
subterranean rock runs deep beneath the surface forming a dam. The subsurface waters are thus trapped at
the upper end of the canyon in an underground reservoir. The canyon and its stream run westward from
the area of this underground reservoir for 3 ¾ miles, starting at an elevation
of 750 feet and ending at sea level in the Gulf of Aqaba. The floor of the canyon descends steadily. Within a few hundred feet, a spring begins to
flow as the canyon floor drops to the level of the underground reservoir. The waters form the small river that runs
above ground almost the rest of the way.
At the point where the river comes to a level grade in the canyon floor,
it runs just underground, leaving the soil moist. But soon the grade increases in its descent, and the river
reappears. It is last seen as it
reaches a gravel bed in the lower canyon about 3/8 mile from the gulf where it
feeds a well used by the coast guard post a short distance away. (If Lehi’s camp were upstream a bit from the
mouth, in the shade of the precipitous cliffs, as we suppose, the stream would
still have appeared to him to flow right into the gulf.)
It should be remembered that we were informed that the government had
placed gasoline pumps on all the wells in the area. As a result, the supervisor whom we met in al-Bada’a indicated
that the wells and springs in the region were drying up. We found this to be the case with the wells
in the upper valley. Our geologist, Dr.
Garner, confirmed to us that a lowering of the water table due to pumping could
cause the river to dry up in the future.
There are at least two indications that a substantial river has flowed
in the canyon for a very long time.
First, there is evidence of significant erosion of rocks and the lower
canyon walls. Second, water-laid
calcite deposits that are found on the valley floor are at times 15 to 20 feet
wide, much wider than the stream bed.
At places in the canyon, one can find such deposits that have formed at
higher layers of the rocks. We have
measured these deposits 11 inches higher on the rocks than the level of the
stream today. These observations point
to the flow of a larger stream in the past, evidently long before the pumps were
installed.
As I noted, the river flows under a gravel bed for the last 3/8 mile as
it approaches the Gulf of Aqaba. The
reason the river does not reach the Red Sea today is simple. The elevation of the floor of the canyon is
not the same as it was at the time of Lehi.
According to geologist Garner, in Lehi’s era this lowest part of the
canyon was submerged by the Red Sea.
Where the river ends today was below the surface of the Red Sea in
ancient times. As the continental
plates have moved along the Great Rift Valley that forms the Gulf of Aqaba,
they have pushed the eastern plate upward by one to five centimeters per
year. During the 2,600 years since Lehi
camped in the area, the canyon floor has risen out of the Red Sea, perhaps as
much as 200 to 400 feet. Thus, not so
long ago, the flat lower part of the canyon would have been below sea
level. Therefore if the river flowed at
the same rate in Lehi’s time as it does today, it would have reached all the
way to the waters of the Red Sea. In the
lower part of the canyon, the smooth stony floor of the canyon and the eroded
cavelike undercuttings of the cliff seem to confirm that the lower part was
once a sea floor rather than a river bed [erosion cause by wave action]. The ancient river, carrying a significantly
higher volume of water, would have run the entire distance to the Red Sea.
I
have escorted over a dozen people into the valley. Several others have made their own way there based on my
directions. Are we witnesses of the river
Laman and the valley of Lemuel? In my
view, the characteristics of the site are compelling evidence that this is
so. In the four years since the
discovery, I have surveyed the entire Arabian shoreline of the Gulf of Aqaba
and the valleys that open onto it. With
the exception of the springs at Maqna, which are not in a valley, I have found
only rocky valleys almost entirely devoid of vegetation and with no flowing
water. Although I have not conducted a
thorough survey of the entire region, I have so far found no other place within
three-day’s walk of the tip of the Gulf of Aqaba that is as inviting as these
Waters of Moses.
I
have drunk from the pure spring-fed waters of what I believe is the river
Laman. From the staggering heat of 120oF
plus, I have walked into the cool confines of a deep canyon that I believe is
the valley of Lemuel. On the shore of
the Gulf of Aqaba, my tent has been blown over by the torrentlike winds that
swirl each night along the shoreline. I
have stood in awe of the force required to split open a pass through the
four-mile wide granite mountain barrier to form this canyon refuge, with
towering walls that could protect those camped in its shadows from the heat and
the tempests and sand storms that blow into Arabia from the Sinai
Peninsula. I now seem to sense why
Isaiah’s words were so relevant to Nephi’s family: “And a man shall be as an hiding place from the wind, and a
covert from the tempest; as rivers of water in a dry place, as the shadow of a
great rock in a weary land” (Isaiah 32:2).
Here the handiwork of the Lord appears at every turn and reminds me of a
passage from the Qur’an: “Whithersoever
ye turn, there is the presence of God…all that is in the heavens and on the
earth; everything renders worship to Him” (Qur’an 2:115,116).
[i] My efforts, of
course, tie to the work of others, Earlier Latter-day Saints who attempted to
visit the areas that may have been inhabited by Lehi and Sariah including Lynn
and Hope Hilton, In Search of Lehi’s Trail (Salt Lake City: Deseret
Book, 1976), 62-75. My suggested
candidate lies north and west of their choice.
Before them, Hugh Nibley offered the view that Lehi had camped “not far
above [north of] the Straits of Tiran” near “Mt. Musafa or Mt. Mendisha,” Hught Nibley, Lehi in the Desert, The
World of the Jaredites, There Were Jaredites, 2nd ed. (Salt Lake
City: Deseret Book and FARMS, 1988, orig. publ 1959), 85. Actually, Mt. Mazhafa (Musafa?) is the
granite mountain that forms the north side of the canyon that is my candidate
for the valley of Lemuel. One must also
consult the works of Eugene England: “Thought the Arabian Desert to a
Bountiful Land: Could Joseph Smith Have Known the Way?” in Book of Mormon
Authorship, ed. Noel B. Reynolds (Provo, Utah: BYU Religious Studies Center,
1982), 143-56, and Paul Hedengren, The Land of Lehi: A Book of Mormon
Geography (Provo,Utah: Bradford and Wilson, 1995) 3-6. Hedengren suggests that Lehi pitched his
camp in Wadi al-Nuwaybi, 18 miles south of Aqaba.
[ii] Andrew Taylor,Traveling
the Sands, Sagas Of Exploration in the Arabian Peninsula (Dubai:
Emirates Printing, 1995), 19-31.
[iii] Ministry of
Agriculture and Waters, Kingdom of Saudi Arabia United States Joint Commission
on Economic Cooperation, the U.S. National Graphic Center, and the U.S.
Geological Survey, Water Atlas of Saudi Arabia (Riyhad: Saudi
Publishing, 1984), xv.
[iv] James Sauer,
“The River Runs Dry”, Biblical Archaeology Review 22/4 (July/August 1996). Testing by taking core samples from dry
desert lakes and by measuring tree rings has only been done in the Egyptian
desert at latitudes compatible with the Arabian peninsula. Studies show a clear shift toward a drier
environment several thousand years ago with very few periods of greater
moisture. See the summary by Karl W.
Butzer, “Environmental Change in the Near East and Human Impact on the Land,”
in Civilization and the Ancient Near East, ed. Jack M. Sasson et at.
(New Your: Scribner’s Sons, 1995), 1:123-51)
[vi] Nibley, Lehi
in the Desert, 50-51.
[vii][vii] See William L.
Reed, “River,” in The Interpreter’s Dictiionary of the Bible, ed. George
A. Buttrick et al. (Nashville: Abingdon, 1962, 1976), 4:100-101.
[viii] The Hebrew
term nahar is used for both rivers mentioned in Genesis 15:18. On the river of Egypt as Wadi El-Arish or
Nahal Bezor, which are seasonal streams, see Manfred Gorg, “Egypt, Brook of,” and “Egypt, River of,” in Anchor Bible
Dictionary, ed. David Noel Freedman at al. (New York: Doubleday, 1992),
2:321,378.
[ix] Currently one
can find grain as well as three varieties of dates in the upper valley or in
the canyon, (see 1 Nephi 8:1)
[x] Nigel Groom,
Frankincense and Myrrh: A Study of the Arabian Incense Trade (London: Longman,
1981), 173, 211, notes that a loaded camel travels, “slightly less than 2.5
miles an hour” and “rarely exceed(s) 25 miles” per day.
[xi] S. Kent Brown,
“A Case for Lehi’s Bondage in Arabia,” JBMS 6/2 (1997); 206. Nibley made a similar point, see Lehi in the
Desert, 66.
[xii] There has been
discussion about whether the river Laman was seasonal or whether it flowed year
round. Nibley holds to the view of a
season stream (Lehi in the Desert, 76,78,79-81). The Hiltons share the same view (In Search of Lehi, 64-65). From studying maps, Hedengren maintains that
the “lower portion” of wadi al-Nuwaybi has a “continual flow” (Land of Lehi,
3-6; quotations are from p. 4) Of
course Lehi’s party did not, in all probability, stay there anything like a
full year. “Continually” may only refer
to the period of their observation. But
if, as suggested earlier, there were there in the hot season, then surely the
stream would have run in the winter also.
[The problem with all these theses is that today no such seasonal
streams flow, even during the strongest rains, and there is no continually
running stream in wadi al-Nuwaybi.]
[xiii] Retired
professor of geology, King Fahd University Of Petroleum and Minerals, Dhahran,
Saudi Arabia.