C Don Croner’s World Wide Wanders

Tuesday, October 21, 2008

Mongolia | Khentii Aimag | Khökh Nuur to Baldan Bereeven Khiid

Sometime during the night the incessant winds that had been dogging us since our arrival in Khökh Nuur died down and the sky cleared off completely. By four o'clock in the morning Orion was dominating the sky overhead. Daybreak saw a faultless dome of azure overhead and by the time we had finished breakfast temperatures were up in the 60s F. This was the kind of balmy end-of-summer weather I had been anticipating when I planned this trip. In high spirits we scarpered eastward toward our next destination, Baldan Bereeven Khiid.

This is Chingis Khan Country. From our starting point on the Terelj River, near where Temüjin, the young Chingis Khan, was living when the Merkits kidnapped his wife Börte, to the current day town of Binder, near where Temujin was born (according to one school of thought), farther on out to the east, stretches the territory where many of the events in the early life of the future World Conqueror took place. At a place called Tavan Tolgoi we stop to inspect some slabs of rock which local lore maintains were used by Chingis as pot supports at his fireplace when his ger was located here.

Purported pot supports at a “Chingis Slept Here” site

The stone slabs look surprising like the tomb coverings at the Monument to Kontuyuk, the advisor to the eighth century Khökh Turk Chieftain Kultegin. If they were Turk tomb coverings that of course does not mean Chingis could not have used them later as pot supports. Still later we pass by a place where Temüjin and his bosum buddy and later Arch-Nemesis Jamukha had their final falling out.

By lunch time we had arrived at Övör Elegiin Gol where Zevgee assured us there would be water. Much to Zevgee’s chagrin, however, the river was dry where the trail crossed it. We followed the riverbed downstream perhaps a thousand yards and soon came to a pool of water where the underground stream emerged. The water was fresh, clear, and icy cold. By the pool was a grassy glade surrounded by cottonwood trees and nearby dead brush offered plentiful firewood. The three essentials for a successful lunch—us, tülsh, and süüder (water, firewood, and shade)—thus provided for we unloaded our pack horses and threw out carpets on the grass beneath the largest cottonwood tree. We lounged on our carpets as Zevgee’s son-in-law Badmaa and grandson Bondogo fetched water and built a fire and in no time at all we were sipping delightfully fragrant Oolong tea (Shan Ling Xi from Taiwan, highly recommended). Tumen-Ölzii rolled out dough for fresh noodles and soon we were tucking into bowls of Guriltai Shöl—mutton soup with noodles. I hardly wanted to leave this idyllic spot, but finally we had a last bowl of tea and then packed up our horses and moved on.

By early evening we had reached Baruun Bayan Gol. Here, according to legend, was born Boorch, one of Chingis Khan’s boon companions. (See Paragraphs 90–93, 95, 99, 103, 120, 124–25, 156, 163, 172, 177, 202, 205, 209, 210, 220, 240, 242, 259–60, and 266 of the Secret History of the Mongols [also Kindle Version] for more on Boorch.) Camped on the sward by the river, with plentiful firewood nearby. Yunnan Gold tea followed by boiled sheep ribs and potato and cabbage soup heavily larded with stick-to-the-ribs mutton fat.
Yunnan Gold—the Perfect Complement to boiled sheep ribs and mutton fat

Just after dark breathtakingly luminous Jupiter appeared in the southern sky, just above the Sagittarius Teapot and just below the dimmer Sagittarius Teaspoon. The clear, cloudless sky soon revealed a full panoply of stars overhead: the constellations of Cygnus, Cepheus, and my personal favorite Cassiopeia to the northeast; the ever-glorious Scorpius off to the south; and of course the Seven Gods (Big Dipper) to the west. And then in the early hours toward morning magnificent Orion appeared. All and all a mindbogglingly gorgeous night. The next morning we moved out quickly, hoping to reach Baldan Bereeven Khiid by lunch time.

On the Road to Baldan Bereeven Khiid

We soon passed Khangalyn Nuur, where there is a monument to “Nature.” A sign on the monument implores people to protect the environment.

Monument at Khangalyn Nuur

Then we moved into the wooded foothills and began the climb to 4,698-foot Khangalyn Davaa.

Khangalyn Davaa

View eastward from Khangalyn Davaa. Baldan Bereeven Khiid is at the base of the mountain on the right edge of the photo.
We arrived at Baldan Bereeven just after noon. We were of course anxious to visit the monastery but first we set up camp, built a fire, and had a pot of Tie Kwan Yin Oolong tea. Tie Kwan Yin, the Iron Goddess of Mercy, is, as you probably know, the Chinese version of Avalokitesvara (Tibetan: Chenresig; Mongolian: Janraisag), the Bodhisatta of Companion, and thus a fitting drink in the environs of a monastery. In honor of our arrival Tumen-Ölzii also whipped up a big batch of Tsuivan, a much hallowed mutton and noodle dish which holds a special place of honor in the firmament of Mongolian cuisine.

Zevgee oversees the teapot at our Baldan Beereveen campsite

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Monday, June 23, 2008

Mongolia | Khövsgöl Aimag | Darkhad Depression #3

I rose just as the last stars were fading from the sky. Only Jupiter still glowed brightly over the southwest horizon. I kindled the fire, brewed up a pot of Puerh, and sat on my carpet drinking tea as the sky shaded from pearly gray to azure, with not a cloud from horizon to horizon. Two hours later everyone was finally up and we discussed your plans for the day. Batmönkh said the source of the Mungaragiin Gol was just over a low pass to the southwest, where Jupiter had been shining in the morning. The route to our next destination, the source of the Khoogiin, however, was over the pass at the head of the valley we were in, to the northwest. He now suggested that Bayarkhüü and I ride to the source of the Mungaragiin ourselves while he and the others stayed in camp. When we returned we would break camp and cross the pass to the northwest. This way we would not have to backtrack with the pack horses. I agree to this. Enkha announces that she does not want to miss out on anything and will come along with Bayarkhüü and me. That’s fine with me.
Valley of the Mungaragiin, with Belchir Uul in the distance

The low pass is only about a mile and a half away. To the left, down the valley of the Mungaragiin Gol, can be seen Mungaragiin Nuur (lake). At the valley, at its head, we get our first glimpse of 10,994-foot Belchir Uul, the highest peak of the mountains to the west of the Darkhad Depression. The source of the Mungaragiin Gol is right at the base of this mountain. Heading upstream, we ride by a small lake dotted with sea gulls. Had they come from the ocean? The Arctic Ocean is over 2000 miles away to the north. Further on is another small lake, this one still almost completely ice covered.
First Lake

Second Lake

We ride on another half mile to yet another small lake. According to my map, there are several small ponds still further on in the cirque directly below Belchir Uul, but there is no water flowing down the rocky ravine above the third lake we are on. The ponds apparently drain underground into this lake. Thus the outlet of the lake is, at least at this time of the year, the source of Mungaragiin Gol.
Source of the Mungaragiin, and one of three sources of the Yenisei
10,994-foot Belchir Uul

The Mungaragiin Gol, I have determined, is one of sources of the Yenisei River System. The Mungaragiin flows west of here and combines with the Guna Gol to form the Bakhmakh Gol, which we had crossed on the way to Batmönkh’s Ger. According to most sources, including Batmönkh, the Bakhmakh combines with the Altgana Gol, flowing in from the mountains to the east of the Depression, to form the Shishigt Gol, which then flows into Tsagaan Nuur. Some say the river known as the Shishigt Gol begins not at confluence of the Bakhmakh and Altgana but at the outlet of the Tsagaan Nuur. In either case, the Shishigt Gol flows out of Tsagaan Nuur and continues west to the Russian border, where it combines with the Busiin Gol and the Bilin Gol to form the Kyzyl Khem. The Kyzyl Khem then continues west to the city of Kyzyl, capital of the autonomous repubic of Tuva, where it combines with the Biy Khem to form the Yenisei proper. The National Geographic Atlas of the World lists both the Biy Khem and the Kyzyl Khem-Shishigt as the two sources of the main branch of the Yenisei (zoom in on the Lake Khövsgöl area of the map).

In 1995 I had hiked some sixty miles to the source of the Biy Khem in the extremely remote East Sayan Mountains in the Autonomous Republic of Tuva. A geographer at the Russian Academy Sciences in Irkutsk, in Siberia, where I was living at the time, had opined to me that this was the real source of the main branch of river known as the Yenisei, since the Biy Khem is bigger than the Kyzyl Khem in terms of volume of water where the two come together. But he allowed that the actual drainage area of the Kyzyl Khem system was larger than that of the Biy Khem so it too had a claim to be the source of the Yenisei. It should be pointed out that there is no scientific definition of the source of a river system, and almost any finding is open to interpretation; hence the long running dispute over the source of Nile, for example, which ended up with One Of The Disputants getting so frustrated he allegedly committed suicide.
Source of the Biy Khem -Yenisei in East Sayan Mountain, Tuva

In any case, it would appear that the outlet of the lake where we are now standing is at least one of the sources of the Yenisei. The location is N50º51.382' / E098.41.223' and the altitude is 7,802 feet. One atlas (no two agree) states the Yenisei branch of the Yenisei River System is 2537 miles long, although it neglects to mention which source it is using as the beginning of the river.

But the hydrology of the Yenisei River System is extremely complicated. Where the westward flowing Angara River, the big, fast-flowing river that runs out of Lake Baikal in Siberia, and the northward flowing Yenisei branch of the river system combine, the Angara is almost twice as big in terms of water volume. Thus by some definitions the ultimate source of the Yenisei River System would be at the beginning of the Angara branch of the system. The largest river flowing into Baikal is the Selenga (Selenge, in Mongolia). The Selenge, in turn, starts at the confluence of the Delger Mörön and Ider rivers in Mongolia. Since the Ider is bigger in terms of water volume its source would be the beginning the Yenisei-Angara-Selenge branch of the Yenisei River System. The Times [of London] World Atlas considers the Yenisei-Angara-Selenge the main branch of the river system and gives its length as 3448 miles, considerably longer than the Yenisei-Biy Khem branch. And it is not clear if the 281 mile-long Ider is included in this measurement. If not then this branch would measure 3729 miles long. This would be in line with the figure of 3742 miles given to me by the geographer in Irkutsk for the Yenisei-Angara-Selenge-Ider. In either case, it would rank as either the fifth or sixth longest river in the world, depending on which atlas we consult. In terms of water volume it is the Largest North-Flowing River in the world. In 1997 I visited Zavkhan Aimag and rode three days by horse to the source of the Ider, which I located near 11,873-foot Öndör Ölziit Uul, at an elevation of 9,880 feet, as described in my book Travels in Northern Mongolia.
Source of the Ider-Selenge-Angara-Yenisei, in Khangai Mountains, Zavkhan Aimag

As we sit by the outlet of the lake, the source of the Mungaragiin Gol, I explain all this to Enkha, who sweet girl that she is listens patiently and nods knowingly every so often to indicate that she is still listening. I suspect she does not have the slightest idea what I am talking about. Not everyone shares my fascination with the sources of rivers. Finally I ask Bayarkhüü if this lake has a name. He says not to his knowledge. I say that I will name this lake. This morning I had been teasing Enkha, calling her moo busgui (bad girl) since she had been the last one to get up every morning so far. I now christen the lake Moo Busgui Nuur (Bad Girl Lake). “I am not a bad girl! I am a good girl!” Enkha insists. Whatever, I say, you now have a lake named after you. Finally it is time to leave. Two hours later we are back in camp where Nergui has a kettle of Yunnan Gold and dinner ready for us. Now I have now been to All Three Sources Of The Yenisei River System.
At Moo Busgui Nuur, with Belchir Uul beyond

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Saturday, September 22, 2007

Mongolia | Töv Aimag | Horse Trip #2

At the last moment Zevgee’s son-in-law Badmaa decided to come along on the trip. He would help Zevgee with the horses. Thus there was six of us: Zevgee and his wife Tumen-Olzii, Badmaa, Saraa, Gunj, and myself.
Badmaa and his three boys
Our group at Biren Buren Pass, the Continental Divide of Inner Asia. East of here drains into the Kherlen River, in the Pacific Ocean Watershed, and west of here into the Tuul River, in the Arctic Ocean watershed.
Günj and Tumen-Olzii, who although sixty-five years old is always ready for a horse trip
Dropping down to the Tuul River from Biren Buren Pass
Crossing the the upper reaches of the Tuul River
From the Tuul River we headed up Khiidiyn Gol. Around two in the afternoon we stopped for lunch and I immediately brewed up some Yunnan Gold black tea. Both Saraa and Günj remarked on how good the tea tasted. This was in large part due to the remarkably pure and soft water found in Khiidiyn Gol. I had been here on a previous trip and had sampled this excellent water before. Saraa immediately decided to wash her hair, knowing that the soft water would bring out the luster of her locks.
Saraa doing a quick shampoo in Khiidiyn Gol

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