Damavand

Bolourchi clarified: "We don't have enough information to foresee the potential volcanic movement of Damavand precisely. The liquefying of the ice top could expand temperatures and trigger a volcanic emission. Geographical proof has demonstrated that the first and last time that Damavand ejected was two million years prior and 7,000 years back, separately."

Damavand Aerial View

"Satellite pictures demonstrate that Damavand is persistently evolving. It is protected to accept that these land occasions would make the mountain emit one day soon," Bolourchi noted. "The administration does not have a far reaching crisis the executives intend to manage catastrophic events including seismic tremors, streak floods, and volcanic emissions."

The GSI has been pushing – futile – for the production of the Damavand national volcanic research focus since 2000. The administration hasn't given the GSI authorization to set up office on the land apportioned for this reason. Researchers have as of late had the option to introduce seismometers at the base of Damavand to gauge the ground movement brought about by quakes and volcanic emissions.

"There are in excess of 30 towns around the base of Damavand. The administration doesn't have a crisis clearing plan in the event of a volcanic ejection. The crisis administrations ought to have the option to shut down Road 77 (Hraraz Road) — which interfaces Tehran toward the northern hilly areas — to deflect an enormous scale debacle," Bolourchi said. He included: "A volcanic emission on Damavand could be considerably more dangerous than the one on Mount St. Helens in the U.S. in 1980."

With an elevation of 5,670meters (18,600 feet), Mount Damavand is the most noteworthy top in Iran. It is 70 kilometers (44 miles) upper east of Tehran, amidst the Alborz mountain extend, which stretches along the whole western and southern shore of the Caspian Sea. Source Keyhan Life. MDIC19JUN04A

Scientists examining puzzling flood at Iran well of lava base, Damavand Mountain in Iran, a dozing spring of gushing lava in Iran. In August 2018. French and Iranian specialists have collaborated to discover what set off the puzzling ongoing blaze flood in Gazanak town at the foot of mount Damawand, 120 kilometers (75 miles) upper east of the capital, Tehran.

At 5,670 meters (around 18,600 feet) above ocean level, damavand is the most astounding top in the Middle East and the most astounding spring of gushing lava in Asia. The Iranian-French group is concentrating ongoing movement inside Damavand's fountain of liquid magma, said prestigious Iranian seismologist Mehdi Zare', with expectations of increasing some knowledge into what caused a monstrous flood in August of water starting from the mountain that immersed the town of Gazanak underneath.

The flood happened all of a sudden when there was no overwhelming precipitation anyplace close to the hazardous situation. This video cut demonstrates the abrupt blaze flood descending the mountain in August. At the time, a few specialists pointed at environmental change and a worldwide temperature alteration, demanding that it had prompted an abrupt softening of the snow and colossal ice sheets on Damavand, at last causing the flood.

The Iranian-French group is right now gauging that hypothesis too, Zare' says. In the interim, Zare' and his French partner from the college of Strasbourg, Jacques Hinderer, are additionally attempting to get some answers concerning the ongoing unexplained attractive and gravitational changes on Volcano Damavand. Educator Zare' has over and over advised that Damavand's area so close to the Iranian capital and amidst such a thickly populated territory needs steady observing, as it could eject whenever.

The last known ejection of Damavand's well of lava was in 5,300 B.C., yet the danger of another emission is exacerbated by Iran's incessant quakes and extreme seismic action. Tehran itself sits on soil, for the most part made up of magma stores from Damawand's ejections previously. In 2005, the UN evaluated Iran as the main nation on the planet for quakes, regardless of whether estimated in force, recurrence, or the quantity of losses. MDIC19MAY12J

Mount Damavand is a gigantic stratovolcano. This superb fountain of liquid magma is situated in Iran among Tehran and south of the Caspian Sea amidst Alburz Mountain Range. This immense spring of gushing lava lies between the Eurasian and the Arabian structural plate impact zone and is the most elevated heap of the Middle Eastern district.

Spring of gushing lava Damavand summit hole is around 200-meter-wide and 30 m profound, it contains a 40-meter distance across solidified lake in the base. There is no lasting icy mass on the south face (other than a little icefall) in light of the fact that the atmosphere is excessively dry. Be that as it may, there are patches of solidified enduring snow.

Hike Damavand Iran
Cloud Cap view from Nava Village
Phot by Ardeshi Soltani

Damavand Mountain in Iran has incredible fumaroles vent close to the summit hole. The Powerful fumaroles vent close to the summit cavity makes some trouble for climbers. No authentic emissions have happened at this incredible well of lava in Iran.

The last ejection and most recent movement happened around 7000 years prior and delivered magma streams from the summit hole that spread the western flank. It has dynamic fumaroles just underneath the summit, fumaroles vent just beneath the summit transmits hot steam and hot SO2-rich gases.

Damavand has just couple of flank vents. There is an amazing fumaroles vent on the south course close to the summit cavity which discharges hot steam and SO2-rich gases. Dynamic fumaroles at the summit propose that the well of lava is as yet dynamic. Just underneath the summit, there are squares of unadulterated Sulfur and expansive Sulfur-bearing squares. Sulfur stores are available on the encompassing inclines

Lar Dam (Persian: سد لار dismal de lār) is a dam situated at the foot of Mount Damavand in Amol area, Mazandaran, Iran. The dam is situated inside the ensured Lar National Park and arranged only 70 kilometers upper east of the capital and the most crowded city of the nation, Tehran. The main role of the dam is metropolitan water supply to Tehran yet preceding the water achieving the city filtration plant, it is utilized to control the Kalan and Lavarak Hydroelectric Power Stations, with a joined introduced limit of 162.5 MW.

The development started on the dam in 1974, and finished four years after the fact in 1981. At the point when the repository started in 1980, spillage was found downstream. The spillage is expected to a karst establishment. The establishment was grouted from 1983 until 1989 with no achievement. With the populace development happening in Amol, there was a requirement for more water and vitality. The perfect spot for the dam was over the Lar stream, in the upper east area of the city, at the raised statures of the Kalanbasteh mountain on the incline of Damavand Mountain. The territory is called Polour, and tasks started in 1984.

One of the goes for structure the Lar Dam shut to Damavand, was to supply some portion of Amol with drinking water; it was unrealistic at first to work the dam at its ostensible limit, on account of a water leakage issue. Water put away in the dam's repository is first exchanged to the Kalan Power Station (35°48′24.87″N 51°47′29.46″E) at that point to the Lavark Power Station (35°48′34.97″N 51°44′54.67″E), a separation of 3 kilometers from the Latyan Dam's store, through the 20-kilometer-long Kalan burrow (3 meters in size). After power age, the water joins and feeds the Latyan dam's repository. The Kalan Power Station was dispatched in 1998 and the Lavarak in March 2012 and July 2013.

Lar Lake is situated at the foot of Mount Damavand
Lar Lake view from Camp 3 Bargah Sevom
Phot by Ardeshi Soltani

Uncontrolled development and extension of Tehran made a circumstance where the current water assets at Karaj, Latyan and Lar dams close fountain of liquid magma Damavand and the profound wells which should be abused just in the amid the pinnacle water utilization period. These were never again fit for gathering the city's water request, so unavoidable reflection from ground assets began to increment in a way that at the current circumstance, the amount of bored profound wells has added up to 230 rings. Truth be told, from 1997-2000, it had been methodical preoccupied, 317, 289, 374 and 357 MCM (million cubic meters) of water from groundwater assets of the city.

Lar lake from Damavand mountain.
The lake is 84 km upper east of Tehran, and because of its vicinity to Mount Damavand it makes a cool and charming atmosphere just as lovely scenes. The lake gives the degree to water sports, for example, swimming and waterskiing.

Mt. Damavand is a brilliant symmetrical cone well of lava with a restricted cold summit. It would appear that Fujiyama in Japan. Demavand lethargic spring of gushing lava lies around 80 kilometers north-east of Tehran in the northern Persian level. Damawand's white pinnacle and its lovely cloud top is the most alluring sight of Iran mountains.

Snow covers the whole Damavand Mountain in winter and the upper parts and slops in spring and fall. Damawand Summit is snow-topped a while a year. Ice and solidified snow stay all the year on the north face icy masses called Sioleh and Dobi Sel, the north east ice sheet Yakhar and furthermore the south course Icefall called Abshar Yakhi.

Every year Damawand is visited by numerous tourists, mountain visitors and climbers for climbing, trekking, mountaineering and ski visiting. The prominent trekking beginning stage is Polour Resort in the Polur Village on the south face, it is an alternate route to the Damavand and an agreeable spot for acclimatization and settlement. Climbing season is from mid-June to mid-September, or mid-May to mid-October for progressively experienced climbers.

Mount Damavand is encompassed by numerous pinnacles and edges of the Albroz Range, yet it unrivaled tallness (5671 meters) is obvious from numerous kilometers away. In a decent perceivability when the air is clear it very well may be seen from Tehran and from far away in focal part, Karkas Mountains and the incomparable Salt Desert and from north of Iran, the Caspian Sea.

Damawand is an outstanding image of Iran and has an extraordinary spot in Iranian legend, fanciful stories, workmanship and photography. As a general rule it is a brilliant torpid well of lava that conveys some sulphuric smoke. Numerous legends and stories are identified with Damawand Iran.

The most punctual endeavor to climb Damavand mountain was made by unknown neighborhood Iranians. They climbed normally to gather Sulfur from the top for business purposes. The primary recorded rise has a place with an English voyager called W Taylor Thomson in 1837.

Well of lava Damavand is a lethargic fountain of liquid magma that last ejected around 6000 - multi year prior. In the verifiable occasions there has been no recorded emission of this fountain of liquid magma. Some trusts this mountain is a wiped out spring of gushing lava. In any case, there is sufficient evidence, for example, warm hot springs on its lower inclines and incredible fumaroles vent close to the summit cavity that demonstrate Damawand Volcano is torpid. On the top there is a summit Crater, around 150-200 meters over, with loads of yellow rocks containing sulfur and pumice stones.

Hike Trek Ski Tour Damavand Peak

Damawand Quick Facts
Rise: 5671 meters, 18,605 feet.
Noticeable quality: Ranked sixteenth
Rank: Highest fountain of liquid magma in Asia, the second most noteworthy spring of gushing lava in the northern side of the equator.
Area: North-East Tehran in Alburz Mountains Iran.
Directions: 35-57-19 N, 52-06-37 E
Topography Type: Stratovolcano
Last ejection: About 6000 - multi year prior
Climbing: Moderate to troublesome
First rising: By unknown Iranian neighborhood individuals
Most straightforward course: South, Trekking
Posting: UNESCO World Natural Heritage Site
Articulation: دماوند - dæmävænd
Substitute Spellings: Damawand, Demavand, Damavend, Damāvand

Best Source of Information for Mt Damavand Iran
Suggested by Lonely planet - Iran (likewise in English manual sixth edtion 2012 - page 73):
Two astounding wellspring of data on all things Damavand:
Damavand Info: (our site: http://www.damawand.de/) and
Mt Damavand Guide:
(our weblog: http://damavandmt.blogspot.com/2010/01/damavand-crowd.html).

The data of this article is for the individuals who need to climb mount damavand and they have to realize the fundamentals like: nature with the course, nourishment program, conveying knapsack and gear, acclimation and its methodologies, drinking water, the most basic hardware that ought to be given, physical and the earth perils. It's imperative to know, what dimension of physical wellness you need; In what months of the year you should climb; What days of the week you should climb; The climbing should begin at what time and what pace; And a lot more fundamentals.

Damavand Mountain Climbing
What physical wellness is required for climbing Damavand?
Adequate physical wellness is the main essential condition to climb Damawand. Climbing to the Damavand Summit from the southern side is a practically simple trek for the individuals who consistently go climbing and trekking and have enough physical wellness. Obviously, the sulfur gas close to the summit may require more exertion for the last ascension.

Damavand Climbing Season
Mount Damavand's climate in March, April and May is entirely unstable and with high shot of enormous abrupt tempests. These elements can upset climbing projects and increment the dangers and risks of climbing. The best time to trek Damavand crest is between mid-June to mid-September. As we go from July to August, the territory will be drier and face unexpected changes in the atmosphere.

Best Days for Trekking Damavand
This point is progressively significant on the southern side of Mount Damavand. Since it is the most straightforward course to climb, the nearness of innumerable climbers along this way brings an excess of crowdedness and clamor, and separated from slaughtering the experience, it will cause some different issues like anticipating a decent rest and having a simple ascension. This issue is very unmistakable on ends of the week (Thursday and Friday are the ends of the week in Iran). Accordingly, it is prescribed to climb this course on Saturday (the first days of the Iranian week).

Climbing Mount Damavand Summit Iran
Highest Summit in the Middle East
Second Highest Volcano in Asia and Northen Hemisphere

Best Time of Day to Trek Damavand
As indicated by experienced climbers, because of the impact of the day warmth and daylight on sulfuric rocks which spread the smell of Damavand Volcano sulfur, it is smarter to move in the early morning. Be that as it may, it appears that daylight does not have much impact on this factor, and the benefit of resting amid the night and climbing the summit with more vitality in the early morning has the specific need.

Damavand Tenting Area
In the Damavand third campground, notwithstanding the two existing havens, some level region and reasonable grounds have been accommodated rising. In any case, because of the nearness of various climbers from all pieces of Iran on ends of the week, there might be deficiencies of room for tents in these spaces.

On the off chance that you are going to Damavand zone, it is smarter to move with local people or co-climbers who know about the territory. Despite the fact that there is an unmistakable way along the trek, however the rock stones in the trail, abrupt changes in the climate, and other surprising issues may cause issues amid the ascension. The most straightforward approach to climb Damawand is from the southern course, with better offices for climbers in camp 1 Poloor town and camp 3 Bargah Sevom. In the event that you are searching for a nearby mountain guide, we likewise offer directing help with various choices. get in touch with us for more subtleties.

It is better that no less than one individual from the gathering has just move to the summit of Damavand. In the last period of the move, from the last asylum to the summit, if there are associates in the gathering that there is no finished confirmation about their capacity to climb, it is smarter to ensure in the last piece of the ascension so bunch individuals don't get isolated; or before the trip, an individual from the gathering can be volunteered to return and go with the depleted people from the rising.

Mount Damavand Camp III Bargah Sevom
Old Shelter 4220m

Step by Step Instructions to Climb Damavand Summit
One of the principal significant focuses in climbing Damavand is gradual moving, which is significant in a few perspectives. The division of vitality for the whole way is conceivable with gradual advances, particularly on longer ways with more prominent inclines. Likewise, getting a charge out of the mountains and ascending exercises are achieving the summit, yet the whole length of the course and its different attractions can be agreeable, and the objective of ascending Damawand summit is to utilize every one of the attractions of the way. Particularly, in transit of astonishing and breathtaking Damavand.

Amid trekking to high elevation mountains, for example, Damavand mountain in Iran 5671 masl, the slow procedure of coordinating the body with the oxygen inadequacy in high height is classified "Ascending acclimation" or Acclimatization. These change makes it simpler to convey more oxygen to the cells and furthermore improve oxygen usage. There are noteworthy individual contrasts in the capacity of people to adjust to height. A few, rapidly adjust to elevation, while others have intense mountain eardrums and require longer timeframes to match up with the height.

The most significant signs and manifestations that happen until you are completely synchronized with existing air are cerebral pains, sickness and discombobulation. To adapt to enduring inconveniences and more preparation for the last move to Damavand, one can well arrangement with this issue by completing a move of 4,500 meters high and coming back to the safe house. If there should be an occurrence of progressively significant issues and serious indications, take the individual to the lower elevations rapidly and get help from experts who know about the emergency treatment till achieving the official restorative assistance.

Equipment List for Trekking Damavand
To appreciate a sheltered move to Damavand summit, it is basic to bring the best possible hardware. Continually get enough riggings to secure yourself instance of awful climate. Depending to the climate on the summit day, you can choose which gears you have to take with you and which pointless apparatuses to abandon at camp 3 Bargah Sevom. Probably the most significant things to bring are recorded beneath.

Equipment for Damavand Iran

Risks of climbing Mount Damavand
To the extent climbing trouble and trekking grade is concerned, Damavand isn't in fact troublesome. Yet, it is unsafe because of the unexpected climate changes and low environmental pressure at its pinnacle which is just 456 mm Hg. This typical climbing danger may cause a few issues for the climbers.

Climate
Damawand Winter Warning. Cautioning for Winter Climb and Ski Mountaineering, Environmental risks on Damavand Peak. Keep in mind climate condition at Mount Demavand could change to grievous in winter season, with solid breezes achieving in excess of 100 km/h (62 m/h) and frigid temperature dropping down to beneath - 70° Celsius (- 94 Fahrenheit) at the summit.

You should be well-prepared and well-experienced for such a troublesome ascension and ski mountaineering endeavors in unforgiving atmosphere and further more recall that salvage and therapeutic offices are not accessible in damavand zone and in the event of damage and crisis you need a good karma for enduring, so additional consideration ought to be taken for ascending and ski visiting in winter and it is finished by your own hazard.

This low temperature additionally relies upon the heading and side of damavand mountain run. The north face is the coldest course of Damavand, and the temperature some of the time achieves short 50 ° C. The southern course is the second point on which the virus commands, since it is in the shadows until early afternoon and late morning. Consequently, moving in such a circumstance requires its own involvement and gear, and climbers who don't consider this basically face the danger of solidifying and afterward removal of the organs. Demavand has solid breeze accelerate to 120 Km/h (77 M/h).

Damavand Warning and Risks

Storm and Fog
Damavand spring of gushing lava pyramid is situated in an open space and the tempest strikes from each side forestall air moistness stream from the north and west sides. As the outcome, a cloud cap will be conformed to the summit. In such a circumstance, snow falls, hail or solid breeze blowing is conceivable. These conditions are additionally risky for climbers. In the winter, particularly on the west side of the mountain, there are loads of tempests, winds, mist and the mists which cause losing he ways.

Snow and Avalanche
The breeze blows cause the collection snow in Damavand gaps, and in the long run the torrential slide to fall, particularly in the pre-spring and late-winter on the south course, there is an opportunity of snow torrential slide. The torrential slide crashes in Damavand are visit, so the commonality and distinguishing proof of the torrential slide course is fundamental to maintain a strategic distance from the risk.

Avalanche
With the beginning of summer and snow dissolving, this hazard will be higher than at any other time, particularly in the western course where rough materials are flimsy, and with the smallest weight there will be a slide. In the spring, there is a danger of shake falls in the ice sheets, shake and mud slide.

AMS
Physical dangers on the summit of Damavand dependably has its very own dangers because of its high height for climbers who are not physically prepared or don't have enough involvement. Creating tallness related manifestations which typically show up as cerebral pains, queasiness, or unsteadiness are the signs witch ought to be paid attention to by each climber. That is to say, the climber shouldn't keep up the course and needs to return at the earliest opportunity.

Access Road and Trails to the Peak
To achieve the damavand beginning stage, first camp, which is additionally called the base of Iran hiking alliance, you can ride to Poloor town through Haraz Road. Haraz street or street N 77, alongside street No 59 (Karaj-Chalous), are the most significant streets which associate capital Tehran to Mazandaran area. Haraz Road is additionally the best way to Damawand Mountains. Haraz street is a standout amongst the most excellent and memorable streets in Iran, chosen by the Iranian individuals in 2010, as the loveliest road in Iran. This street is the briefest course among Tehran and Amol city.

Footpaths and Tracks to Damavand Peak
Mount Damawand has sixteen routes. Four of these ways are well known for trekking and climbing. The four basic courses are South, West, North and the North-East course. Every one of these Damawand trails have an asylum/shelter at around 4000 meters' elevation. The North face has an additional haven at about 5000m. The South face is the most well-known side of the mountain, with a superb new mountain resort at 4250m. Most mountain climbers want to move from the exemplary South course.

Damavand Road Map and Route Trail
By A. Soltani

South Route
It is effectively available from Tehran or North of Iran. The short separation from T
ehran to the Haraz fundamental road makes Damavand southern route the best trail. This is by a long shot the least demanding and the best side and the rising to the summit by along these lines is likewise shorter. Visit also Damavand Routes.

Damavand Peak
Mount Damavand is known as the most astounding mountain in Iran and the greatest fountain of liquid magma in the Middle East. It is situated in the focal piece of the Alborz mountain extend (central Alburz), and in the south of the Caspian Sea, in the Larijan area of Amol.

Damavand Height
Damavand Mountain peak is situated in Mazandaran region has the elevation of 5671 m, as indicated by the national Iranian Statistics; be that as it may, as indicated by some different sources, including the National Geospatial Data Base of Iran and the NASA Earth Observatory site, the statures of 5610 meters and 5671 meters has likewise been announced for Damawand.