A search on the internet reveals very little useful information about the Alborz Mountains. This page will hopefully introduce the reader to these mountains and provide an interactive map that will allow the reader to zoom on pre-selected areas. A partial list of those peaks whose elevations exceed 4000 meters has also been provided. I am not aware of any other source that provides such a list. Most of these peaks have been linked to a page or at least a picture. As new pages/pictures are added, new links will be made.
With few exceptions, all elevations are per the 1:50 000 maps (see Maps section below).
With few exceptions the names of all of the peaks between Karaj/Chalus and Haraz Rivers are as they appear on “Guide map of Climbing the Peaks of Central Alborz” and the names of the peaks of the Takhte Soleyman Massif are as they appear on “The Guide Map of Takhte Soleyman & Alam Kuh Region”. The names of other peaks are as they appear on the 1:50 000 maps or otherwise commonly used names.
Click on above map to zoom on selected areas.
Click on above image and click again to see Large/detailed Map of Central Alborz
ALBORZ MOUNTAINS OVERVIEW
The lush north slopes
The lush north slopes
The term “Alborz Mountains” has been loosely used in reference to all of the mountains of northern Iran, from the Turkish border to the northwest, to the border with Afghanistan to the northeast (a distance of more than 1500 km). The Alborz Mountains gain their maximum height and density along the southern shores of the Caspian Sea where they create a formidable barrier that separates the coastal plains from the internal plateau of Iran. Close proximity to the Caspian coast has created a steamy lush environment on the coastal plains and the northern-most slopes of the mountains. In some places (near the coastal towns of Ramsar and Noshahr), the strip of land between the mountains and the sea is no more than one kilometer wide.
The southern slopes of the Alborz drop onto the central plateau of Iran. The average elevation of this plateau at the base of the mountains is around 1500 m (Please be ware that the plateau itself is covered by other scattered mountains. In fact, there are few places in Iran where mountains can not be seen in the horizon). In contrast to the lush northern slopes, the southern slopes of the Alborz Mountains are barren. Trees can be found only on stream banks at the bottom of the valleys. Grasslands, alpine tundra and permanent snow cover the higher slopes of the Alborz. Evidence suggests that in the past, glaciers used to cover a much larger area of the Alborz Mountains than they do today. At the present time, glaciers can be found on Mt. Damavand, Takhte Soleyman Massif, Mt. Sabalan and to a much lesser extent on some of the higher peaks of the range. Winter brings a heavy coat of powdery snow that creates an ideal environment for skiing. The abundance of snow gives rise to fairly large mountain streams that provide fresh water for the nearby cities including the 10 million plus mega-city of Tehran. When viewed from space, some of these streams appear to have dug deep gorges that penetrate into the heart of the mountains. The distance between the 5671 m Mt. Damavand and the bottom of the Haraz Valley to the northeast of it where the elevation is only 1000 m is no more than 17 kilometers.
TEHRAN AND THE ALBORZ MOUNTAINS
The capital city of Tehran sits on a plain at the foot of the Alborz Mountains. The 3964 m Mt Tochal creates a dramatic background for Tehran's skyline.
Tehran & the Alborz Mountains
PEAKS HIGHER THAN 4000 METERS
Peaks higher than 4000 meters can be found in two areas in the Alborz Mountains (Please note that this discussion excludes the Zagros Mountains of western/southern Iran that also have many groups of peaks higher than 4000 m):
1) A few peaks around the 4811 m summit of Mt. Sabalan in northwestern Iran
2) Depending on how you count them, around one hundred in Central Alborz
CENTRAL ALBORZ OVERVIEW
The boundaries of Central Alborz can be defined as follows (300 km E-W by 90 km N-S. See Signature Photo):
-South of the Caspian Sea
-North of the Capital city of Tehran and vicinity
-East of the Coastal town of Rasht
-West of the coastal town of Sari
Much of Central Alborz consists of very long parallel ridgelines that generally run east-west (parallel to the coast of the Caspian Sea). Deep valleys divide these ridgelines into distinct “groups”. Defining individual peaks along the length of these ridgelines that might be many tens of kilometers long and entirely above 3500 or 4000 m, can be arbitrary. Except for the prominent peaks, it appears that traditionally names have been used in reference to whole groups of peaks rather than individual ones. While many peaks remain nameless, others might be known by different names. The most accurate maps of the Alborz Mountains are those with a scale of 1:50 000 (see below). These maps provide exact elevations for hundreds of peaks/high points on each sheet but they leave most peaks without a name. It seems that the climbing community in Iran has recently started to publish maps that identify individual peaks and provide them with names (that will hopefully standardize). I am not aware of the criteria used for identifying these “Peaks” but looking at the 1:50 000 maps reveal that most of these peaks are at least 50 m higher than their surrounding saddles (most are much more than that).
The higher than 4000 meters peaks of Central Alborz can be divided into several groups as below:
a) ALAM KOOH/TAKHTE SOLEYMAN MASSIF
Large Map of Takhte Soleyman Massif
Alam Kooh & part of the Takhte Soleyman Massif to the south of it
Alam Kooh & part of the Takhte Soleyman Massif to the north of it
After the single volcanic cone of Mt. Damavand that rises to 5671 m (see below), the Takhte Soleyman Massif contains the highest peaks of Central Alborz (and the only place where the elevation of the peaks exceeds 4400 m). The crest of the massif consists of a 19 km long ridgeline that runs (unlike the rest of the ridgelines in Central Alborz) north-south and is entirely above 4000 m. Two branch ridgelines (the Haft Khan and the Chaloon/Siah Kaman ridgelines) bring the total length of the interconnected ridgelines that are entirely above 4000 m to 30 km (there are other connecting ridgelines that are partially above 4000 m).
Deep “V-shaped” valleys that surround the massif to the east, north and west of it, are heavily forested and drop steeply to the Caspian Sea. Sheer walls and high “U-shaped” valleys point to extensive glacial activity in the area. In fact, the massif contains the largest collection of glaciers in Iran.
In his “Takhte Soleyman Massif”page, Summitpost member “nomad” gives a list of 160 peaks that are higher than 4000 m. I simply do not have enough detailed information to know how many of these peaks pass the rule of “91 meters (300 ft) above the surrounding saddle” that is used in the Colorado Mountains of western United States for defining individual peaks. My personal experience in the massif and consulting the 1:50 000 maps seem to indicate that there are at least twenty peaks higher than 4400 m that probably meet the rule of 91 meters as listed below. Lower than 4400 m, the peaks become too numerous for me to count.
b) MT. DAMAVAND AND THE MIDDLE WALL OF CENTRAL ALBORZ
Map of Damavand & Dokhaharan Massif
Map of Kholeno Massif
The spine of this area consists of an 80 km long ridgeline that starts with Mt. Damavand (to the west of the Haraz Valley) and stretches west to near the Kandovan Pass on Karaj-Chalus Road. Except for the 3420 m Kabood Pass, the elevation of this ridgeline never drops below 3500 m. If you add the length of the many branches of this ridgeline, you will come up with more than 150 km of interconnected ridgelines whose elevations are entirely above 3500 m (except for Kabood Pass).
High glacially carved valleys can be found near some of the higher peaks (especially Kholeno and its nearby peaks). I am not a geologist but these valleys seem to point to glacial activity in the distant past. While today, some snow remains in the valleys year round, by late summer, the remaining snow patches are probably not large enough to be classified as “glaciers”.
The 5671 m summit of Mt. Damavand that rises on the eastern-most part of this ridgeline is by far the highest peak of Central Alborz (and the Middle East). Damavand is an almost perfect volcanic cone whose superior height makes it visible from miles away.
After Mt. Damavand, the highest peaks of this area are in the low 4000 meter range as listed below. The 4000 m peaks can be lumped into two distinct groups: The Kholeno Massif to the west and the Dokhaharan Massif to the east. (I have tried to limit the list to only those that seem to rise at least 50 meters above their surrounding saddles)
Consists of a 20 Km long ridgeline in the western part of Central Alborz that runs east-west and is entirely above 3500 m. The eastern half of the ridgeline forms a broad hump, the highest point of which is the 4003 m Saat Peak. The western half has five peaks above 4000 m. The northern slopes of the western half seem to have much steeper slopes than the southern slopes. The two halves are connected via the 3575 m Tanoorakan Pass. The peaks of this area are as follows:
A long chain of peaks that form a line that runs east-west in western Central Alborz north of the Karaj River Valley and south of the Shah Rood River Valley. The elevations of these peaks are mostly above 3700 m. Only two peaks are higher than 4000 m:
A 52 km long ridgeline that runs east-west in the southeastern part of Central Alborz. The elevation of 32 km of this ridgeline is entirely above 3500 m. Depending on how you count them, there are at least 5 peaks higher than 4000 m. West to east, these include:
1) Angemar II 4020 m
2) Amgemar I 4047 m
3) West Dobrar 4072 m
4) East Dobrar 4070 m
5) Ghareh Dagh 4057 m
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When To Climb
Mid June to early Octcober. I prefer late June/early July when there is still much snow on the mountains.On the lower slopes the grass is green and flowers are in bloom. Too much snow, however, will obviously make the climb harder.
Many people climb these mountains in winter. That obviously requires training and special equipment.
Generally, camping is allowed anywhere. You will also find mountain huts on the more popular areas.
In summer, the weather is generally clear. Isolated thunderstorms (sleet/snow at higher elevations) do happen.
The most accurate topographic maps of the area are those with a scale of 1:50 000 produced by the Iranian armed forces, These maps are available in Tehran at the Geographical office of the armed forces on Moalem St. (Tel 98 21 88408088). Outside of Iran, the same maps can be purchased at www.cartographic.com for a very high price. These maps are in Farsi. While they provide accurate/detailed topographic info, these maps do not necessarily provide a name for each and every peak.
For the Takhte Soleyman Massif, “The Guide map of Takht-e-Soleiman & Alam Kuh Region” by Iran Kuhro and for the mountains between the Karaj/Chalus and Haraz Rivers the “ Guide Map of Climbing the Peaks of Central Alborz” by Gitashenasi provide additional information and names for most of the peaks. These maps are schematic (cartoon-like) and distort distances and relative positions but can be useful when used with the 1:50 000 maps.
The maps provided here have been created by me based on the 1:50 000 maps and are to scale.
Children refers to the set of objects that logically fall under a given object. For example, the
Aconcagua mountain page is a child of the 'Aconcagua Group' and the 'Seven Summits.' The
Aconcagua mountain itself has many routes, photos, and trip reports as children.