Pico de Orizaba : High Mountain in Mexico

Pico de Orizaba : High Mountain in Mexico

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Pico de Orizaba : High Mountain in Mexico – Orizaba is the third highest ridge in North America, with alone Denali (Mt. McKinley) in Alaska and Mount Logan in Canada being higher.

Some Basic Info on Mexico’s Highest Mountain

  • Elevation : 18,491 feet (5,636 rhythms). Notation that Orizaba’s exact height is not agreed upon. Different questionnaires have produced different upshots, especially as increasingly accurate means of measurement ought to have employed. It’s generally agreed that the mountain is at least 18,400 high pitched and no higher than 16,600 feet.
  • Prominence : 16,148 paws( 4,922 rhythms) 7th most prominent ridge in “the worlds”
  • Location : East-central Mexico
  • Coordinates : 19.029959 N/ -97.269527 W
  • First Ascent : First recorded ascending by U.S. solders William Raynolds and G. Maynard in 1848. The ridge was almost certainly descended earlier by neighbourhoods who did not record expected accomplishment in any documents that survive.
  • Orizaba is sometimes called by its Aztec name Citlaltepetl, which necessitates star Mountain. It’s also called Volcan Pico de Orizaba, meaning “Volcano Peak of Orizaba”.
  • Orizaba is the highest peak in “the worlds” between 10 and 20 grades north latitude and the most important one volcano in North America.
  • Orizaba is noticeable on a clearly defined daytime from the Gulf of Mexico and the city of Veracruz over 60 miles to the east.
  • Orizaba is set 120 miles east of Mexico City on their own borders of the Mexican moods Puebla and Vera Cruz.

Origins Of Orizaba’s Name

The name Orizaba comes from a nearby township and the valley south of the peak.

Orizaba is a bastardized Spanish term from the Aztecan name Ahuilizapa (declared awil lis a pan), which translate to “Place of the Playing Water”. Early natives caled it Poyautecatl, which alters “mountain that reaches the mas”.

Basic Geology : Glacier And Volcano

Orizaba is a huge hibernating volcano that last appeared between 1545 and 1566.

It is the second highest dormant volcano in “the worlds” exclusively Kilimanjaro in Africa is higher.

The volcano assembled in three theatres in the Pleistocene Epoch over a million years ago.

Pico de Orizaba is alsoa true alpine environment with nine glaciers Gran Glaciar Norte, Lengua del Chichimeco, Jamapa, Toro, Glaciar de la Barba, Noroccidental, Ocidental, Surocidental, and Oriental. Most of the glaciers occur on the northern line up of the volcano, which receives less sun than the countries of the south flank.

The Gran Glaciar Norte or Great Glacier of the North is the largest on Orizaba, flooding down from the summit to about 16,000 feet. Until lately, the average thickness of these glaciers was of about 160 feet, and submerge about 3.5 square miles. Various twenty first century climbers’ blogs, nonetheless , tone rapid further deterioration of glaciated fields. Countless propose that this is the result of global warming.

Climbing Pico De Orizaba

Among the highest mountains, Orizaba is a relatively easy climb. The standard ascending street is along the the Jamapa Glacier, The final ascending “re starting” the Piedra Grande Hut at 14,010 feet (4270 rhythms). The climb traverses a snowfield province and then ascends the glacier, which reaches an tilt of 40 grades near the top.

This expects climbers to be competent with an sparkler axe, crampons, and descending tether.


Orizaba is not a particularly difficult climb, which doesn’t mean there aren’t dangerous phases. among them :

  • The high altitude can affect climbers, peculiarly older climbers. This are now beginning as mountain sickness weaknes, headaches and nausea but can progres to pulmonary edama (HAPE) and cerebral edama, both of them often fatal at high altitudes.
  • The traverse along the crater rim to its high point elevation, although not technically difficult, is potentially dangerous a slip contributes either into the crater or down the steep sided volcano. Either route represents a potentially fatal dusk.

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