Nevado de Toluca

Coordinates: 19°06′06″N 99°46′03″W / 19.10167°N 99.76750°W / 19.10167; -99.76750
Source: Wikipedia, the free encyclopedia.
Nevado de Toluca
North America prominent 61st
  • Mexico highest major peaks 4th
  • Coordinates19°06′06″N 99°46′03″W / 19.10167°N 99.76750°W / 19.10167; -99.76750[1]
    Geography
    Nevado de Toluca is located in State of Mexico
    Nevado de Toluca
    Nevado de Toluca
    Location in Mexico
    Location
    México, Mexico
    Geology
    Mountain typeStratovolcano
    Volcanic arc/beltTrans-Mexican Volcanic Belt
    Last eruption1350 BCE (?)
    Climbing
    Easiest routeroad, hiking trail

    Nevado de Toluca (Spanish:

    Iztaccíhuatl. The volcano and the area around it is now a national park
    .

    Etymology

    It is often called by the

    archeology discoveries in and around the area. It has been concluded that its correct etymology is Chicnauhtecatl meaning "Lord of Nine", probably referring to the various deep lakes at the top of the cone.[4]

    Description

    Lago del Sol (Sun Lake)

    The volcano has a 1.5-kilometre (0.93 mi) wide summit

    summit, the 4,680-metre (15,354 ft) Pico del Fraile (Friar's Peak), is on the southwest side of the crater
    and the second highest, the 4,640-metre (15,223 ft) Pico del Aguila (Eagle's Peak), is on the northwest.

    There are two crater lakes on the floor of the basin at about 4,200 m (13,800 ft), the larger Lago del Sol (Sun Lake) and the smaller, but deeper, Lago de la Luna (Moon Lake).[5]

    A road formerly ran into the caldera to the lakes, but is now gated 2 km before the lakes.[citation needed]

    From the southeast, Nevado de Toluca looks flat-topped, like shoulders without a head. A Nahuatl legend (recounted as part of the legend of Popocatépetl and Iztaccíhuatl) provides a mythical explanation.[6]

    360° panoramic view from crater rim of Nevado Toluca, 120 km to the east the Popocatépetl rises out of the clouds

    Geology

    It is believed that Nevado de Toluca may once have been as tall as Popocatépetl, until an enormous eruption nearly 25,000 years ago blasted the top of the cone off and reduced its height by as much as 900 m (3,000 ft).[5] The same eruption generated thick lahars, or mudflows, which coated the sides of the mountains. An eruption approximately 500 years later deposited layers of pumice on the mountain's east and northeast slopes.[5]

    The last major

    VEI strength of 6 (comparable to the 1991 eruption of Mount Pinatubo). The eruption emplaced 1.5 m (5 ft) of pebble-sized pumice in the City of Toluca region and ~50 cm (2 ft) of medium to fine sand in the Mexico City region. Distal lahar deposits derived from the Upper Toluca Pumice event incorporated mammoth
    bones and other mammals in the basin of Mexico.

    The volcano became inactive after a volcanic plug formed in the volcano's vent. The plug eventually became known as El Ombligo ("the Navel").[5]

    Climate

    Near the summit, Nevado de Toluca has a cold alpine climate (Köppen climate classification ET) with cold temperatures year round. There is little variation in the temperatures and frost and snow can occur in any month. The winter season covers from November to April and precipitation is low, averaging 7.5 millimetres (0.5 in) in March, the driest month.[7] Temperatures during this time are cold, averaging 2.3 °C (36.1 °F) in January. The summer season spans from May to October and precipitation is very high, averaging 235.4 millimetres (9.5 in) in July. Temperatures during this time are warm, averaging 5.3 °C (41.5 °F) in May. The summit is often foggy, averaging 78 days with fog, most of it during the monsoon season.[7] The wettest record month was July 2008 when 513.5 millimetres (20 in) of precipitation fell and the wettest recorded day was July 16, 1999 when 90.5 millimetres (3.5 in) of precipitation fell. The highest temperature ever recorded was 23 °C (73.4 °F) on August 16, 1993 and the lowest temperature recorded was −10 °C (14.0 °F) on February 2, 2004.

    Climate data for Nevado de Toluca (4283 m) (1981-2010 normals, extremes 1964-2019)
    Month Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Year
    Record high °C (°F) 15.0
    (59.0)
    16.5
    (61.7)
    19.0
    (66.2)
    19.0
    (66.2)
    19.3
    (66.7)
    19.0
    (66.2)
    21.0
    (69.8)
    23.0
    (73.4)
    16.0
    (60.8)
    19.0
    (66.2)
    14.0
    (57.2)
    13.0
    (55.4)
    23.0
    (73.4)
    Mean daily maximum °C (°F) 7.4
    (45.3)
    8.2
    (46.8)
    9.8
    (49.6)
    10.5
    (50.9)
    10.1
    (50.2)
    9.6
    (49.3)
    8.6
    (47.5)
    8.5
    (47.3)
    8.2
    (46.8)
    8.2
    (46.8)
    7.8
    (46.0)
    7.5
    (45.5)
    8.7
    (47.7)
    Daily mean °C (°F) 2.3
    (36.1)
    2.9
    (37.2)
    4.4
    (39.9)
    5.3
    (41.5)
    5.3
    (41.5)
    5.2
    (41.4)
    4.5
    (40.1)
    4.5
    (40.1)
    4.3
    (39.7)
    3.9
    (39.0)
    3.0
    (37.4)
    2.5
    (36.5)
    4.0
    (39.2)
    Mean daily minimum °C (°F) −2.9
    (26.8)
    −2.3
    (27.9)
    −1.0
    (30.2)
    0.0
    (32.0)
    0.6
    (33.1)
    0.8
    (33.4)
    0.5
    (32.9)
    0.4
    (32.7)
    0.4
    (32.7)
    −0.4
    (31.3)
    −1.7
    (28.9)
    −2.4
    (27.7)
    −0.7
    (30.8)
    Record low °C (°F) −7.5
    (18.5)
    −10.0
    (14.0)
    −8.0
    (17.6)
    −6.0
    (21.2)
    −5.0
    (23.0)
    −4.0
    (24.8)
    −4.0
    (24.8)
    −7.0
    (19.4)
    −5.0
    (23.0)
    −9.0
    (15.8)
    −6.5
    (20.3)
    −8.5
    (16.7)
    −10.0
    (14.0)
    Average precipitation mm (inches) 13.6
    (0.54)
    10.1
    (0.40)
    7.5
    (0.30)
    54.6
    (2.15)
    125.6
    (4.94)
    205.5
    (8.09)
    235.4
    (9.27)
    229.4
    (9.03)
    209.2
    (8.24)
    92.1
    (3.63)
    23.9
    (0.94)
    9.0
    (0.35)
    1,215.9
    (47.88)
    Average rainy days 2.5 2.2 1.7 6.0 13.4 19.7 23.6 22.9 20.7 11.8 3.8 1.9 130.2
    Source: Servicio Meteorológico Nacional[7][8]

    Archeological sites

    There are 18 registered archeological sites in the park, as this was a ritual center during pre-Hispanic periods. Bernardino de Sahagún wrote about the lakes as a place where the indigenous held ceremonies and sacrifices. The lakes themselves are considered to be two sites, as a large number of offerings, especially copal, were deposited in the lakes. These deposits can be found all over the lakebed as the burning copal was set adrift on the lakes’ waters until it sank. Other objects have been found such as ceramics and sculpted stones. Divers used to sack many of the pieces found here but now authorities carefully monitor those who dive.[9][10]

    Most of the other sites are found on the crater's walls and peaks. One of the sites is called Xicotepec which is at the top of a rocky dome known as the Cerro de Ombligo (Spanish for "the navel").

    Archangel Michael since the colonial period.[9]

    There have been intermittent archeological

    priests to predict the growing season.[11]

    Gallery

    See also

    Notes

    1. ^ a b c d "Mexico Ultras" Peaklist.org. Retrieved 2012-01-29.
    2. ^ a b c d "Nevado de Toluca, Mexico" Peakbagger.com. Retrieved 2012-01-29.
    3. ^ Arqueologia Mexicana
    4. ^ Archeologia Mexicana magazine vol.VIII #43
    5. ^ .
    6. ^ Text by Martín N. Méndez, recorded ca. 1944, published as “The Three Volcanoes” in Pittman, Richard S (1954), A Grammar of Tetelcingo (Morelos) Nahuatl, Language 30 Number 1 (Part 2), p.59.
    7. ^ a b c "Normales climatológicas 1981-2010" (in Spanish). Servicio Meteorológico Nacional. Retrieved March 3, 2023.
    8. ^ "Extremas" (in Spanish). Servicio Meteorológico Nacional. Retrieved March 3, 2023.
    9. ^ a b Montero García, Ismael Arturo. "Chicnauhtecatl" [Nevado de Toluca] (in Spanish). Mexico City: Fundación Montero. Retrieved 20 February 2010.
    10. ^ Rivas, Vanessa (2001-07-28). "Nevado de Toluca: Majestuosidad y leyenda" [The Nevado de Toluca: Majesty and legend]. Reforma (in Spanish). Mexico City. p. 10.
    11. ^ "ANCIENT OBJECTS ARE ON TOP OF NEVADO DE TOLUCA". National Institute of Anthropology and History (INAH). January 14, 2011. Archived from the original on 3 December 2013. Retrieved 15 January 2011.

    References

    External links