Guadalupe Hill is named after Our Lady of Guadalupe of Badajoz, not -as is commonly believed- after the famous Our Lady of Guadalupe in Mexico.^[2]

The Guadalupe Hill is the type locality for the Campanian-Maastrichtian Guadalupe Group, a sequence of three formations of sandstones and shales; Arenisca Dura, Plaeners, Arenisca de Labor and Arenisca Tierna. The thickness of the Guadalupe Group, defined as formation by some authors, at Guadalupe Hill is 750 metres (2,460 ft).^[3] Approximately 53% of the Eastern Hills consists of the Guadalupe Group.^[4]

The Guadalupe Group is thrusted on top of the younger Guaduas, Bogotá and Cacho Formations by the Bogotá Fault.^[5] The NNW-SSE trending eastward dipping thrust fault forms a barrier for aquifers.^[6] The creeks (quebradas) Manzanares and El Chuscal originate from Guadalupe Hill.^[7]

Guadalupe Hill in the times before the Spanish conquest was one of the sacred hilltops in the religion of the Muisca, the indigenous inhabitants of the Bogotá savanna. They considered the hills sacred and buried their dead in the mountains. The people, organised in a loose confederation of leaders, the Muisca Confederation, had an advanced knowledge of archaeoastronomy and constructed various temples honouring Sué, the god of the Sun, throughout their territories. Guadalupe Hill in pre-Columbian times was called in their language Muysccubun quijicha guexica, "grandfather's foot".^[8] Seen from Bolívar Square, at the winter solstice of December, Sué rises exactly over Guadalupe Hill and at the equinoxes of March and September in the valley between Monserrate and Guadalupe.^[9]

At the time of the conquest, the Eastern Hills were a forested natural boundary of the Bogotá savanna. During the early colonial period, the Spanish constructed a cross on Guadalupe Hill as a symbol to protect the capital of the New Kingdom of Granada.^[2] The wood of the trees of the Eastern Hills were used for construction and heating in the city that grew steadily until the 19th century. This led to deforestation and erosion in the Eastern Hills and when Alexander von Humboldt visited Santa Fe de Bogotá in 1806, he noted "that there was not a single tree left until the open area of Choachí".^[10] The first replanting of trees took place in 1855, and a second phase of reforestation happened in 1940.^[11][12] In 1801, Francisco José de Caldas recalculated the height of Guadalupe Hill.^[13]

Hermitage and statue edit

The first hermitage on Guadalupe Hill was built in 1656 and blessed during a pilgrimage on September 8 of that year.^[2] The hermitage was destroyed by the earthquakes of 1743, 1785 and 1827. During the presidency of Tomás Cipriano de Mosquera, the hermitage was reconstructed, but affected again by the 1917 Bogotá earthquake.^[14] The hermitage was rebuilt in 1945 by Jorge Murcia Riaño and blessed by archbishop Ismael Perdomo. In 1946, the 15 metres (49 ft) high statue of the Virgin of Guadalupe, sculpted by Gustavo Arcila Uribe, was constructed on top of Guadalupe Hill.^[2] In 1967, the chapel and road leading up to it were constructed.^[2][15]

The Guadalupe Hill and the statue of the Virgin of Guadalupe are among the main touristic attractions of Bogotá. The top of the hill offers a viewpoint (mirador) for the Colombian capital. The hill can be accessed via a walking trail, used by pilgrims since colonial times, or by the road to Choachí via the Avenida Circunvalar.^[2][14]

Public transport to Guadalupe Hill leaves on Sundays from Carrera 10 with Calle 6.^[15] Since 1997, a running contest is held to ascend the Guadalupe Hill.^[16]

Every Sunday, the chapel on the hill receives tourists between 7:00 in the morning and 4:00 in the afternoon.^[15] On the first Sundays of the month, a mass is held from 8:00 to 10:00 AM and at noon.^[2]

•  
  Guadalupe Hill from Monserrate
•  
  Guadalupe Hill behind the business district of Bogotá
•  
  Clouds over Guadalupe Hill
  from Avenida Jiménez
•  
  Our Lady of Guadalupe statue
•  
  Head of the statue

• Eastern Hills, Bogotá
• Bogotá savanna

Bibliography edit

• Bonilla Romero, Julio H.; Bustos Velazco, Edier H.; Duvan Reyes, Jaime (2017). "Arqueoastronomía, alineaciones solares de solsticios y equinoccios en Bogotá-Bacatá – Archaeoastronomy, alignment solar from solstices and equinoxes in Bogota-Bacatá". Revista Científica, Universidad Distrital Francisco José de Caldas. 27: 146–155. Retrieved 2017-01-18.
• Bonilla Romero, Julio H (2011). "Aproximaciones al observatorio solar de Bacatá-Bogotá-Colombia – Approaches to solar observatory Bacatá-Bogotá-Colombia". Azimut, Universidad Distrital Francisco José de Caldas. 3: 9–15. Retrieved 2017-01-18.
• De Caldas, Francisco José (1801). Observaciones sobre la verdadera altura del Cerro de Guadalupe que domina esta ciudad, dirigidas a los editores del 'Correo Curioso'. pp. 365–374. Retrieved 2017-01-18.
• Camargo Ponce de León, Germán. "Historia pintoresca y las perspectivas de ordenamiento de los Cerros Orientales de Santa Fe de Bogotá" (PDF). pp. 1–16. Retrieved 2017-01-18.^{[dead link]}
• Guerrero Uscátegui, Alberto Lobo (1992). Geología e Hidrogeología de Santafé de Bogotá y su Sabana (Report). Sociedad Colombiana de Ingenieros. pp. 1–20.
• Mapa geológico de Santa Fe de Bogotá – Geological Map Bogotá – escala 1:50,000 (PDF) (Map). Ingeominas. 1997. p. 1. Archived from the original (PDF) on November 22, 2017. Retrieved 2017-01-18.
• Velandia Patiño, F.A.; De Bermoudes, O. (2002). "Fallas longitudinales y transversales de la Sabana de Bogotá, Colombia". Boletín de Geología. 24: 37–48.
• Wiesner Ceballos, Diana; Sánchez Sanabria, Jean Carlo; Quintero, Otto Francisco; Mesa Ramírez, Andrés; Armotegui, Vicente; Puerta Giraldo, Sebastián (2007). Los caminos de los cerros (PDF) (Report). Alcaldía Mayor de Bogotá. pp. 1–73. Archived from the original (PDF) on June 7, 2021. Retrieved 2017-01-18.

• Ortega Díaz, Alfredo (1924). Architecture of Bogotá. Bogotá. ISBN 958-9054-12-9.{{cite book}}: CS1 maint: location missing publisher (link)

• (in Spanish) Shrine of Our Lady of Guadalupe
• (in Spanish) Seismic history of Bogotá