Saint James the Great in the context of Pilgrimage in Christianity

Christianity has a strong tradition of pilgrimages, both to sites relevant to the New Testament narrative (especially in the Holy Land) and to sites associated with later saints or miracles.

Symbolism of Christian saints has been used from the very beginnings of the religion. Each saint is said to have led an exemplary life and symbols have been used to tell these stories throughout the history of the Church. A number of Christian saints are traditionally represented by a symbol or iconic motif associated with their life, termed an attribute or emblem, in order to identify them. The study of these forms part of iconography in art history. They were particularly used so that the illiterate could recognize a scene, and to give each of the Saints something of a personality in art. They are often carried in the hand by the Saint.

Attributes often vary with either time or geography, especially between Eastern Christianity and the West. Orthodox images more often contained inscriptions with the names of saints, so the Eastern repertoire of attributes is generally smaller than the Western. Many of the most prominent saints, like Saint Peter and Saint John the Evangelist can also be recognised by a distinctive facial type. Some attributes are general, such as the martyr's palm. The use of a symbol in a work of art depicting a Saint reminds people who is being shown and of their story. The following is a list of some of these attributes.

Santiago de Compostela, simply Santiago, or Compostela, in the province of A Coruña, is the capital of the autonomous community of Galicia, in northwestern Spain. The city has its origin in the shrine of Saint James the Great, now the Cathedral of Santiago de Compostela, as the destination of the Way of St. James, a leading Catholic pilgrimage route since the 9th century. In 1985, the city's Old Town was designated a UNESCO World Heritage Site.

Santiago de Compostela has a very mild climate for its latitude with heavy winter rainfall courtesy of its relative proximity to the prevailing winds from Atlantic low-pressure systems.