Contribución al conocimiento de la Cueva de El Sidrón (Piloña, Asturias) con técnicas de láser escáner 3D

  1. G. Santos-Delgado 1
  2. J. Martínez Rubio 2
  3. P.G. Silva Barroso 1
  4. S. Sánchez-Moral 3
  5. J.C. Cañaveras Jiménez 4
  6. M. de la Rasilla Vives 5
  1. 1 Universidad de Salamanca
    info

    Universidad de Salamanca

    Salamanca, España

    ROR https://ror.org/02f40zc51

  2. 2 Universidad de Valladolid
    info

    Universidad de Valladolid

    Valladolid, España

    ROR https://ror.org/01fvbaw18

  3. 3 Museo Nacional de Ciencias Naturales
    info

    Museo Nacional de Ciencias Naturales

    Madrid, España

    ROR https://ror.org/02v6zg374

  4. 4 Universitat d'Alacant
    info

    Universitat d'Alacant

    Alicante, España

    ROR https://ror.org/05t8bcz72

  5. 5 Universidad de Oviedo
    info

    Universidad de Oviedo

    Oviedo, España

    ROR https://ror.org/006gksa02

Erakutsi afiliazioak +
Liburua:
Avances de la geomorfología en España, 2010-2012: actas de la XII Reunión Nacional de Geomorfología, Santander, 17-20 septiembre de 2012
  1. González Díez, Alberto (coord.)

Argitaletxea: PubliCan-Ediciones ; Universidad de Cantabria

ISBN: 978-84-86116-54-5

Argitalpen urtea: 2012

Orrialdeak: 255-258

Biltzarra: Reunión Nacional de Geomorfología (12. 2012. Santander)

Mota: Biltzar ekarpena

DIALNET GOOGLE SCHOLAR

Laburpena

The application of 3D Terrestrial Laser Scanner (TLS) for topographic data sampling, and also its relevant capability to improve detailed 3D terrain models, are commonly applied to a large variety of scientific and technical analyses, such as geomorphology, archaeology and historical heritage studies. This work presents the application of TLS to the Neanderthal Site of “El Sidrón” Cave (Piloña, Asturias). The detailed different topographic analyses carried out in the area are strictly focused on the establishment of relationships between the endo- and exokarstic evolution of the cave system. In other words, on the evolution of the geomorphological evolution of the karstic complex directly related with the Neanderthal site. The TLS terrain model of the “Galería del Osario” presented here helps to put constraints on the geometrical relationships between endo- and exokarstic features, giving support to the analysis of probable ancient connections between these two environments.

Datuen iturria: Dialnet