2019
DOI: 10.1080/17445647.2019.1646675
|View full text |Cite
|
Sign up to set email alerts
|

Geomorphology of the Sierra del Aramo (Asturian Central Massif, Cantabrian Mountains, NW Spain)

Abstract: A detailed geomorphological map of the Sierra del Aramo (Asturian Central Massif) is presented at a scale of 1:25,000. The Sierra del Aramo is one of the major middle-altitude mountains of the Asturian Central Massif (maximum altitude 1,791 m a.s.l.). Specifically, the lithology and the structural landforms, as well as karst, fluvial, periglacial and other landforms and deposits, have been mapped based on meticulous fieldwork, photointerpretation and a geographic information system. The final printing has been… Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1
1

Citation Types

0
2
0

Year Published

2019
2019
2024
2024

Publication Types

Select...
3
2

Relationship

1
4

Authors

Journals

citations
Cited by 7 publications
(2 citation statements)
references
References 37 publications
(40 reference statements)
0
2
0
Order By: Relevance
“…The mineralization style observed is epithermal (epigenetic), specifically Cobalt-Copper-Nickel mineralization. This mineralization is found within specific stratigraphic limestone units of the Upper Namurian period in the Carboniferous Period 7 . The mineralization is controlled by significant Late Variscan structural controls, associated with both East-West and North-South faults and fractures.…”
Section: Aramo Areamentioning
confidence: 80%
“…The mineralization style observed is epithermal (epigenetic), specifically Cobalt-Copper-Nickel mineralization. This mineralization is found within specific stratigraphic limestone units of the Upper Namurian period in the Carboniferous Period 7 . The mineralization is controlled by significant Late Variscan structural controls, associated with both East-West and North-South faults and fractures.…”
Section: Aramo Areamentioning
confidence: 80%
“…The Sierra del Aramo is crowned by a karst platform over 1300 m a.s.l. whereas the Aramo hillsides are steep and present rectilinear slopes between rocky escarpments and debris deposits (Beato Bergua et al, 2019c). In general, the analyzed area experiences Atlantic conditions with annual rainfall between 1100 and 1500 mm (around 2000 mm on the summits) and mild temperatures (between 6 and 13°C).…”
Section: Study Areamentioning
confidence: 96%