周辺の天然記念物・トップ6

Beautiful striking landscape. Towards Dehesas de Guadix it starts to climb. After all we leave the valley of the Rio Fardes and drive to the valley of the rio Guadahortuna.

Googleによる翻訳•原文を表示

Beautiful road through the northern part of the Hoya de Guadix, along the Rio Fardes. The Hoya de Guadix is a tectonic depression that has been filled over millions of years with sediments from the surrounding mountain ranges. These sediments contain clay, sand, marl and gypsum, which contribute to the specific erosion patterns. The landscape is often dry and semi-arid, with clay hills and sandstone formations eroded by erosion known as "badlands" or in Spanish "cárcavas". These formations create a unique and sometimes alien-looking landscape with different colors, ranging from white and ochre to red and purple.

Googleによる翻訳•原文を表示

Hydrogeological studies show that the thermal waters of Alicún de las Torres come mainly from the carbonate aquifer of the Sierra de Baza and, to a lesser extent, from the waters of the Mencal aquifer. Scientists estimate that the aquifer is located at a depth of at least 650 to 800 meters.

Googleによる翻訳•原文を表示

The Troil Canal. According to scientists, they date back at least 3600 years ago. Due to the precipitation of calcium carbonate, these canals grew and continuously formed these amazing walls (some of them are 4 meters wide at the base, less than a meter wide at the top, 15 meters high and reach a length of almost 750 meters

Googleによる翻訳•原文を表示

A very interesting natural phenomenon that goes back to the first humans and beyond. An old calcareous water source that has been building itself for many thousands of years to the wall it has become today. At the top, the water still flows abundantly through the source. The water is still clearly visible on the road side, as the surrounding ground is even higher.

Googleによる翻訳•原文を表示

Special natural phenomenon that goes back to the first people and beyond. An old calcareous water source that has been building itself for many thousands of years to the wall it has become today. At the top, the water still flows abundantly through the source. The water is still clearly visible on the road side, as the surrounding ground is even higher.

Googleによる翻訳•原文を表示

The aqueduct or Acequia del Toril, is a travertine formation (porous limestone), in the form of a wall.

Googleによる翻訳•原文を表示

Rock formations through minerals from the water.

Googleによる翻訳•原文を表示

The aqueduct or Acequia del Toril, is a travertine formation (of porous limestone), in the form of a wall. It has a winding route, just over 1.5 kilometers long, which makes it very stable, reaching at some points more than 10 meters high. The thickness of its walls is variable, in the higher channel the thickness of the walls reaches three meters at its base and 70 centimeters at its highest part, where the water flows. The Acequia del Toril, is formed by porous limestone. It has been created by nature without the help of man, over the millennia. Of course, since the arrival of the first settlers in the area, already in prehistoric times, they used this water channel to supply a settlement from one of the eight hot springs in the environment.

Googleによる翻訳•原文を表示