알콘타르‬에서 가장 멋진 ‪4‬개의 천연기념물

Calar Alto 정상 근처의 Sierra de los Filabres를 지나고 있다면, 해발 1882미터에 위치한 Fuente La Merendera는 거의 필수적인 정류장입니다. 이 샘물은 산의 변성암에서 솟아나는 신선한 물로 유명합니다. 공식적으로는 식수가 아니라는 경고 표지판이 있지만, 그렇다고 해서 이 지역 주민들과 많은 행인들이 물을 길어오기 위해 줄을 서는 것을 막지는 못합니다. 하지만 마시기 전에 물을 여과하는 것이 좋습니다. 긴 휴식이 필요하다면, 길 건너편에는 테이블, 바비큐 시설, 멋진 전망을 갖춘 휴게 공간이 있습니다.

Wow

Both mountain ranges ensure that it hardly rains in this semi-desert area.

시에라 데 바자(Sierra de Baza)와 시에라 데 로스 필라베레스(Sierra de Los Filabres)는 그라나다와 알메리아 주에 위치한 2,000미터 이상의 고지대에 있는 외딴 산맥의 일부이며, 배드랜드(Badlands) 지역 중 가장 고립된 곳입니다. 이 산맥은 역사적인 문화 교차로였으며, 그 유산에는 로마 수도교나 아랍 성곽의 유적이 포함되어 있습니다. 산맥의 가장 높은 지점에는 상징적인 칼라르 알토 천문대(Calar Alto Observatory, 2,168m)가 있으며, 멀리서도 쉽게 알아볼 수 있습니다. 이 산맥에는 또한 이베리아 반도에서 가장 상징적이고 장관을 이루는 산악 도로 중 하나인 엘 푸에르토 데 벨레피케(el Puerto de Velefique, 1,820m)가 포함되어 있으며, 남쪽 면의 많은 헤어핀 커브로 인해 인기가 있습니다. 시에라 데 로스 필라베레스의 남쪽 경계는 타베르나스 사막의 북쪽 관문으로 여겨지는 게르갈(Gérgal) 마을에 이릅니다.

La Encina del El Marchal del Abogado seems to emerge from a world of beings from fairy tales. It is an example of those rare botanical individuals that has survived thousands of years, witnessing the passage of time and the radical transformations of its environment. The common sense of the people, the overwhelming logic has protected them for generations and has allowed them to survive over so many years, tree species that are part of the bustle of people, peoples and their history. In the Almanzora Valley there is an important and still unknown tree mass cataloged and singled out in aspects as diverse as its longevity, a capricious morphology, height or its symbiosis with the nearby population. The Encina del El Marchal del Abogado, located in the municipality of Serón, is an obvious example due to its unique shape, since it offers a perimeter of trunk that exceeds six meters and symbolizes, together with the Poplar of El Marchal del Abogado, a set of opposites that represent the versatility of the arboreal world and evoke the well-known couple of knight and squire. Close to the Sierra de Baza Natural Park, in addition to the area's interesting monumental and ethnographic heritage (Las Menas de Serón mines), the headwaters of the Almanzora offer an interesting Greenway for non-motorized enjoyment. This unique botanical specimen is part of an excellent group of unique trees that dot the Almanzora Valley and its slopes: Acerolo del Cortijo de las Iglesias, Cornicabra del Puente de El Valle, Encina de El Marchal de El Abogado, Poplar de El Marchal de The Lawyer, Encina de la Fuente el Pino, Encina de los Trébedes and Olivo de las Lomas.

Outcrops of carbonate alpujárrides materials that are what make up the aquifer. The schists, phyllites and quartzites define the eastern and northern impervious substratum and edges, while contributing to the compartmentalization of the aquifer due to the existence of numerous tectonic scales. The southern and western limits are occupied by Miocene and Plioquaternary materials, which except those that make up the alluvial of the Almanzora River are of low permeability. The thickness of the limestone and aquifer dolomites is estimated at 300 m. The feeding of the aquifer comes from the direct infiltration of part of the rain that falls on the permeable outcrops and from the surface run-off waters, coming from the shales and phyllites of the environment. The discharge is produced by boreholes and by springs and galleries located on the southern edge. This group of springs emerges together with a group of small Triassic carbonate outcrops that emerge in the Almanzora valley, in the middle of the Miocene loamy pack. The waters of these springs present the peculiarity of being slightly thermal (28 ° C or more), the most important being Cela, Perica, Cañada y Plaza, Algibe and Huelago. This thermalism is also manifested in certain soundings, some of which are upwelling. The springs and galleries that are controlled show flows with slight decreases with a contribution of 3 to 4 Hm3 / year. The evolution of levels and flows of springs reveals the compartmentalisation of the aquifer in different blocks. Like the Cela spring, the Fuencaliente upwellings are possibly linked to the existence of an important fracture, or zone of fractures forming the "horst" of Fuencaliente, parallel to the edge of the Almanzora depression, thanks to which the emergence of water will take place, which would have circulated in depth through the carbonate formations of alpujarrides units.

The water from Fuente Perica comes from carbonated alpujárrides materials. Schists, phyllites and quartzites define the eastern and northern impermeable substrate and edges, while contributing to the compartmentalization of the aquifer due to the existence of numerous tectonic scales. The southern and western limits are occupied by Miocene and Plioquaternary materials, which, except for those that make up the Almanzora River alluvial, are of low permeability. The thickness of the aquiferous limestones and dolomites is estimated at 300 m. The supply of the aquifer comes from the direct infiltration of part of the rain that falls on the permeable outcrops and surface runoff water, coming from the surrounding schists and phyllites. The discharge occurs through boreholes and through springs and galleries located on the southern edge. This group of springs emerges together with a group of small Triassic carbonate outcrops that outcrop in the Almanzora valley, in the middle of the Miocene loamy package. The waters of these springs have the peculiarity of being slightly thermal (28 °C or more), the most important being Cela, Perica, Cañada and Plaza, Algibe and Huelago. This thermalism is also manifested in certain wells, some of which are springs. Like the Cela spring, the Fuencaliente, Perica and Algibe springs are possibly linked to the existence of an important fracture, or zone of fractures forming the Fuencaliente "horst", parallel to the edge of the Almanzora depression, thanks at which the emergence of the water that precisely would have circulated in depth will take place.

Bathing place and enjoy