As its name suggests, the two rocky peaks rise side by side in the shape of a horse's ear. Interestingly, the eastern peak is called Sumaibong Peak and the western peak is called Ammaibong Peak by adding male and female to the name of the peak. Ammaibong Peak is a little higher (687.4m, and Summaibong Peak is 681.1m). Ammaibong Peak was reopened in 2014, and many people ignored it lightly even though it was part-time. Perhaps that is why the part-time system was abolished. However, for safety, let's refrain from hiking at night and dawn. Yongdam Dam can be seen faintly near the summit of Ammaibong Peak. However, you can't see it at Yongdam Dam.
Let's look at some of the hiking trails on the Maisan sign that don't have them. For example, the Taejagul-Kwanggwangbong section. It is difficult to find a way at both entrances because it is buried in the Hapmisanseong-Gwanggwangbong section.
As for the difficulty of hiking, Ammaibong Peak is high, and the way up and down are divided, and there is a hiking trail that is a bare rock in the middle, so please refer to it. If you twist your foot once, it can lead to serious injury, so let's hold onto the railings installed on the left and right sides and go up.[1] For reference, these slopes reach 6-70%, so if you don't fit your healthy physical strength, you may gasp in the middle or give up on the way and go down the mountain, so let's take care of it properly. Perhaps because of the climbing route made up of bare rocks in that part of the section, from mid-November to mid-March of the following year, the entrance will be completely controlled for safety.
On the contrary, roads that are not on most Maisan signs are drawn with oil pens on some signs. It's a real road, so let's relax. Or there's a road that's not on any sign. Typical section is the observatory-Gogeumdang section. If you don't go back because you missed the way to Nambu Mai Mountain, there are two roads to Nambu Mai Mountain on the way. It's pierced wonderfully well why it's not on the sign.
Geologically, it is not surprisingly granite. In the distant Mesozoic era, the entire Gyeongsang-do and Jeolla-do areas, including this area, were freshwater lakes.[2] It is said that the crustal change occurred 70 million years ago, and the rock mass formed by the solidification of the sedimentary layer at the bottom of the lake rose to become a mountain due to this fold. Fossils of freshwater fish are unearthed as evidence. In addition, due to the characteristics of the sedimentary layer, it is considered a representative example of the Tafoni topography in topography.[3] The rock body of Maisan Mountain is a conglomerate in which gravel is embedded all over the place in a sedimentary layer made of sand and mud, and the gravel has fallen off due to weathering and erosion for a long time, and only the place where the gravel was located is recessed. It is estimated that the stone pagoda built under the peak is also related to the weathering of Maisan Mountain, which led to a lot of gravel being separated. Therefore, it is a stone mountain, but not granite.
Source: Namuwiki
#Maisan #Jeollabuk-do #Maisandrone
6 окт 2024
