On. tion.2 ofFigure 1. (A) Place of Mudeungsan within the southwestern Korean Peninsula. (B) Geological map Figure 1. (A) Place of Mudeungsan within the southwestern Korean Peninsula. (B) Geological Figure 1. (A) Location of Mudeungsan within the southwestern Korean Peninsula. (B) Geological map of Mudeungsan (geological details was obtained from Lim et al. (2015)). Locations of the map of Mudeungsan (geological details was obtained from Lim et al. (2015)). Areas of your of Mudeungsan (geological information was obtained from Lim et al. (2015)). Areas Mudeungsan tuff samples are shown as white circles. The location marked using a red circle was re of the Mudeungsan tuff samples are shown as white circles. The area marked having a red circle was reported Mudeungsan tuff samples are shown as white circles. The region marked with a red circle was re ported to become Mudeungsan tuff by Lim et al. (2015).ported to be Mudeungsan tuff by Lim et al. (2015). to become Mudeungsan tuff by Lim et al. (2015).Figure two. (A) Ipseokdae rock (ISD) and talus that was formed by the collapse of columnar joints are shown. Ice rock (IR) is located beyond the scope of this photo. (B) Baekma ridge (BN), Nakta peak (NT), and Anyang peak. (Anyang). BN will be the ridge on the mountain. (C) Closeup view of ISD. (D) Figure 2. (A) Ipseokdae rock (ISD) and talus that was formed by the collapse of columnar joints are shown. Ice rock (IR) is View of IR. This was observed along the trail. Figure 2. (A) Ipseokdae rock (ISD) and talus that was formed by the collapse of columnar joints are situated beyond the scope of this photo. (B) Baekma ridge (BN), Nakta peak (NT), and Anyang peak. (Anyang). BN may be the shown. Ice rock (IR) is located beyond the scope of this photo. (B) Baekma ridge (BN), Nakta peak ridge in the mountain. (C) Close-up view of ISD. (D) View of IR. This was observed along the trail.(NT), and Anyang peak. (Anyang). BN is definitely the ridge of your mountain. (C) Closeup view of ISD. (D) View of IR. This was observed along the trail.Appl. Sci. 2021, 11,3 of2. Supplies and Procedures Whole-rock samples in the Mudeungsan tuff have been processed into powder, and SiO2 , Al2 O3 , TiO2 , Fe2 O3 , K2 O, Na2 O, CaO, MgO, MnO, and P2 O5 abundances had been measured working with X-ray fluorescence spectrometer (SHIMADZU XRF-1700) at the in the National Center for Interuniversity Research Facilities (NCIRF) at Seoul National University (SNU), Republic of Korea. Safranin MedChemExpress Analytical error was within 0.1 based on rock-based requirements, and loss on ignition (LOI) values were calculated by weight just before and right after igniting GYY4137 Epigenetics powder samples at 950 C. Measured key element compositions are shown in Table 1.Table 1. Big element compositions on the Mudeungsan tuff samples (in wt. ). SiO2 ISD-1 ISD-2 IR-1 IR-2 BN-1 BN-2 NT-1 Anyang Typical 64.64 64.53 64.73 64.53 65.09 64.83 64.24 64.55 64.64 Al2 O3 16.16 15.91 15.75 15.56 16.07 15.57 15.93 15.54 15.81 TiO2 0.58 0.56 0.57 0.58 0.58 0.57 0.59 0.59 0.58 Fe2 O3 4.61 4.41 four.52 four.59 four.44 4.45 4.60 four.52 four.52 MgO 1.55 1.51 1.60 1.58 1.44 1.45 1.56 1.48 1.52 CaO 4.11 four.09 four.21 4.00 three.86 3.84 4.08 3.67 3.98 Na2 O 3.79 3.83 3.83 3.78 three.75 3.77 3.79 three.57 3.76 K2 O 3.17 3.22 three.11 3.31 three.34 three.23 three.20 3.34 three.24 MnO 0.09 0.09 0.ten 0.10 0.08 0.09 0.09 0.09 0.09 P2 O5 0.19 0.19 0.19 0.19 0.19 0.19 0.19 0.19 0.19 LOI 1.08 1.61 1.34 1.75 1.06 1.98 1.70 two.39 1.The high-resolution synchrotron XRD evaluation in the selected rock samples was measured at the.