Company: JUPGF
Filing Date: 2025-09-15
Form Type: F-1
Source: 0001493152-25-013292
Chunk: 90

Company: ATLAS CRITICAL MINERALS Corp
Filing Date: 2025-09-15
Form: F-1
Chunk 90
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REO (ppm) |     |             |   451 |     |             |   402 |

<div align='center'>Table 19 – Average contents in surface samples in Blocks 1 and 2.</div>

The samples from Blocks 1 and 2, as well as the high grades, are well distributed throughout the occurrence of the Mata da Corda Group within these areas, indicating lateral continuity for the mineralization of the unit. These samples reflect the occurrence of outcrops, which mostly occur in the slope region, so the plateau region has a smaller number of samples or even lower grades.

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<div align='center'>Figure 22 – Top whole rock sample results in the Alto Paranaíba Project.</div>

Block 1

Our mineral rights of Block 1 (832.698/2024 and 832.699/2024) have profiles with large thicknesses (~110 meters) of outcropping Capacete Formation (Figure 23 and Figure 24), potentially being a type of deposit similar to that of Resouro. The Mata da Corda Group occurs from elevations of 945m to 1050m, with a lateritic cover, suggestive of alteration of the Mata da Corda, overlapping the formation from 1050m to 1100m (Figure 25). The volcanic rocks present magnetism, mostly with an aphanitic texture, locally porphyritic or with amygdalae. Volcanic breccias also occur. The Capacete conglomerate has strong magnetism, is mostly polymictic (clasts of various types) and supported by the matrix, composed of green or reddish clay (Figure 26).

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Detailed mapping observed intercalations of volcanic rock (“Patos Formation”) with sedimentary rock, with laterally restricted continuities. Sampling showed high levels of TREO and TiO 2in samples dispersed in the areas and at different topographic elevations. Significant levels of magnetic rare earths oxides (“MREO”) are also found in the areas (Figure 24).

<div align='center'>Figure 23 – Block 1 representative TREO and TiO 2sample grades.

Figure 24 – Block
1 representative MREO sample grades.

Figure 25 – Block 1 stratigraphic profiles, showing thick layers of conglomerates from the Capacete Formation and the Patos Formation.</div>

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<div align='center'>Figure 26 – Cong