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Item 2. Properties

2022-03-25 compared with 2021-03-31 · 31 added, 206 removed, 4 unchanged (98% of the section changed)

mineral properties are listed in the following table and summarized below.

Grande do Norte, Paraíba

Goiás,

Nickel/Cobalt

of our projects currently has reserves in accordance with the definition of such term by the SEC.

One of our projects

has had an NI 43-101 technical report issued (see details below).

projects owned by Jupiter Gold Corporation (an approximately 30% owned subsidiary) are summarized in the table below.

Gold provides details of its properties in its Annual Report on Form 20-F filed with the SEC.

Name & Location in Brazil

Project - Minas Gerais

Floresta –

- Goiás

Crixás

- Goiás

- Minas Gerais

of the Jupiter Gold Corporation projects currently has reserves in accordance with the definition of such term by

projects owned by Apollo Resources Corporation (an approximately 60% owned subsidiary)

are summarized in the table below.

Name & Location in Brazil

Piracicaba Project –

Iron Quadrangle, Minas Gerais

de Cocais Project –

Iron Quadrangle,

Project –

Iron Quadrangle, Minas Gerais

Mogol Project –

Project –

Corumbá

Mato Grosso do Sul

of the Apollo Resources Corporation projects currently has reserves in accordance with the definition of such term

our properties follow below.

lithium projects are listed in the following table with respective maps below.

Gerais Lithium Project

Minas Gerais Lithium Project encompasses 43 mineral rights for lithium in the Brazilian Western Pegmatite Province in the municipalities

of Araçuai, Coronel Murta, Itinga, Rubelita, Taiobeiras, and Virgem da Lapa.

Mineralizations are described in metric to

decametric pegmatite bodies, with tear geometry, with well-defined zoning, accessible both on surface and in galleries.

ore occurs as crystals of centimetric to metric sizes of spodumene among masses of lepidolite and albite.

We have a dedicated

exploratory geology team responsible for the detailed mapping, systematic sampling and analysis of the pegmatite occurrences within

our project area.

State of Minas Gerais

Infrastructure :

Paved highway, water, nearby electrical power grid

our Minas Gerais Lithium Project area there are schist and meta-gravels of the Salinas

Formation as well as schist of the Chapada Acauã

Formation outcrop, both with occurrence of cordierite and andalusite.

rocks are arranged in structures accommodating the deformation imposed by t granitic intrusions, which would be the parent material

in which the fluid responsible for the lithium mineralization’s was derived.

The structures to which the rocks of Fm.

Chapada Acauã

are conditioned, are the same responsible for the transport, accommodation, and accumulation of the

fluids responsible for the lithium mineralization.

Our project areas are marked by numerous occurrences of gemological and industrial

spodumene and has a decades-long history of mining in the region.

Lithium Project

Northeast Lithium Project encompasses 7 mineral rights for lithium in the surroundings of Parelhas and Jardim do Seridó,

State of Rio Grande do Norte, and São José

do Sabugi, State of Paraíba in Brazil.

The Borborema Province

located in the Northeast Region of Brazil has a wide variety of geological / tectonic environments that contain different types

of mineral deposits, varying between the classes of metals, non-metals, gems and precious metals.

The pegmatitic province of Seridó

corresponds to an important mining district located in the northeast of Brazil between the states of Paraíba and Rio Grande

This province is characterized by important mineral occurrences, which include several minerals with industrial application.

States of Rio Grande do Norte and Paraíba

Infrastructure :

Paved highway, water, nearby electrical power grid

our Northeast Lithium Project mineralizations are described in metric to decametric pegmatite bodies with exotic geometry, accessible

both at surface and in underground galleries.

Lithium ore occurs as crystals of varying size of spodumene and ambligonite, rarely

petalite, these develop in varying paragenesis.

In general, the fertile pegmatite bodies occur horst in the metasedimentary rocks

of the Seridó

Formation and Equador Formation, the latter being responsible for sustaining the relief.

Our project is located

within the Borborema Province, a macroregion of continental deformation accommodation, our mineral rights are arranged along large

dome structures generated at the time of ascent of lithium fertile bodies.

These structures are the same ones that condition the

accommodation of the pegmatite bodies containing lithium mineralization.

Our Northeast Lithium Project is marked by numerous occurrences

of industrial spodumene, which is treated as tailings from gem mines in the region.

Goiás/Tocantins

Rare Earths Project

Goiás/Tocantins Rare Earths Project is located within the states of Goiás and Tocantins in the Center-West of Brazil.

This Project is further divided into 2 component projects according to the local geology, Serra Dourada and Serra do Mendes.

Serra Dourada Project comprises three mineral rights.

One located SW of the state of TO, and one NW of the GO state.

We have confirmed

presence of all rare earth elements via geochemical sample testing.

The Serra do Mendes Project contains a mineral right located

in the NE region of the GO state.

States of Goiás and Tocantins

Infrastructure :

Paved highway, water, nearby electrical power grid

Goiás/Tocantins Rare Earth Elements Project is inserted within the Goiás Tin Province (PEG), which is developed

within the geological province of the Goiás Magmatic Arc.

The region is marked by numerous magmatic events that developed

in an orchestrated manner by the tectonics of the time.

The PEG is characterized by a zone with type A granitic intrusions rich

in tin and rare earth elements.

These fertile granites are responsible for the formation of supergene deposits with exotic minerals

such as fluocerite-Ce, ETR oxifluorides, bastnaesite, monazite, allanite, solid solutions of zircon-torite and xenotite-torite

in addition to apatite, rich in rare earth elements (REE).

PREG/T targets regions bordering the dome of these granites, since

it is understood that the REE-enriched deposits would form as regolith of the generating fertile granite, being formed by sediments,

transported and deposited in nearby depressions.

The area has a history of Sn deposits in PEG, so its potential for REE was not

explored until the last decade, after which the regions potential for world-class deposits was understood.

Rare Earths Project

Project is located in the SW portion of State of Bahia in the Northeast Region of Brazil.

The Project comprises a total of 5 mineral

State of Bahia

Infrastructure :

Paved highway, water, nearby electrical power grid

Bahia Rare Earth Elements Project is inserted within the regions of Serra do Ramalho

and Serra Pitarana which are located in the São Francisco sedimentary basin, an extensive Proterozoic cover of the São

Francisco Craton, where the Bambuí

Group, which is part of the upper part of the São Francisco Supergroup, is represented

by a thick carbonatic-pelitic sequence.

The Bambuí

Group sits directly on a gneissic–migmatitic base of the ancient

Archean crust, occurring sub-horizontally in the center-north portion of the area.

Serra do Ramalho stands out as one of the main

geomorphological features of the region.

It has a relatively flat top and steep flanks, with ruiniform or “lapiês”

erosional structures typical of the calcitic limestone dissolution processes, supported by the Sete Lagoas Formation limestone

Titanium Project is located in the central-western region of the state of Minas Gerais in Brazil, and is composed of 5 mineral

State of Minas Gerais

Infrastructure :

Paved highway, water, nearby electrical power grid

Titanium Projects target region is situated within the São Francisco Basin and approximately 60km from the alkaline carbonate

complex of Alto Paranaíba.

The complex is formed by carbonatitic intrusions of exotic chemistry associated with a local

paleo hotspot, this igneous activity influenced the percolation of fluids into the subsequent sediments generating the basic to

ultrabasic complexes of the Mata da Corda Group host in the rocks of the Bambuí

Group (São Francisco Basin).

is the rocks of this igneous complex (Mata da Corda Group) that host ilmenite mineralizations and form titanium deposits.

of Minas Gerais

Brazil Lithium Project

of Paraíba and Rio Grande do Norte

other strategic minerals properties are listed in the following table with respective maps below.

Earths I Properties

of Goiás and Tocantins

Earths II Properties

of Minas Gerais

Nickel/Cobalt

Nickel/Cobalt Project is located in the states of Goiás and Piauí

in Brazil, and composed of 3 mineral rights.

Nickel and Cobalt

States of Goiás and Piauí

Infrastructure :

Paved highway, water, nearby electrical power grid

Nickel/Cobalt Projects target region in the Goiás magmatic arc.

The region is marked by numerous intrusions enriched in

heavy elements.

The deposit is formed through supergene enrichment and soil formation, derived from ultramafic rocks from mantle

intrusions and therefore forms metric layers of soil with high Nickel and Cobalt contents.

Access to the mineralized layers occurs

on surface, facilitating blasting and exploitation operations.

In Piauí, the nickel deposits occur constrained to the fold

belts Riacho do Pontal.

This geological structure depicts tectonic stresses responsible for the rise of basic to ultrabasic fluids

that crystallize element-rich minerals such as Nickel and Cobalt.

The presence of these mineralized rocks added to the arid climate

of the region results in the formation of soil layers enriched in these elements, such as in Goiás.

Diamond Project is located in the State of Minas Gerais and comprises a total of 24

mineral rights, including 10 mining concessions, the highest level of mining title in Brazil.

All our diamond rights are located

along the banks of the Jequitinhonha River in the northern part of Minas Gerais.

This river rises within the Diamantina Plateau,

a region where more than alluvial diamond produced in the world for more than 200 years.

The Diamantina region stands out not only

for being the place where diamonds were first discovered in the country, in 1714, but also for being responsible for most of the

Brazilian production to date.

State of Minas Gerais

Infrastructure :

Paved highway, water, nearby electrical power grid

do Espinhaço is a mountain range that extends for more than 1,000 km, in a south-north direction, from the east of the

Quadrilátero Ferrífero (central region of Minas Gerais) to the border of the states of Bahia with Piauí.

Throughout this extension, diamonds occur in several locations, in addition to involving Chapada Diamantina, in the state of Bahia.

In this province, the diamond districts of Diamantina, Grão Mogol, Serra do Cabral and Itacambira are included.

do Espinhaço is mostly supported by quartzites, with subordinated phyllites and conglomeratic rocks, in addition to local

occurrences of metamagmatic rocks, all members of the Espinhaço Supergroup.

In the Diamantina region, the Espinhaço

Supergroup is subdivided into the Diamantina and Conselheiro Mata groups;

the first consisting mainly of continental sedimentary

deposits and the upper, by deposits of marine origin.

Such sedimentation occurred in a rift-type basin, which evolved during the

Paleoproterozoic and Mesoproterozoic periods.

diamonds in the latter area originated from the conglomeratic rocks of the Sopa-Brumadinho Formation, one of the units of the

Diamantina Group.

Primary rocks such as kimberlites or lamproites, even if metamorphosed, are not known along the mountain spike.

The main diamond rocks are conglomerates and loopholes in that formation, which flourishes mainly in the highest mountain portions.

Such rocks were sedimented in fluvial and alluvial fan systems, which probably collected diamonds from some area west of the mountain,

where the São Francisco River basin is currently located.

an original distribution of kimberlitic or lamproitic rocks, still unknown, the diamonds were initially invested in the conglomerates

and crevices of the Sopa-Brumadinho Formation.

From Proterozoic to recent, a complex multiphase evolutionary history of diamond

deposits present in this province can be summarized from data compiled from studies by several authors.

Although some of these

ages are not absolute, most of them are well established by radiometric dating (case of proterozoic deposits) or by fossils and

inferences about major climatic events at the regional level (case of phanerozoic deposits).

sand deposits are located on the banks and on the Jequitinhonha River in the state of Minas Gerais.

High-quality, commercial grade

sand for construction use is found in our deposits.

A professional mining engineer surveyor measured one of our deposits to contain

1,140,400 cubic meters of sand in the surveyed area, with an average modeled body thickness of 3.07 m, very close to the average

of 3.19 m found in the 13 sampled holes.

Several other deposits of similar size are thought to exist in our overall project area.

State of Minas Gerais

Infrastructure :

Paved highway, water, nearby electrical power grid

Nickel/Cobalt

II Properties

alluvial gold and diamonds, and industrial sand properties are listed in the following table with respective maps below.

Gold and Diamonds

Gold and Diamonds Mine

of Minas Gerais

Sand Mine I & Mine II

of Minas Gerais

of Our Properties

Minas Gerais Lithium Project

Northeastern Brazil Lithium Project

Rare Earths I Properties

Rare Earths II Properties

Titanium Properties

Graphite Properties

Nickel/Cobalt I Properties

Nickel/Cobalt II Properties

Titanium Properties

Alluvial Gold and Diamond Properties

Industrial Sand Properties

Legal Proceedings.

We are not a party to any pending legal proceedings

which we consider to be material.

are not a party to any material legal proceedings.

Mine Safety Disclosures.

Compared sentence by sentence after normalising whitespace, quotation marks, case and digits, so re-formatting and restated figures do not read as changed language. Wording changes appear as one removal and one addition. The current filing and the prior one are authoritative.

What changed 10-K

Item 2. Properties