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Marawat” or the “Concession”), located in the Eastern Desert of Egypt.

Drill Results

FOR IMMEDIATE RELEASE:

ATON ANNOUNCES FURTHER DRILL INTERSECTIONS FROM RODRUIN, INCLUDING 38M @ 1.84 G/T GOLD

FROM SURFACE

Vancouver, October 16, 2018: Aton Resources Inc. (AAN: TSX-V) (“Aton” or the “Company") is very pleased

to update investors with further exploration results from the Rodruin prospect, including assay results from

drill holes ROP-004 to ROP-007 completed during the ongoing reverse circulation percussion (“RC”) drilling

programme. Rodruin is located within the Company’s 100% owned Abu Marawat Concession (“Abu

Marawat” or the “Concession”), located in the Eastern Desert of Egypt.

Highlights:

• Assay results are now available from RC drill holes ROP-004 to R OP-007, testing gossan -hosted

mineralisation on the margins of Aladdin’s Hill at Rodruin . Drill hole ROP -004 has returned a

mineralised intersection of 38m @ 1.84 g/t Au from surface;

• Drill holes ROP -005 to ROP-007 all had to be abandoned at less than 10m depth after intersecting

large ancient underground workings, but all 3 holes intersected gossan-hosted mineralisation at or

very near to surface, including 2m @ 8.92 g/t Au (hole ROP -008) from 8m depth , prior to

abandonment;

• RC drilling is continuing, as is drill access road and pad construction. Drill roads and pads have been

completed in the Spiral Pit and Central Buttress areas, in the process exposing additional gossan-

hosted mineralisation. Aton is continuing to actively open up mineralisation for drill testing over large

areas of the South Ridge at Rodruin.

“These results continue to demonstrate the extent of the mineralised area around Aladdin’s Hill and the fact

that mineralisation extends below surface to depth. It also shows the potential of the large amount of ancient

workings that we have identified and mapped over the length of the South Ridge. It is amazing to think of the

thousands of ancient miners working over maybe hundreds of years who were chasing the rich deposit they

had found. Our ongoing drilling appears to have hit ancient workings down to 85 meters below surface, which

would make these amongst the deepest ancient workings found to date in Egypt. ’ said Mark Campbell,

President and CEO . “These results continue to confirm our belief that we are in a significant mineralised

system and one which we believe has large bulk tonnage at good grades, with high grade shoots interspersed

within. We are preparing to drill test along the length of the South Ridge to confirm this. We are planning to

be drilling until Christmas, when we will take a short break and return in early January.”

RC drilling at Rodruin

RC drilling commenced at Rodruin on August 27, 2018 (see news release dated August 28, 2018), with Aton

having contracted Capital Drilling to undertake the drilling using a track -mounted Gemrok MP-1000 multi-

purpose rig, which is capable of both RC and diamond drilling , operating with a large, truck -mounted

500psi/1300cfm compressor. The first phase of drilling is planned to consist of approximately 4,000 to 6,000

metres of RC drilling, with the drilling having started at the main zone of ancient workings and mapped

mineralisation in the Aladdin’s Hill area . Aton have mapped and identified gold mineralisation, much of it

gossan-hosted, and ancient workings over a large areal extent at Rodruin (see Figure 1), and plan to drill test

potential mineralisation in several locations, starting initially in the Aladdin’s Hill area, during the first phase

of drilling, in order to assess the overall prospectivity of the South Ridge.

Figure 1: Surface sampling plan of the Rodruin prospect, with showing location of individual point samples and channel sample profiles, and drill access roads and pads

Drilling commenced at Aladdin’s Hill at the western end of the Rodruin prospect (see Figure 2). Surface rock

chip sampling of highly altered rocks at Aladdin’s Hill has returned an average grade at surface of 3.75 g/t Au

(see news release dated September 4, 2018), and drill hole ROP -003 testing this zone has returned an

intersection of 36m @12.47 g/t Au (see news release dated October 1, 2018). Surface channel sampling

around Aladdin’s Hill, as well as other areas (see Figures 1 and 2), has recently returned significant and wide

mineralised intersections including 65.3m @ 2.84 g/t Au and 5.26% Zn from gossanous carbonates and slates

(see news release dated September 24, 2018), indicating the potential development of mineralisation over a

wide area away from the main workings at Aladdin’s Hill. Visible gold in highly altered rocks has also been

identified in outcrop at Aladdin’s Hill, as well as other areas, including the Spiral Pit.

Figure 2: Schematic geological plan of the Aladdin’s Hill area, showing location s of drill holes ROP-001 to ROP-007

Results of drill holes ROP-004 to ROP-007

Assay results are now available for the drill holes ROP-004 to ROP-007, which were all drilled on a southerly

orientation around the margins of the main Aladdin’s Hill workings (see Figure 2) to test gossan -hosted

mineralisation mapped at surface . Details of the collar locations are provided in Table 1. 3 of the 4 holes

intersected ancient workings very near to surface, with these holes being abandoned at depths of between

5 and 10m, but hole ROP -003 returned a significant mineralised intersection from surface . Mineralisation

was intersected in all 4 holes, and details of the gold-zinc mineralised intersections are provided in Table 2.

All 4 holes targeted zones of gossa n-hosted mineralisation on the margins of the main ancient workings at

Aladdin’s Hill, and intersected gold -zinc (-silver) mineralisation. Hole ROP-004 to the east of A laddin’s Hill

returned a significant intersection of 38m @ 1.84 g/t Au from surface (see Table 2). This hole also intersected

several narrow voids, believed to be ancient underground mine workings and stopes. Hole ROP -005

intersected mineralisation from surface, increasing in grade before a large void was hit at 4m, which could

not be drilled through. Furthermore the large pad from which holes ROP-004 and ROP-005 were drilled had

to be abandoned, due to the presence of previously unidentified workings and voids only a couple of metres

below ground level.

Hole ID

Collar co-ordinates1

Dip Grid

Azimuth

EOH

depth (m) Comments

X Y Z

ROP-004 552382 2913017 779 -70 190 50 Several ancient workings and

voids

ROP-005 552395 2913015 778 -70 170 5 Hole abandoned at 5m, due to

ancient workings

ROP-006 552309 2913025 783 -55 190 5 Hole abandoned at 5m, due to

ancient workings

ROP-007 552310 2913030 784 -55 190 10

Hole abandoned at 10m, due to

ancient workings (same as hole

ROP-006?)

Notes:

1) Surveyed collar co-ordinates

2) All co-ordinates are UTM (WGS84) Zone 36R

Table 1: Collar details of RC drill holes ROP-004 to ROP-007

Holes ROP-006 and ROP -007 were drilled on the westernmost pad at Aladdin’s Hill, and were designed to

test gossanous carbonate -hosted mineralisation. Hole ROP-006 was abandoned at 5m after intersecting a

large underground void, but intersected mineralisation from surface. The rig was stepped back, and hole

ROP-007 was collared behind ROP -006 but this again intersected a large void, presumed to be d epth

extension of that in ROP -006, and again had to be abandoned. Encouragingly this drill hole intersected 2

metres of high grade mineralisation, on the margins of the underground stope.

Hole

ID

Hole

depth

(m)

From To Interval Au

(g/t)

Ag

(g/t)

Zn

(%) Comments

ROP-004

50 0 38 38 1.84 14.6 0.86 Mineralisation in gossanous

carbonates, with numerous

ancient workings and voids incl. 0 11 11 2.62 12.9 0.44

incl. 18 30 12 2.40 15.4 1.51

ROP-005 5 0 4 4 0.78 2.3 1.13

Hole abandoned at 5m, after

intersecting large ancient

workings, NSR from 4m

ROP-006 5 0 5 5 1.21 3.6 0.82

Hole abandoned at 5m, after

intersecting large ancient

stope

ROP-007 10 8 10 2 8.92 3.5 0.49

Hole abandoned at 10m, after

intersecting large ancient

stope (same as hole ROP-006)

Notes:

1) Intersections based on a nominal cutoff grade of 0.5 g/t Au. Internal waste intervals are partially determined by geological

considerations, as well as width

2) Cu values in all quoted intersections <0.07% Cu , and lead <0.15% Pb

Table 2: Mineralised intersections from RC drill holes ROP-004 to ROP-007

While it was clearly disappointing that 3 of the latest holes were unable to penetrate through substantial and

hitherto unmapped ancient underground workings, their presence is nonetheless encouraging and indicative

of gold mineralisation in gossanous carbonate rocks at Rodruin, as anticipated. Hole ROP-004 intersected

significant gold mineralisation from surface, and the confirmation of gold mineralisation in this material from

drill holes is most encouraging as large areas of gossanous material have been mapped a t surface on the

South Ridge at Rodruin. The results from the latest batch of drill holes adds credence to the Company’s belief

that drilling will intersect significant mineralisation over wide areas of the South Ridge at Rodruin, and that

these broad zones are also likely to carry significant high grade zones within them. The results of the initial

drilling, as well as access road and pad construction, are also confirming significant structural complexity at

Rodruin, as mapped at surface, with significant dislocation of mineralised zones (see Figure 3). Aton is actively

working to open up mineralisation over as large an area as is possible for drill testing in the ongoing Phase 1

RC programme.

Activity Update

• Construction of drill access roads and pads is ongoing at Rodruin to support the current Phase 1 RC

drilling programme. New drill pads have been constructed at the Spiral Pit (see Figure 3), and on the

“gossan road” high on the Central Buttress of the South Ridge . One of the excavators onsite is now

progressing towards the GF Zone, so me 500m SE of Aladdin’s Hill to open up another large area of

gossanous mineralisation mapped at surface for drill access (see Figure 1).

• Sampling of channel profiles ROC-018 to ROC-022, to test mineralisation exposed in access roads (see

Figure 1), has now been completed. Initial assay results are expected from these profiles shortly, and

it is expected that these will help to define further mineralisation at surface, away from the

immediate Aladdin’s Hill area. Further mineralisation has been exposed in new access roads,

including a lower road below the “gossan road” (see Figure 1), which is progressing towards the

Central Buttress to allow access for drill testing a large area of mapped gossan and ancient workings

on the Central Buttress.

• Drilling was temporarily suspended at Rodruin in late September, due to various mechanical

problems with the rig, and issues with drill hole surveying. Capital have worked diligently to resolve

all these issues, and drilling is now back underway again.

Figure 3: Fault truncating gossan-hosted mineralisation below the Spiral Pit in new drill pad. The entrance to the

Spiral Pit, which appears to follow several structures including the one pictured above , and has returned assays

including 35.3 g/t and 20.6 g/t Au, is visible immediately above the fault. The gossan-hosted mineralisation

returned a surface intersection of 24m @ 2.27 g/t Au in channel sample profile ROC-017 immediately to the SE of

this fault, and is overlain and largely covered at surface by unmineralised carbonate seen in the top and top left of

the photo. This carbonate unit comprises the overthrust block, above the main thrust fault mapped in Figure 2.

Drilling and sampling procedures

Drill holes were drilled at c. 140mm diameter, and the bulk percussion chip samples were collected directly

into large plastic bags from the cyclone every metre, numbered with the hole number and hole depths by

the drill crew, and laid out sequentially at the drill site. RC chips were logged onsite by a senior Aton geologist.

The bulk 1m samples were weighed, and subsequently riffle split through a 3-tier splitter onsite by Aton field

staff to produce an approximately 1/8 split, which was collected in cloth bags, numbered and tagged wit h

the hole number and depth. The reject material from this initial bulk split was re-bagged, labelled and tagged,

and the bulk reject samples will be stored and retained on site at Rodruin. A representative sample of each

metre was washed, stored in marked plastic chip trays, each containing 20m of samples, photographed, and

retained onsite as a permanent record of the drill hole (see Figure 4).

Figure 4: Composite image of the ROP-004 chip trays. Mineralisation can be seen to be associated with weather ed

and gossanous carbonate rocks (brown), which occur to a depth of 41m before the hole passes into green altered

slates

All the 1m split samples were weighed again, and the samples selected for assay were riffle split onsite,

typically a further 3 -4 times using a smaller lab splitter, to produce a nominal c. 250-500g sample split for

dispatch to the assay laboratory. All sa mples were sent for assay from holes ROP -004 to ROP -007. The

laboratory splits were allocated new sample numbers. QAQC samples were inserted into the sample runs

dispatched to the assay laboratory at a nominal rate of 1 duplicate sample for every 10 drill samples, 1 blank

sample every 10 samples, and 1 standard sample of a certified reference material every 40 samples. Reject

material from the 1m samples after the laboratory split had been taken, and any unused 1m splits will be

retained at the Company’s Hamama laboratory for future reference purposes, as and when required.

The selected c. 250-500g split samples were shipped to ALS Minerals at Rosia Montana, Romania for analysis.

Samples were analysed for gold by fire assay with an atomic absorption spectro scopy (“AAS”) finish

(analytical code Au -AA23); and silver, copper, lead and zinc with an aqua regia digest followed by an AAS

finish (analytical code AA45). High grade gold samples (>10 g/t Au) were re -analysed using analytical code

Au-AA25 (also fire assay with an AAS finish). High grade Ag and base metal samples (Ag >100 g/t, and Cu, Pb,

and Zn >10,000ppm or >1%) were re-analysed using the ore grade technique AA46 (also an aqua regia digest

followed by an AAS finish).

Rodruin

The Rodruin prospect was di scovered in December 2017 by Aton geologists (see news release dated

December 14, 2017), and is located approximately 18km east of the Company’s Hamama West mineral

deposit (see Figure 5). Field mapping and sampling has indicated the presence of ancient mine workings and

extensive gold mineralisation over an area of at least 700m x 400m at surface. Abundant visible gold has been

identified in hand specimens from surface outcrops, and ancient dumps and underground workings, with

individual selective grab samples assaying up to 321 g/t Au. The main series of extensive ancient underground

workings in the Aladdin’s Hill area has also been sampled to a depth of approximately 40m below ground

level, indicating continuation of the surface mineralisation at depth (s ee news releases dated February 6,

2018, March 5, 2018 and April 16, 2018), and drilling has now confirmed the presence of high grade gold

mineralisation with individual samples returning assays of up to 221 g/t Au over metre intervals.

Underground working s at the Spiral Pit have been sampled to a depth of 12 -15m below ground level,

returning assays of up to 35.3 g/t Au and 37.9% Zn (see news release dated August 7, 2018).

Figure 5: Abu Marawat regional geology, showing the location of the Rodruin prospe ct

About Aton Resources Inc.

Aton Resources Inc. (AAN: TSX-V) is focused on its 100% owned Abu Marawat Concession (“Abu Marawat”),

located in Egypt’s Arabian-Nubian Shield, approximately 200km north of Centamin’s Sukari gold mine. Aton

has identified a 40km long gold mineralised trend at Abu Marawat, anchored by the Hamama deposit in the

west and the Abu Marawat deposit in the east, containing numerous gold exploration targets, including three

historic British mines. Aton has identified several distinct geological trends within Abu Marawat, which

display potential for the development of RIRG and orogenic gold mineralisation, VMS precious and base

metal mineralisation, and epithermal -IOCG precious and base metal mineralisation. Abu Marawat is over

738km2 in size and is located in an area of excellent infrastructure; a four-lane highway, a 220kV power line,

and a water pipeline are in close proximity.

Qualified Person

The technical information contained in this News Release was prepared by Javier Orduña BSc (hons), MSc,

MCSM, DIC, MAIG, SEG(M), FGS, Exploration Manager of Aton Resources Inc. Mr. Orduña is a qualified person

(QP) under National Instrument 43-101 Standards of Disclosure for Mineral Projects.

For further information regarding Aton Resources Inc., please visit us at www.atonresources.com or contact:

Mark Campbell

President and Chief Executive Officer

Tel: +202-27356548

Email: [email protected]

Note Regarding Forward-Looking Statements

Some of the statements contained in this release are forward -looking statements. Since forward -looking

statements address future events and conditions; by their very nature they involv e inherent risks and

uncertainties. Actual results in each case could differ materially from those currently anticipated in such

statements.

Neither TSX Venture Exchange nor its Regulation Services Provider (as that term is defined in policies of the

TSX Venture Exchange) accepts responsibility for the adequacy or accuracy of this release.