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Goldshore Reports Additional Step-Out Intercepts on the Margin of the Main Zone at Moss Lake, Ontario Visible Gold Discovered in Unsampled Historic Drill Core

Exploration Programs

Goldshore Reports Additional Step-Out Intercepts on the

Margin of the Main Zone at Moss Lake, Ontario

Visible Gold Discovered in Unsampled Historic Drill Core

VANCOUVER, B.C., April 19, 2022: Goldshore Resources Inc. (TSXV: GSHR / OTCQB: GSHRF

/ FWB: 8X00) (“Goldshore” or the “ Company”), is pleased to announce assay results from its

ongoing 100,000-meter drill program at the Moss Lake Project in Northwest Ontario, Canada.

Drilling is aiming to better define and expand high -grade structural zones within the Moss Lake

deposit in an attempt to improve the overall grade and volume beyond that of the historic Mineral

Resource.

Key Highlights

• Drilling of the Main Zone has expanded the zone and provided better definition

for high grade corridors: Drilling within the Main Zone has continuity to improve the

continuity and volume of high grade zones within the Main Zone. Highlight intercepts

include:

o 13.0m @ 1.25 g/t Au from 192.0m in MMD-22-011

o 29.75m @ 1.03 g/t Au from 33.0m in MMD-22-012A

o 13.0m @ 1.02 g/t Au from 238.0m in MMD-22-013

• Parallel structures intersected on every section: Drilling continues to intersect new

mineralized structures parallel to the main body of mineralization, within a 100 metre

corridor along the northern hanging wall side of the Main Zone (see Plan View Figure

4).

• Visible gold found in unsampled section of historic drillholes: Sampling of

previously unsampled drill core has found visible gold confirming the Company’s belief

that historic exploration missed parallel zones of mineralization . All a ssays from

historic core remain pending.

• West edge of the Main Zone defined : Drill holes MMD-21-010, MMD-22-011 and

MMD-22-012A intersected a major post-mineralization structure that cuts the western

edge of the Main Zone and most likely offsets mineralization to the south where it is

reflected by the previously drilled Southwest Zone (See Figure 4).

Brett Richards, President and Chief Executive Officer of Goldshore commented : “Once

again, we are pleased to illustrate recent drill results from the Moss Lake Gold Project Inc.,

highlighting continued mineralization on the periphery of the historic resource in the main zone.

Referring back to the high grade feeder system identified from the March 2, 2022 press release

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News: Goldshore Drills 6.3 g/t Au over 58.85m at Moss Lake (goldshoreresources.com) as well

as the release on the VTEM geophysical survey indicating 29 new targets Technical Analysis:

Goldshore’s VTEM Results Greatly Expand the Prospectivity (goldshoreresources.com) , the

consistency of the mineralization continues to illustrate the size and scale of the Moss Lake

Project. The ongoing drilling is increasing our confidence in the extent and size of the high grade

corridors within the main zone deposit to be incorporated into future resource updates and

possible benefits to future mining. Additionally, the limited outside of the main zone has identified

several potential parallel zones that remain open along strike and down dip and remain one of

the focuses for this campaign. Also, the visible gold we are seeing in the historic core is a great

indication of higher grade areas that will guide us towards a greater understanding of the

geological controls in this system”.

Results have been received for drill holes MMD-21-010, MMD-22-011 and -012A evaluating the

western margin to the Main Zone and holes MMD -22-013 and -015 testing the southern margin

of the Main Zone. Significant drill intercepts are summarized in Tables 1 and 2, respectively,

shown in Figures 1-3 as drill sections. Table 3 and Figure 4 show the location of the drill holes.

Figure 1: Drill section through MMD-22-011 showing mineralized intercepts relative to the 2013 grade model

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Figure 2: Drill section through MMD-22-013 showing mineralized intercepts relative to the 2013 grade model

Figure 3: Drill section through MMD-22-015 showing mineralized intercepts relative to the 2013 grade model

4

Figure 4: Drill plan showing the drill holes relative to the 2013 resource model and historic drill hole location

Table 1: Significant downhole gold intercepts along western margin of Main Zone

HOLE ID FROM TO

HOLE

LENGTH

(m)

TRUE

WIDTH

(m)

CUT

GRADE

(g/t Au)

UNCUT

GRADE

(g/t Au)

MMD-21-010 38.15 42.00 3.85 2 0.34 0.34

MMD-22-011 163.00 166.10 3.10 1 0.54 0.54

190.45 231.35 40.90 19 0.54 0.54

including 192.00 205.00 13.00 6 1.25 1.25

395.20 429.00 33.80 16 0.51 0.51

502.00 508.00 6.00 3 0.42 0.42

525.00 537.55 12.55 6 0.31 0.31

548.45 596.75 48.30 23 0.34 0.34

including 560.00 562.55 2.55 1 1.59 1.59

621.50 625.40 3.90 2 0.31 0.31

661.00 664.00 3.00 2 0.54 0.54

723.25 726.00 2.75 1 0.85 0.85

758.00 760.20 2.20 1 0.61 0.61

777.70 780.90 3.20 2 0.43 0.43

794.00 825.00 31.00 16 1.07 1.07

including 795.00 807.00 12.00 6 2.18 2.18

MMD-22-012A 150.00 152.00 2.00 2 0.65 0.65

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296.00 298.00 2.00 2 0.39 0.39

329.65 336.00 6.35 5 0.49 0.49

352.00 358.95 6.95 6 1.98 1.98

including 358.55 358.95 0.40 0 28.8 28.8

377.85 382.00 4.15 3 0.73 0.73

410.00 412.00 2.00 2 0.54 0.54

474.00 484.50 10.50 9 0.41 0.41

including 479.00 481.00 2.00 2 1.11 1.11

Intersections calculated above a 0.3 g/t Au cut off with a top cut of 30 g/t Au and a maximum internal waste

interval of 10 metres. Shaded intervals are intersections calculated above a 1.0 g/t Au cut off. Intervals in bold

are those with a grade thickness factor exceeding 20 gram x metres / tonne gold. True widths are approximate

and assume a subvertical body.

Table 2: Significant downhole gold intercepts along southern margin of Main Zone

HOLE ID FROM TO

HOLE

LENGTH

(m)

TRUE

WIDTH

(m)

CUT

GRADE

(g/t Au)

UNCUT

GRADE

(g/t Au)

MMD-22-013 33.00 62.75 29.75 21 1.03 1.03

including 48.00 62.75 14.75 11 1.71 1.71

75.00 88.00 13.00 9 0.35 0.35

92.00 116.00 24.00 17 0.76 0.76

including 98.00 98.40 0.40 9 29.6 29.6

126.65 198.80 72.15 53 0.37 0.37

216.00 259.00 43.00 32 0.54 0.54

including 225.80 227.80 2.00 1 1.50 1.50

and 238.00 251.00 13.00 10 1.02 1.02

333.00 337.00 4.00 3 0.42 0.42

421.40 454.65 33.25 26 0.32 0.32

463.00 481.65 18.65 15 0.32 0.32

including 470.00 473.00 3.00 2 1.22 1.22

509.00 511.00 2.00 2 0.37 0.37

MMD-22-015 31.00 36.00 5.00 4 0.40 0.40

59.00 84.00 25.00 19 0.67 0.67

including 61.00 63.00 2.00 2 1.94 1.94

and 78.00 80.50 2.50 2 1.29 1.29

99.20 149.00 49.80 38 0.35 0.35

including 105.40 108.50 3.10 2 1.46 1.46

160.00 179.90 19.90 15 0.81 0.81

including 160.00 167.00 7.00 5 1.47 1.47

223.00 225.00 2.00 2 0.45 0.45

340.70 344.80 4.10 3 0.77 0.77

446.50 458.00 11.50 9 0.40 0.40

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482.00 484.00 2.00 2 0.55 0.55

491.95 494.00 2.05 2 0.45 0.45

530.65 534.90 4.25 4 1.11 1.11

Intersections calculated above a 0.3 g/t Au cut off with a top cut of 30 g/t Au and a maximum internal waste

interval of 10 metres. Shaded intervals are intersections calculated above a 1.0 g/t Au cut off. Intervals in bold

are those with a grade thickness factor exceeding 20 gram x metres / tonne gold. True widths are approximate

and assume a subvertical body.

Table 3: Location of drillholes

HOLE EAST NORTH RL AZIMUTH DIP EOH

MMD-21-010 668357 5378845 437 135 -45 501,0m

MMD-22-011 668659 5379089 428 155 -65 840.0m

MMD-22-012A 668453 5378938 429 135 -45 497.0m

MMD-22-013 669013 5379180 427 155 -45 513.0m

MMD-22-015 669128 5379246 427 155 -45 551.95m

Approximate collar coordinates in NAD 83, Zone 15N

MMD-21-010 and MMD-22-012A drilled the western extension of the Main Zone. MMD-22-012A

is a redrill of MMD-22-012 that was lost in overburden. MMD-22-011 drilled at -65° beneath MMD-

21-006 (reported on January 28, 2022) and skirted the northwestern margin of the mineralization

model estimated by InnovExplor in 2013.

All three holes intersected zones of altered and mineralized diorite with local zones of higher

grade (e.g., 0.4m @ 28.8 g/t Au from 358.55m in MMD -22-012A), showing that the mineralized

system continues. MMD-22-011 intersected mineralized diorite to a greater depth than the

InnovExplor 2013 model, as well as the now familiar parallel high grade structure to the south of

the Main Zone (31.0m @ 1.07 g/t Au from 794m depth). While this intersection is deep, the

structure almost certainly extends to surface as is indicated by drilling on parallel sections.

The drillholes are notable for intersecting a major post-mineralization fault zone that shaves the

western edge of the Main Zone and most likely offsets mineralization to the south where it is

reflected by the previously drilled Southwest Zone.

MMD-22-013 and MMD-22-015 were drilled at -45° along the southern margin of the Main Zone.

MMD-22-013 was drilled above MMD-21-008 (reported on March 2, 2022), which returned several

high grade intercepts.

Both holes intersected strongly altered diorite with low grade gold mineralization san dwiched

between the variably altered volcaniclastic wallrock sequence. They also intersected the parallel

structural zone to the south of the Main Zone. Local high grades were also intersected (e.g., 0.4m

@ 29.6 g/t Au from 98.0m in MMD-22-013).

Goldshore has been logging historic core throughout this campaign to maximise the value of the

historic drill core. As part of this program, the team has commenced resampling sections of

historic core that were not sampled in the past. This has been driven by the recognition of

additional zones of mineralization that were previously ignored.

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Recently, the team discovered visible gold in quartz-pyrite veinlets in drillhole NS-92-247 at 546.9

meters depth (Figure 5). This highlights the potential for high grades in previously unrecognized

zones parallel to the main targets. In this case, it is a parallel structure along the northern edge of

the QES Zone.

Figure 5: Visible gold in quartz-pyrite veinlet in NS-92-247

Peter Flindell, VP Exploration commented : “These assay results come from our pre -winter

drilling programme, which largely tested the margins of the main zone. Drilling continues to show

the continuity of mineralization wit hin the main zone and the existence of mineralization in a

southern parallel zone , which we hope points to a larger mineralized volume and potentially a

much bigger project.”

Analytical and QA/QC Procedures

All samples were sent to ALS Geochemistry in Thunder Bay for preparation and analysis was

performed in the ALS Vancouver analytical facility. ALS is accredited by the Standards Council of

Canada (SCC) for the Accreditation of Mineral Analysis Testing Laboratories and CAN -P-4E

ISO/IEC 17025. Samples were analyzed for gold via fire assay with an AA finish (“Au-AA23”) and

48 pathfinder elements via ICP-MS after four-acid digestion (“ME-MS61”). Samples that assayed

over 10 ppm Au were re-run via fire assay with a gravimetric finish (“Au-GRA21”).

In addition to ALS quality assurance / quality control (“QA/QC”) protocols, Goldshore has

implemented a quality control program for all samples collected through the drilling program. The

quality control program was designed by a qualified and independent third party, with a focus on

the quality of analytical results for gold. Analytical results are received, imported to our secure

on-line database and evaluated to meet our established guidelines to ensure that all sample

batches pass industry best practice for analytical quality control. Certified reference materials are

considered acceptable if values returned are within three standard deviations of the certified value

reported by the manufacture of the material. In addition to the certified reference material, certified

blank material is included in the sample stream to monitor contamination during sample

preparation. Blank material results are assessed based on the returned gold result being less

than ten times the quoted lower detection limit of the analytical method. The results of the on-

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going analytical quality control program are evaluated and reported to Goldshore by Orix

Geoscience Inc.

About Goldshore

Goldshore is an emerging junior gold development company, and owns the Moss Lake Gold

Project located in Ontario. Wesdome Gold Mines Ltd. is currently a strategic shareholder of

Goldshore with an approximate 22% equity position in the Company. Well-financed and

supported by an industry -leading management group, board of directors and advisory board,

Goldshore is positioned to advance the Moss Lake Gold Project through the next stages of

exploration and development.

About the Moss Lake Gold Project

The Moss Lake Gold Project is located approximately 100 km west of the city of Thunder Bay,

Ontario. It is accessed via Highway 11 which passes within 1 km of the property boundary to the

north. The Moss Lake Gold Project covers 14,292 hectares and consists of 282 unpatented and

patented mining claims.

Moss Lake hosts a number of gold and base metal rich deposits including the Moss Lake Deposit,

the East Coldstream Deposit (Table 4), the historically producing North Coldstream Mine (Table

5), and the Hamlin Zone, all of which occur over a mineralized trend exceeding 20 km in length.

A historical preliminary economic assessment was completed on Moss Lake in 2013 and

published by Moss Lake Gold1. A historical mineral resource estimate was completed on the East

Coldstream Deposit in 2011 by Foundation Resources Inc2,3. In addition to these zones, the Moss

Lake Gold Project also hosts a number of under-explored mineral occurrences which are reported

to exist both at surface and in historically drilled holes. The Moss Lake Deposit is a shear-hosted

disseminated-style gold deposit which outcrops at surface. It has been drilled over a 2.5 km length

and to depths of 300 m with 376 holes completed between 1983 and 2017. The last drilling

program conducted in 2016 and 2017 by Wesdome Gold Mines Ltd. (“ Wesdome”), which

consisted of widely spaced holes along the strike extension of the deposit was successful in

expanding the mineralized footprint and hydrothermal system 1.6 km to the northeast.

Additionally, the deposit remains largely open to depth. In 2017, Wesdome completed an induced

polarization survey which traced the potential extensions of pyrite mineralization associated with

the Moss Lake Deposit over a total strike length of 8 km and spanning the entire extent of the

survey grids.

The East Coldstream Deposit is a shear -hosted disseminated-style gold deposit which locally

outcrops at surface. It has been drilled over a 1.3 km length and to depths of 200 m with 138

holes completed between 1988 and 2017. The deposit remains largely open at depth and may

have the potential for expansion along strike. Historic drill hole highlights from the East

Coldstream Deposit include 4.86 g/t Au over 27.3 m in C-10-15.

The historically producing North Coldstream Mine is reported to have produced significant

amounts of copper, gold and silver 4 from mineralization with potential iron- oxide-copper-gold