Wolf Wiese CEO of Golden Dawn Minerals Inc., (TSX-V:GOM)
(Frankfurt:3G8A) (OTC:GDMRF) (the “
Company” or
“Golden Dawn”) announces final results from 2017
surface diamond drilling at its Golden Crown property, part of the
Greenwood Precious Metals Project.
Surface diamond drilling at the Golden Crown
property in 2017 totaled 3,121 metres drilled in 33 holes. Results
for holes 1 to 19 were previously released (see news release dated
December 4, 2017). Significant results for holes 20 to 33 are
presented in the table below, followed by results for the first 19
holes in a separate table.
Table of Significant Results for 2017
Golden Crown Drill Holes 20 to 33
Hole |
From (m) |
To (m) |
Length (m) |
Sampled Length |
Gold (g/t) |
Copper (%) |
Silver (g/t) |
Comment |
GC17-22 |
60.88 |
62.62 |
1.74 |
1.74 |
11.11 |
0.23 |
7.0 |
average |
including |
60.88 |
61.18 |
0.30 |
0.30 |
13.40 |
0.58 |
8.3 |
sulphide veinlets |
61.18 |
61.88 |
0.70 |
0.70 |
0.28 |
0.11 |
2.0 |
sulphide veinlets |
61.88 |
62.31 |
0.43 |
0.43 |
0.93 |
0.21 |
6.5 |
sulphide veinlets |
62.31 |
62.62 |
0.31 |
0.31 |
47.50 |
0.16 |
17.6 |
sulphide veinlets |
GC17-22 |
70.65 |
72.00 |
1.35 |
1.35 |
4.50 |
0.12 |
N/S |
average |
|
70.65 |
70.94 |
0.29 |
0.29 |
15.60 |
0.35 |
4.2 |
qtz sulphide vein |
including |
70.94 |
71.25 |
0.31 |
0.31 |
0.42 |
0.07 |
0.2 |
sulphide veinlets |
|
71.25 |
71.70 |
0.45 |
0.45 |
0.07 |
0.02 |
NS |
sulphide veinlets |
|
71.70 |
72.00 |
0.30 |
0.30 |
4.64 |
0.10 |
1.1 |
qtz sulphide vein |
GC17-23 |
79.67 |
80.00 |
0.33 |
0.33 |
10.80 |
0.93 |
16.0 |
sulphide veinlets |
GC17-24 |
102.40 |
103.20 |
0.62 |
0.62 |
16.50 |
1.33 |
12.95 |
average |
including |
102.40 |
102.76 |
0.36 |
0.36 |
26.40 |
2.19 |
20.5 |
massive sulphide (South Zone) |
102.76 |
103.20 |
0.26 |
0.26 |
2.79 |
0.14 |
2.5 |
sulphide veinlets |
GC17-25 |
65.72 |
66.14 |
0.42 |
0.42 |
17.80 |
0.90 |
12.0 |
massive sulphide (South Zone) |
76.37 |
76.77 |
0.40 |
0.40 |
1.98 |
0.08 |
1.2 |
fault with qtz sulphide vein |
83.25 |
83.60 |
0.35 |
0.35 |
6.58 |
0.04 |
0.1 |
fault gouge |
Table of Significant Results for 2017 Golden Crown Drill
Holes 20 to 33 (Cont’d).
GC17-26 |
93.67 |
94.67 |
1.00 |
1.00 |
14.2 |
0.5385 |
11.3 |
average |
including |
93.67 |
94.17 |
0.50 |
0.50 |
17.00 |
0.49 |
9.9 |
massive sulphide (South Zone) |
94.17 |
94.67 |
0.50 |
0.50 |
11.40 |
0.58 |
12.7 |
massive sulphide (South Zone) |
GC17-27 |
80.77 |
81.63 |
0.86 |
0.86 |
2.04 |
0.04 |
0.6 |
Disseminated sulphides |
GC17-28 |
118.71 |
119.06 |
0.35 |
0.35 |
1.26 |
0.04 |
0.7 |
sulphide veinlets |
GC17-28 |
126.24 |
126.63 |
0.39 |
0.39 |
4.74 |
0.59 |
7.3 |
qtz sulphide veinlets |
130.90 |
131.70 |
0.80 |
0.80 |
10.30 |
0.62 |
11.3 |
massive sulphide (South Zone) |
135.14 |
135.47 |
0.33 |
0.33 |
4.14 |
0.54 |
8.6 |
massive sulphide (South Zone) |
142.68 |
143.06 |
0.38 |
0.38 |
1.06 |
0.04 |
1.0 |
sulphide veinlets |
153.99 |
154.36 |
0.37 |
0.37 |
3.86 |
0.33 |
4.0 |
massive sulphide (South Zone) |
GC17-29 |
77.91 |
78.21 |
0.30 |
0.30 |
14.80 |
1.43 |
15.40 |
massive sulphide (South Zone) |
80.04 |
80.35 |
0.31 |
0.31 |
1.43 |
0.05 |
0.6 |
pyrite on fractures |
83.60 |
84.00 |
0.40 |
0.40 |
4.33 |
0.16 |
1.0 |
massive sulphide (South Zone) |
93.83 |
94.14 |
0.31 |
0.31 |
3.12 |
0.08 |
1.0 |
sulphide veinlets |
GC17-30 |
58.15 |
59.81 |
1.66 |
1.66 |
15.20 |
1.37 |
20.1 |
average |
including |
58.15 |
58.63 |
0.48 |
0.48 |
24.20 |
1.83 |
30.9 |
massive sulphide (South Zone) |
58.63 |
59.12 |
0.49 |
0.49 |
16.50 |
1.90 |
22.0 |
59.12 |
59.51 |
0.39 |
0.39 |
4.66 |
0.23 |
3.6 |
59.51 |
59.81 |
0.30 |
0.30 |
12.40 |
1.23 |
21.0 |
qtz sulphide veinlets |
G17-30 |
62.30 |
63.08 |
2.28 |
2.28 |
3.18 |
0.11 |
1.2 |
average |
including |
62.30 |
63.08 |
0.78 |
0.78 |
5.02 |
0.21 |
2.1 |
sulphide veinlets |
63.08 |
63.58 |
0.50 |
0.50 |
4.17 |
0.12 |
1.2 |
sulphide veinlets |
63.58 |
64.58 |
1.00 |
1.00 |
1.24 |
0.04 |
0.4 |
sulphide veinlets |
G17-30 |
70.42 |
71.54 |
1.12 |
1.12 |
1.26 |
0.06 |
0.4 |
sulphide veinlets |
GC17-31 |
6.83 |
7.73 |
0.90 |
0.90 |
2.92 |
0.18 |
3.0 |
sulphide veinlets |
12.66 |
13.1 |
0.44 |
0.11 |
3.68 |
0.60 |
12.5 |
sulphide veinlets |
16.39 |
17.23 |
0.84 |
0.84 |
1.01 |
0.02 |
3.0 |
sulphide veinlets |
60.43 |
60.75 |
0.32 |
0.32 |
1.62 |
1.80 |
26.7 |
massive sulphide (Samaritan Zone) |
107.22 |
107.84 |
0.62 |
0.62 |
1.15 |
0.03 |
NS |
disseminated sulphides |
149.63 |
149.95 |
0.32 |
0.32 |
2.45 |
0.16 |
1.3 |
massive sulphide (King Zone) |
GC17-31 |
158.33 |
160.30 |
1.97 |
1.97 |
1.62 |
0.24 |
4.28 |
average |
|
158.33 |
159.38 |
1.05 |
1.05 |
1.14 |
0.08 |
1.1 |
sulphide veinlets |
including |
159.38 |
159.8 |
0.42 |
0.42 |
1.80 |
0.36 |
4.6 |
sulphide veinlets |
|
159.8 |
160.3 |
0.50 |
0.5 |
2.46 |
0.50 |
10.7 |
qtz sulphide vein |
GC17-32 |
72.07 |
72.57 |
0.50 |
0.5 |
1.71 |
0.04 |
0.7 |
sulphide veinlets |
87.93 |
88.23 |
0.30 |
0.30 |
1.97 |
0.07 |
1.9 |
sulphide veinlets |
GC17-33 |
7.33 |
7.67 |
0.34 |
0.34 |
1.72 |
0.13 |
3.6 |
sulphide veinlets |
15.69 |
15.98 |
0.29 |
0.29 |
1.83 |
0.92 |
22.4 |
qtz sulphide vein |
75.45 |
75.76 |
0.31 |
0.31 |
1.02 |
0.126 |
2.3 |
sulphide veinlets |
113.63 |
113.94 |
0.31 |
0.31 |
15.7 |
0.699 |
10.2 |
disseminated and veinlet sulphides |
NS = not significant; g/t = grams per tonne; qtz
= quartzThe widths of zones reported above for the drill holes are
core lengths, which may be different from true width. There is
insufficient information at this time to accurately estimate the
true width of the zones.
Table of Significant Results for Golden
Crown Drill Holes 1 to 19.
Hole |
From (m) |
To (m) |
Length (m) |
Sampled Length |
Gold (g/t) |
Copper (%) |
Silver (g/t) |
Comment |
GC17-02 |
9.24 |
21.58 |
12.30 |
6.91 |
3.53 |
0.11 |
N/S |
average (King) |
including |
9.24 |
9.79 |
0.55 |
0.55 |
1.61 |
NS |
NS |
sulphide veinlets |
9.79 |
14.02 |
4.23 |
0.89 |
1.08 |
0.13 |
NS |
sulphide veinlets |
14.02 |
14.83 |
0.81 |
0.81 |
3.58 |
0.19 |
NS |
Massive sulphide (King) |
14.83 |
17.00 |
2.17 |
0.59 |
NS |
NS |
NS |
sulphide veinlets |
17.00 |
17.57 |
0.57 |
0.57 |
7.57 |
0.08 |
NS |
massive sulphide (King) |
17.57 |
18.18 |
0.61 |
0.61 |
4.03 |
0.15 |
NS |
massive sulphide (King) |
18.18 |
18.84 |
0.66 |
0.66 |
14.10 |
0.18 |
NS |
massive sulphide (King) |
18.84 |
19.74 |
0.9 |
0.52 |
2.52 |
0.11 |
NS |
massive sulphide (King)57% recovery |
19.74 |
20.6 |
0.86 |
0.86 |
17.30 |
0.27 |
NS |
massive sulphide (King) |
20.6 |
21.58 |
0.98 |
0.85 |
1.91 |
NS |
NS |
sulphide veinlets |
GC17-04 |
24.2 |
25.1 |
0.9 |
0.9 |
1.05 |
NS |
NS |
sulphide veinlets |
41.47 |
42.47 |
1.0 |
1.0 |
1.04 |
NS |
NS |
sulphide veinlets |
69.54 |
69.95 |
0.41 |
0.41 |
11.20 |
0.12 |
NS |
massive sulphide (King) |
GC17-05 |
14.65 |
21.60 |
6.95 |
6.95 |
6.77 |
1.18 |
|
average (King) |
including |
14.65 |
14.96 |
0.31 |
0.31 |
1.36 |
3.19 |
37.4 |
massive sulphide (King) |
14.96 |
15.95 |
0.99 |
0.99 |
NS |
NS |
NS |
sulphide veinlets |
15.95 |
16.92 |
0.97 |
0.97 |
0.51 |
0.60 |
9.0 |
sulphide veinlets |
16.92 |
18.13 |
1.21 |
1.21 |
0.14 |
0.71 |
10.3 |
sulphide veinlets |
18.13 |
18.44 |
0.31 |
0.31 |
16.90 |
4.15 |
72.7 |
massive sulphide (King) |
18.44 |
18.84 |
0.40 |
0.40 |
58.30 |
3.18 |
75.6 |
massive sulphide (King) |
18.84 |
19.24 |
0.40 |
0.40 |
24.50 |
3.92 |
67.5 |
massive sulphide (King) |
19.24 |
20.56 |
1.32 |
1.32 |
0.81 |
0.19 |
3.0 |
sulphide veinlets |
20.56 |
20.82 |
0.26 |
0.26 |
18.80 |
3.47 |
59.9 |
sulphide veinlets |
20.82 |
21.28 |
0.46 |
0.46 |
2.72 |
0.57 |
9.7 |
sulphide veinlets |
21.28 |
21.60 |
0.32 |
0.32 |
1.01 |
0.64 |
13.5 |
sulphide veinlets |
Hole |
From (m) |
To (m) |
Length (m) |
Sampled Length |
Gold (g/t) |
Copper (%) |
Silver (g/t) |
Comment |
GC17-08 |
47.98 |
48.36 |
0.38 |
0.38 |
2.01 |
0.12 |
NS |
sulphide veinlets |
79.96 |
80.52 |
0.56 |
0.56 |
12.60 |
0.26 |
2.9 |
massive sulphide (Winnipeg) |
80.52 |
81.22 |
0.7 |
0.7 |
7.55 |
0.23 |
2.4 |
massive sulphide (Winnipeg) |
109.15 |
109.45 |
0.3 |
0.3 |
2.71 |
NS |
NS |
sulphide veinlets |
GC17-09 |
41.91 |
42.21 |
0.3 |
0.3 |
4.01 |
NS |
NS |
sulphide veinlets |
GC17-10 |
69.56 |
79.06 |
0.5 |
0.5 |
3.26 |
0.35 |
5.4 |
massive sulphide (King) |
GC17-11 |
30.38 |
31.18 |
0.80 |
0.80 |
1.98 |
3.72 |
92.8 |
massive sulphide(King) |
46.90 |
47.65 |
0.75 |
0.75 |
1.67 |
0.11 |
NS |
sulphide veinlets |
GC17-12 |
56.42 |
56.70 |
0.28 |
0.28 |
6.75 |
NS |
NS |
massive sulphide (King) |
60.20 |
60.70 |
0.50 |
0.50 |
2.45 |
0.09 |
NS |
sulphide veinlets |
64.38 |
65.88 |
1.50 |
1.50 |
4.99 |
0.12 |
NS |
qtz-sulfide veins in serpentinite |
72.68 |
73.38 |
0.70 |
0.70 |
1.74 |
NS |
NS |
sulphide veinlets |
GC17-13 |
41.0 |
42.13 |
1.13 |
1.13 |
2.51 |
0.15 |
NS |
massive sulfide (King) |
GC17-14 |
33.88 |
34.45 |
0.57 |
0.57 |
27.20 |
0.11 |
NS |
qtz-sulphide vein(Portal) |
37.17 |
38.47 |
1.30 |
1.30 |
4.29 |
0.07 |
NS |
qtz-sulphide vein(Portal) |
GC17-15 |
22.32 |
22.80 |
0.48 |
0.48 |
2.34 |
0.10 |
NS |
qtz-sulphide vein(Portal) |
38.66 |
38.91 |
0.25 |
0.25 |
3.76 |
NS |
NS |
qtz-sulphide vein(Portal) |
41.00 |
41.50 |
0.50 |
0.50 |
1.30 |
NS |
NS |
greenstone |
43.73 |
44.04 |
0.31 |
0.31 |
3.04 |
0.13 |
NS |
qtz-sulphide vein(Portal) |
49.86 |
50.13 |
0.27 |
0.27 |
1.16 |
NS |
NS |
massive sulfide (Portal) |
GC17-16 |
27.00 |
27.73 |
0.73 |
0.73 |
7.21 |
0.24 |
NS |
qtz-sulphide vein (Portal) |
39.53 |
39.90 |
0.37 |
0.37 |
7.20 |
NS |
NS |
qtz-sulphide vein (Portal) |
45.00 |
45.33 |
0.33 |
0.33 |
1.13 |
NS |
NS |
sulphide veinlets |
49.50 |
51.50 |
2.00 |
2.00 |
5.11 |
NS |
NS |
qtz-sulphide vein & diorite (Portal) |
GC17-18 |
31.25 |
31.55 |
0.30 |
0.30 |
41.40 |
0.17 |
5.9 |
qtz-sulphide vein (SW Zone) |
GC17-19 |
58.47 |
59.00 |
0.53 |
0.30 |
4.09 |
0.81 |
6.5 |
qtz-sulphide vein (SW Zone) |
Table of Significant Results for Golden
Crown Drill Holes 1 to 19 (cont’d).
NS = not significant; g/t = grams per tonne; qtz
= quartzThe widths of zones reported above for the drill holes are
core lengths, which may be different from true width. There is
insufficient information at this time to accurately estimate the
true width of the zones.
The 2017 drill holes reported above were
designed to test the King, Winnipeg, Portal, Southwest and South
zones. The drill program intersected zones of significant gold and
copper associated with massive sulphide and quartz-sulphide veins
and veinlets. Typical sulphide minerals include pyrrhotite, pyrite,
chalcopyrite, and arsenopyrite in general order of abundance.
Interesting gold values are also associated with veinlet-controlled
and disseminated sulphides in the host rocks (meta-diorite,
greenstone and serpentinite).
At least in part, the deposit now appears to
consist of a field of multiple veins and veinlets, with the main
vein structures identified as targets for underground development.
Potential for open pit extraction exists where significant gold
values occur in wall rocks adjacent to the main veins and near
surface.
The 2017 drilling results intersected grades and
widths similar to those previously reported for the Golden Crown
deposit, encountered additional mineralization marginal to the
known zones, and defined extensions to some of the zones
tested.
The Main Zone (King Vein and parallel lodes) was
verified by intercepts in drill holes GC17-02, 04, 05, 10, 12 and
13. Drill holes GC17-11 and-31 hit the structure beyond the
previously defined limits, with hole 31 possibly extending the
MacArthur structure 68 metres to the east.
The Winnipeg zone was intersected in drill hole
GC17-09 and the Portal Zone was intersected in holes GC17-14, 15
and 16.
The MacArthur zone was intersected in holes
GC17-31 and GC17-33 indicating the zone extends a further 28 metres
down dip than previously defined. The Samaritan Zone was also
intersected in these holes, possibly defining the Samaritan Zone an
additional 46 metres further west and may extend up to 95 metres to
where sulphide mineralization was encountered in hole GC17-32.
The Southwest zone was intersected in drill
holes GC17-18 and 19, which encountered mineralization up to 54
metres below a 2004 surface trench on the structure.
The South Zone was confirmed by hole GC17-22
that intersected gold mineralization similar to that recorded in
historic 1986 drilling. Holes GC17-23 to -26 indicate this zone
extends 100 metres further down dip, and in GC17-28 the zone was
defined 28 metres down dip and 17 metres east of a 1986 drill hole
intercept.
Further surface exploration drilling is
scheduled to commence in the next few weeks, aimed at increasing
the resource inventory, upgrading Inferred resources to Indicated
category, and for new discoveries. Initial work will explore the
western extension of the King zone, eastern extension of the
MacArthur zone, infill and extend the Samaritan zone to the east,
and explore east and west extensions of the Portal zone. The drill
program will then progress to the JD Zone and the area between the
Golden Crown mine property and JD, within a 3 km trend of anomalous
soil geochemistry and surface mineral showings. The historic JD
Zone is located 3 km west of the Golden Crown Mine and hosts quartz
and sulphide veins similar to those intersected in the 2017
drilling. As reported in the news release dated October 18, 2017,
gold values for individual 1 metre wide surface rock chip samples
from the JD area range between 1.8 and 15.8 g/t gold, with
an overall average of 7.4 g/t gold. The table below shows
weighted average results for consecutive samples (sample traverses)
from the JD area in 2017.
Table of averaged results for
consecutive surface rock chip samples at JD area
(2017)
Sample Traverse |
Sampled Length (m) |
Gold (g/t) |
Copper (%) |
Silver (g/t) |
1 |
2.0 |
10.70 |
0.01 |
3.0 |
2 |
2.0 |
2.36 |
0.01 |
0.5 |
3 |
2.0 |
8.31 |
0.03 |
3.7 |
4 |
1.5 |
10.64 |
0.01 |
6.1 |
5 |
4.0 |
5.87 |
0.16 |
28.8 |
The Golden Crown property lies 3 km from the
Greenwood Processing Plant and is planned to be mined and processed
at the plant after the Lexington mine is brought online. The
Company is continuing with permitting an underground mine and bulk
sampling in 2018, leading to full production from the Golden Crown
Mine.
In addition, surface rock chip sampling was
conducted in late fall of 2017 at the Lexington property. The
surface outcrop of the historic City of Paris mine consists of a
quartz-sericite altered zone containing disseminated pyrite. A chip
sample across this zone returned significant grade and width
(14.50 grams per tonne gold over 4.5 metres true
width). This result warrants further investigation to
determine the extent of mineralization remaining in this historic
mine.
DISCUSSION:
The numerous mineralized zones on the Greenwood
Precious Metals Project (15,400 hectares), as evidenced by the 34
historic mines including the large scale historic Phoenix
copper-gold mine and our present exploration results, all point to
the necessity to view this mining district holistically. It is
believed that the many precious and base metal deposits on this
property were triggered by several geological events, which formed
a plethora of mineralization styles, thus requiring our
geoscientists to remain open to all possibilities. The exploration
effort is utilizing state-of-the-art technology and is being
conducted from a bird’s eye perspective as well as a localized
focused view to locate potential sources of the mineralization on
the Greenwood Precious Metals Project. Importantly, the Greenwood
Mining Camp is situated within an area of tectonic extension as
evidenced by the Republic Toroda Grabens, which extend from south
of the 49th parallel in the USA where they are associated with gold
deposits in the prolific Republic Mining District. Past
exploration efforts in the area of Greenwood Precious Metals
Project were severely limited due to the fragmented claim holding
situation. Due to our Company’s success in consolidating this
prolific mining camp and the presence of a modern processing plant,
the Company has the opportunity to produce precious and base metals
in the immediate term. Our work over this year will continue
towards production at the Lexington and Golden Crown properties,
and at the same time conduct an all-inclusive geological assessment
of the district aimed at discovering additional resources to
prolong the life of the operation.
The Company is rapidly progressing towards the
start-up of mining operations at the Lexington mine, located 17 km
south of the Greenwood Processing Plant, with de-watering now
complete and mine planning and geotechnical assessments being
conducted prior to initial mining. The Greenwood Processing Plant
will be wet commissioned once the mining operation is underway. The
Company is also awaiting assay results to quantify the test work
completed in December utilizing new state-of-the-art product/waste
separation sensor sorting technology provided by Steinert US
Inc.
All of the samples reported above were collected
under the supervision of Dr. Mathew Ball, P.Geo. and delivered to
Activation Laboratories (Act-Labs) in Kamloops, B.C. Activation
Laboratories (Act-Labs) is an independent commercial laboratory
that is ISO 9001 certified and ISO 17025 accredited. Analyses for
gold were by the fire assay method using 30 gram samples with an AA
finish. Fire assay gravimetric analyses were carried out on initial
gold analytical results in excess of 30000 ppb gold. Silver and
other elements were analyzed by ICP-OES using an aqua regia
digestion. Copper results above 1% were re-analyzed by peroxide
fusion. Results above 100 g/t silver were re-analyzed in duplicate
for ore grade concentrations by the Fire Assay gravimetric method
using a 30 gram sample. Quality control was monitored using
reference and blank samples inserted into the sample sequence at
intervals. Check analyses are being performed on selected
samples.
The Company would like to clarify that its
decision to proceed to extract mineralized material from the Golden
Crown and Lexington deposits for processing at its facility located
at the Greenwood Precious Metals Project is not based on a
feasibility study. The Company cautions that, in such cases, there
is increased uncertainty and higher economic and technical risks of
failure.
Technical disclosure in this news release has
been approved by Dr. Mathew Ball, P.Geo., a Qualified Person as
defined by National Instrument 43-101, and Chief Operating Officer
of the Company.
For more details, please see the most recent
National Instrument 43-101 Technical Report on the Company's
website at www.goldendawnminerals.com.
On behalf of the Board of
Directors:GOLDEN DAWN MINERALS INC.
Wolf Wiese, President & Chief Executive
Officer
For further information, please
contact:Corporate Communications604-221-8936
allinfo@goldendawnminerals.com
THIS PRESS RELEASE WAS PREPARED BY MANAGEMENT, WHO TAKE FULL
RESPONSIBILITY FOR ITS CONTENTS. NEITHER THE TSX VENTURE EXCHANGE
NOR ITS REGULATION SERVICES PROVIDER (AS THAT TERM IS DEFINED IN
THE POLICIES OF THE TSX VENTURE EXCHANGE) ACCEPTS RESPONSIBILITY
FOR THE ADEQUACY OR ACCURACY OF THIS RELEASE. THIS DOCUMENT
CONTAINS CERTAIN FORWARD LOOKING STATEMENTS WHICH INVOLVE KNOWN AND
UNKNOWN RISKS, DELAYS, AND UNCERTAINTIES NOT UNDER THE COMPANY’S
CONTROL WHICH MAY CAUSE ACTUAL RESULTS, PERFORMANCE OR ACHIEVEMENTS
OF THE COMPANY TO BE MATERIALLY DIFFERENT FROM THE RESULTS,
PERFORMANCE, OR ACHIEVEMENTS IMPLIED BY THESE FORWARD LOOKING
STATEMENTS. WE SEEK SAFE HARBOR.
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