Gold, Silver PM's Rich Mines, Utah

[NYBob]

Unico, Inc. Announces Initial Geological Work Conducted at -
Clyde and Crown Point Mines -
Unico, Incorporated -
(OTCBB: UCOI), a natural resource company in the precious metals mining sector, today announced that initial geological work has been conducted in the areas of
the Clyde and Crown Point mining -
claims by Dean Misantoni, senior geologist for
Deer Trail Mining Company -
a wholly owned subsidiary of
Unico, Incorporated.

The Clyde and Crown Point -
claims were subjects of a lease agreement with
Deer Trail Mining Company, Inc. -
that was announced in July 2006.

The report submitted by Mr. Misantoni states:

"Since August, 2007,
initial geologic work has been conducted on the Clyde and Crown Point Mine areas.
This includes the review of very limited previous geochemical data and maps of the area, aerial photographic examination, surface reconnaissance mapping and sampling, and
Brunton and tape mapping/sampling of -
accessible underground workings.

As of this date, some 20 samples have been collected and
analyzed by ALS Chemex in Vancouver, British Columbia.
The initial focus has been on understanding the nature of
the deposit(s), establishing -
the widths of mineralized structures, establishing -
the geochemical signature of the mineralization -
as an aid in guiding further exploration at depth,
and its relationship to the mining district as a whole.

A mineralized, generally fine-grained hornblende-biotite
porphyry of unknown dimensions is exposed on the surface
and in underground workings on the property.
It crops out over at least 500 feet in an east-west direction
in the vicinity of the of
the Clyde adits,
and extends downhill to the south to near Cottonwood Creek Road.
It was not noted in or near -
the Crown Point Mine.
Faulted and mineralized intrusive contacts are exposed,
either within steeply dipping clastic rocks, possibly shales
of the Triassic Chinle Formation, on the west, or
quartzites of the Jurassic Navajo sandstone on the east.

The property lies along several large, regional faults,
and the Mesozoic sedimentary rocks are jumbled and rotated
to near vertical, probably due to fault rotation, and
possibly in part due to the intrusion.
The form of the intrusive body appears to be that of a
small plug or stock, as opposed to a dike, at the
present level of exposure. Hydrothermal alteration varies
from moderate propylitization (chlorite, magnetite, calcite)
to intense phyllic alteration (clay/sericite)
with disseminated pyrite and Fe-oxides.
Rocks devoid of alteration are not exposed.

Mineralization consists of veins and mineralized
breccias within the intrusion, and extends into
the country rocks, which are sometimes altered
to hornfels or fine-grained, green calc-silicate
assemblages.

The strongest zones of mineralization seem to occur
along the northwest flank of the intrusion, at
the brecciated contact of the intrusion with the
enclosing sedimentary rocks, at the junction of at
least two faults.

Minerals consist of fine-grained
pyrite-chalcopyrite-galena-sphalerite-tetrahedrite-tennantite
in white to clear quartz veins and breccias.
Other phases (enargite-covellite-chalcocite) have
been tentatively identified.
The mineralization appears to be unoxidized except
for extensive, post-mine copper sulfate staining of
fractures in the upper Clyde adit winze.

Although much work remains to be done,
the Clyde prospect -
is definitely anomalous in a suite of elements,
including gold (Au),
silver (Ag),
copper (Cu),
lead (Pb),
zinc (Zn),
molybdenum (Mo),
bismuth (Bi),
barium (Ba,)
and fluorine (F),
consistent with the model for the mining district
as a whole, and with a subvolcanic
porphyry-type environment.

The petrology of the intrusive, structural setting,
and hydrothermal alteration types also fit the model
quite well.

The presence of a buried intrusive stock and
porphyry system beneath Alunite Ridge has long
been hypothesized, and the Clyde prospect
(to the south and topographically beneath Alunite Ridge)
may represent one instance where the top of such
an intrusive system is exposed at the surface.

Road access and drilling platforms are present,
and are much more logistically sound than historic
proposals to drill from platforms high on the mountains
to the north."

Mark Lopez, chief executive officer of Unico, Inc., stated,
"As we prepare to initiate processing operations at
the mill and processing facility at the Deer Trail Mine,
we will concurrently work to explore and develop
additional sources beneficial to the facility.

These sources are expected to include underground mining
activities associated with the Deer Trail Mine,
as well as other potential targets from the additional
claims in the area, which include
the Clyde and Crown Point mines.

"We are quite pleased to have received this initial report
from Mr. Misantoni and look to continue the geological
analysis of these claims as we move forward with
our exploration efforts," Mr. Lopez added.

In August 2007, Unico announced that it had completed
the purchase of
the Deer Trail Mine -
for its Deer Trail Mining Company subsidiary.

Shareholders who would like to sign up to receive information by email directly from Unico, Inc. are asked to visit the company's website at
http://www.unicomining.com/IR/mailinglist.php
and fill in the appropriate fields.

About Unico, Inc.

Unico, Inc. (OTCBB: UCOI) is a publicly traded natural resource company in the precious metals mining sector that is focused on the exploration, development and production of gold, silver, lead, zinc, and copper concentrates at its three mine properties: the Deer Trail Mine, the Bromide Basin Mine and the Silver Bell Mine. The company has also announced agreements to acquire over 70 additional mining claims. In August 2007, Unico announced that its wholly owned Deer Trail Mining Company subsidiary had completed the purchase of the Deer Trail Mine from Crown Mines, LLC. For more information, please visit www.unicomining.com.

Forward-Looking Statements

This news release may contain forward-looking statements within the meaning of Section 27A of the Securities Act of 1933, as amended and such Section 21E of the Securities Exchange Act of 1934, as amended. Such statements are subject to risks and uncertainties that could cause actual results to vary materially from those projected in the forward-looking statements. The company may experience significant fluctuations in operating results due to a number of economic, competitive and other factors. These factors could cause operation results to vary significantly from those in prior periods, and those projected in forward-looking statements. Information with respect to these factors, which could materially affect the company and its operations, are included on certain forms the company files with the Securities and Exchange Commission.

Contacts:
Gemini Financial Communications, Inc.
A. Beyer
951-677-8073
Email Contact

OTC Financial Network
Rick McCaffrey
781-444-6100, x625
Email Contact
www.otcfn.com/ucoi

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