UNITED STATES
                       SECURITIES AND EXCHANGE COMMISSION
                             WASHINGTON, D.C. 20549

                             ----------------------

                                    FORM 8-K

                             ----------------------

                                 CURRENT REPORT
                     PURSUANT TO SECTION 13 OR 15(D) OF THE
                         SECURITIES EXCHANGE ACT OF 1934


          August 30, 2005                                333-101960
           Date of Report                            Commission File Number
  (Date of earliest event reported)

                          YUKON GOLD CORPORATION, INC.
             (Exact name of registrant as specified in its charter)

          Delaware                                       98-0413063
  (State or other jurisdiction of        (I.R.S. Employer Identification Number)
   incorporation or organization)

                                 347 Bay Street
                                    Suite 408
                            Toronto, Ontario M5H 2R7
               (Address of Principal Executive Offices) (Zip Code)

                                 (416) 865-9930
              (Registrant's telephone number, including area code)

--------------------------------------------------------------------------------


<PAGE>

Item 8.01 Other Events

On July 7, 2002, Yukon Gold Corp., our wholly owned subsidiary ("YGC"),  entered
into an option  agreement with the Hinton Syndicate to acquire a 75% interest in
the 273 unpatented  mineral claims  covering  approximately  14,000 acres in the
Mayo Mining District of the Yukon Territory, Canada. This agreement was replaced
with a revised and amended  agreement  dated as of July 7, 2005 among Yukon Gold
Corporation, Inc., YGC and the Hinton Syndicate and is referred to herein as the
"Hinton Option  Agreement." The Hinton Option Agreement  superseded the original
agreement and amendments thereto.

YGC must make  scheduled cash payments and perform  certain work  commitments to
earn up to a 75%  interest  in the mineral  claims,  subject to a 2% net smelter
return royalty in favor of the Hinton Syndicate, as further described below.

The schedule of Property Payments and Work Programs are as follows:

      PROPERTY PAYMENTS

      a. On execution of the July 7, 2002 Agreement     $   25,000 Paid
      b. On July 7, 2003                                $   75,000 Paid
      c. On July 7, 2004                                $  150,000 Paid
      d. On January 2, 2006                             $  150,000
      e. On July 7, 2006                                $  150,000
      f. On July 7, 2007                                $  150,000
      g. On July 7, 2008                                $  150,000
                                                  TOTAL $  850,000

      WORK PROGRAM-expenditures to be incurred in the following periods;

      a. July 7/02 to July 6/03                         $  150,000 Incurred
      b. July 7/03 to July 6/04                         $  250,000 Incurred
      c. July 7/04 to July 6/05                         $  325,000 Incurred
      d. July 7/05 to Dec.31/06                         $  750,000
      e. Jan. 1/07 to Dec 31/07                         $1,000,000
      f. Jan. 1/08 to Dec 31/08                         $1,250,000
      g. Jan  1/09 to Dec 31/09                         $1,500,000
                                                  TOTAL $5,225,000

All Property Payments and Work Programs due to date of this report have been
made and incurred. Work Program expenditures have exceeded those required by
approximately $75,000.

Provided all Property Payments have been made that are due prior to the Work
Program expenditure levels being attained, Yukon Gold shall have earned a:

      25% interest upon Work Program expenditures of $1,500,000

      50% interest upon Work Program expenditures of $2,500,000

      75% interest upon Work Program expenditures of $5,225,000

In some cases,  payments made to service  providers  include amounts advanced to
cover the cost of future work.  These  advances are not loans but are considered
"incurred"  exploration expenses under the terms of the Hinton Option Agreement.
Section 2.2(b) of the Hinton Option  Agreement  defines the term,  "incurred" as
follows:   "Costs  shall  be  deemed  to  have  been  "incurred"  when  YGC  has
contractually  obligated  itself to pay for such  costs or such  costs have been
paid, whichever should first occur." Consequently, the term, "incurred" includes
amounts  actually paid and amounts that YGC has obligated  itself to pay.  Under
the Hinton Option  Agreement there is also a provision that requires YGC to have
raised and have  available  the Work  Program  funds for the period from July 7,
2005 to December 31, 2006, by May 15 of 2006.


                                       2
<PAGE>

The  Hinton  Option  Agreement  contemplates  that upon the  earlier  of:  (i) a
production  decision or (ii) investment of CDN$5.225  million or (iii) YGC has a
minority interest and decides not to spend any more money on the project,  YGC's
relationship  with the Hinton  Syndicate  will  become a joint  venture  for the
further  development  of the property.  Under the terms of the Hinton  Syndicate
Agreement, the party with the majority interest would control the joint venture.
Once the 75% interest is earned, as described above, YGC has a further option to
acquire the remaining 25% interest in the mineral  claims for a further  payment
of CDN$5,000,000.

The Hinton Option Agreement provides that the Hinton Syndicate receive a 2% "net
smelter  returns  royalty."  In the event that we exercise our option to buy-out
the remaining 25% interest of the Hinton Syndicate (which is only possible if we
have reached a 75% interest,  as described  above) then the "net smelter  return
royalty"  would  become 3% and the Hinton  Syndicate  would  retain this royalty
interest  only.  The "net smelter  return  royalty" is a percentage of the gross
revenue  received  from the sale of the ore produced  from our mine less certain
permitted expenses.

The Hinton  Option  Agreement  entitles the Hinton  Syndicate  to recommend  for
appointment one member to the board of directors of the Yukon Gold.

The Hinton Syndicate Agreements provides both parties (YGC and Hinton Syndicate)
with rights of first  refusal in the event that either party  desires to sell or
transfer its interest.

The Hinton Syndicate members, each has the option to receive their share of
property payments in stock of Yukon Gold at a 10% discount to the market and
once Yukon Gold has obtained a listing on a Canadian stock exchange YGC and
Yukon Gold have a further option to pay 40% of any property payment due after
the payment on January 2, 2006 with common stock of Yukon Gold.

The Mount Hinton  Property is located  approximately  6 miles  southeast of Keno
City and 150 north of Whitehorse in the Yukon Territory Canada.

The Hinton Property is located within the Tombstone Gold Belt immediately to the
east of the Keno-Elsa  Silver Camp.  Recognized  as one of the more  prospective
gold  regions in the world,  the  Tombstone  Gold Belt is  comprised  of several
mineral rich  districts  that extend more than 1000 km across the North American
Cordillera  (Alaska and Yukon).  Though  mineralization  types vary they are all
related to a distinctive  northwest trending belt of plutonic  intrusions termed
the Tombstone Suite.

The Mt. Hinton gold veins and silver deposits of the Keno Hill Silver Camp occur
within the Keno Hill Quartzite  where brittle failure has created major fracture
zones for mineral deposition.  The brittle quartzite represents a tectonic sheet
or bed separated by two major faults  called the  Tombstone  and Robert  Service
thrusts.  The Keno Hill Quartzite is 600 metres thick in the silver zones and as
much as 2000 metres thick on the Mt. Hinton property

Economic  silver  deposits  in the  Keno  Hill  are best  developed  within  the
relatively  brittle Keno Hill Quartzite.  Within  productive areas the ore zones
occur  throughout the full  quartzite bed from hanging wall to footwall.  Strike
lengths of individual ore shoots range from 30 to 335 metres,  with  thicknesses
ranging  from 0.3 to 30 metres.  The  Hinton  gold  zones  mirror  the  physical
characteristics  of the Keno  Hill  silver  zones  although  they are much  more
enriched in gold.

Over 50  mineralized  gold  veins,  vein  segments  and float  trains  have been
identified  on the Mount  Hinton  Property.  These veins form a broad vein fault
system,  (Mt. Hinton Gold Trend),  300 metres wide and 3000 metres long. To date
gold  mineralization  has been found over a vertical distance of 426 metres. The
extent of this system may  encompass the entire  lateral and vertical  extent of
the Keno Hill Quartzite bound by the Tombstone and Robert Service thrust faults.
From footwall to hanging wall the  relatively  shallow  dipping  quartzite  unit
represents better then 2000 metres of thickness and 8000 metres of strike length
where it is  intersected  by the Mount Hinton vein fault  system.  Parallel vein
fault systems may also be present.


                                       3
<PAGE>

The two  strongest  veins,  the 19 and 52 vein systems  represent the key target
area. The 19 vein has been traced through  mapping,  trenching and a defined air
photo lineament for 366 metres. Current exploration has extended the 52 vein for
1000  metres.  Geochemical  sampling has  outlined a highly  anomalous  gold and
pathfinder element anomaly  representing the projected westerly strike of the 52
Vein.

Gold and silver  mineralization  occurs within quartz veins as well as clay-rich
fault  gouge  zones  that  bound the  veins.  These  clay-rich  zones were never
historically sampled by previous operators whereas recent sampling by Yukon Gold
has shown  that  significant  gold and silver  values may be present  across the
entire vein structures and, therefore,  relatively well developed precious metal
mineralization may be present over greater widths than previously thought.  Grab
samples of 52 Vein material exposed intermittently by hand trenching and machine
trenching on a steep north  facing slope  assayed up to 6.0 g/t Au with 2350 g/t
Ag and 127.5 g/t Au with 1575 g/t Ag and a 1.30 m channel  sample ran 9.0 g/t Au
with  39.0  g/t Ag.  Results  of 2003  and 2004  exploration  on the Mt.  Hinton
property  suggest  that  the  52  vein  system  may  be  well-mineralized   with
significant gold and silver mineralization along its entire strike length.

Other veins of merit within the same area are:

      o     21 vein,  weighted  average of samples over a 22 metre strike length
            ran 42.5 g/t Au and 319 g/t Ag over average width of 105 cm.

      o     35 vein,  weighted average of samples over a 6.1 metre strike length
            ran 16.80 g/t Au and 614 g/t Ag over average width of 183 cm.

These  individual  veins  delineate  continuous  gold  mineralization  over  the
distances sampled and sampling was terminated because of talus thicknesses.

The two bulk metallurgical samples taken from the 15 and 21 veins by United Keno
Hill Mines Ltd. in 1967/68  returned  head grades of 50.88 g/t Au, 144.96 g/t Ag
and 72.32 g/t Au, 659.2 g/t Ag respectively. The geological and structural model
developed  from 100  years  of  mining  similar  structures  in the  Keno  area,
demonstrates  the potential for continuity of gold  mineralization  in the Mount
Hinton trend.  There is a very high probability of locating economic gold lenses
of such  grade  that  direct  shipping  is  possible.  All  attempts  to further
delineate  the ore shoots  contained  within the system  have been  thwarted  by
coarse  talus,  permafrost,  steep  terrain and the  difficulty in sampling clay
mineralization.  Because of the physical  setting of the known  veins,  the most
cost  effective  way  to  test  the  Mount  Hinton  trend  is  via   underground
development.

Item 9.01 Financial Statements and Exhibits.

      Exhibits

99.1 Hinton Option  Agreement  dated with an effective  date of July 7, 2005 and
executed on August 22, 2005.

--------------------------------------------------------------------------------


                                       4
<PAGE>

                                   SIGNATURES

      Pursuant to the  requirements of the Securities  Exchange Act of 1934, the
registrant  has duly  caused  this  report  to be  signed  on its  behalf by the
undersigned hereunto duly authorized.


                                        YUKON GOLD CORPORATION, INC.


Date: August 30, 2005                   By: /s/ W. Warren Holmes
                                            ------------------------------------
                                        Name:   W. Warren Holmes
                                        Title:  Chairman and CEO



                                       5
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UNITED STATES
                       SECURITIES AND EXCHANGE COMMISSION
                             WASHINGTON, D.C. 20549

                             ----------------------

                                    FORM 8-K

                             ----------------------

                                 CURRENT REPORT
                     PURSUANT TO SECTION 13 OR 15(D) OF THE
                         SECURITIES EXCHANGE ACT OF 1934

          August 30, 2005                                333-101960
           Date of Report                            Commission File Number
  (Date of earliest event reported)

                          YUKON GOLD CORPORATION, INC.
             (Exact name of registrant as specified in its charter)

          Delaware                                       98-0413063
  (State or other jurisdiction of        (I.R.S. Employer Identification Number)
   incorporation or organization)

                                 347 Bay Street
                                    Suite 408
                            Toronto, Ontario M5H 2R7
               (Address of Principal Executive Offices) (Zip Code)

                                 (416) 865-9930
              (Registrant's telephone number, including area code)

--------------------------------------------------------------------------------
Item 8.01 Other Events

On July 7, 2002, Yukon Gold Corp., our wholly owned subsidiary ("YGC"),  entered
into an option  agreement with the Hinton Syndicate to acquire a 75% interest in
the 273 unpatented  mineral claims  covering  approximately  14,000 acres in the
Mayo Mining District of the Yukon Territory, Canada. This agreement was replaced
with a revised and amended  agreement  dated as of July 7, 2005 among Yukon Gold
Corporation, Inc., YGC and the Hinton Syndicate and is referred to herein as the
"Hinton Option  Agreement." The Hinton Option Agreement  superseded the original
agreement and amendments thereto.

YGC must make  scheduled cash payments and perform  certain work  commitments to
earn up to a 75%  interest  in the mineral  claims,  subject to a 2% net smelter
return royalty in favor of the Hinton Syndicate, as further described below.

The schedule of Property Payments and Work Programs are as follows:

      PROPERTY PAYMENTS

      a. On execution of the July 7, 2002 Agreement     $   25,000 Paid
      b. On July 7, 2003                                $   75,000 Paid
      c. On July 7, 2004                                $  150,000 Paid
      d. On January 2, 2006                             $  150,000
      e. On July 7, 2006                                $  150,000
      f. On July 7, 2007                                $  150,000
      g. On July 7, 2008                                $  150,000
                                                  TOTAL $  850,000

      WORK PROGRAM-expenditures to be incurred in the following periods;

      a. July 7/02 to July 6/03                         $  150,000 Incurred
      b. July 7/03 to July 6/04                         $  250,000 Incurred
      c. July 7/04 to July 6/05                         $  325,000 Incurred
      d. July 7/05 to Dec.31/06                         $  750,000
      e. Jan. 1/07 to Dec 31/07                         $1,000,000
      f. Jan. 1/08 to Dec 31/08                         $1,250,000
      g. Jan  1/09 to Dec 31/09                         $1,500,000
                                                  TOTAL $5,225,000

All Property Payments and Work Programs due to date of this report have been
made and incurred. Work Program expenditures have exceeded those required by
approximately $75,000.

Provided all Property Payments have been made that are due prior to the Work
Program expenditure levels being attained, Yukon Gold shall have earned a:

      25% interest upon Work Program expenditures of $1,500,000

      50% interest upon Work Program expenditures of $2,500,000

      75% interest upon Work Program expenditures of $5,225,000

In some cases,  payments made to service  providers  include amounts advanced to
cover the cost of future work.  These  advances are not loans but are considered
"incurred"  exploration expenses under the terms of the Hinton Option Agreement.
Section 2.2(b) of the Hinton Option  Agreement  defines the term,  "incurred" as
follows:   "Costs  shall  be  deemed  to  have  been  "incurred"  when  YGC  has
contractually  obligated  itself to pay for such  costs or such  costs have been
paid, whichever should first occur." Consequently, the term, "incurred" includes
amounts  actually paid and amounts that YGC has obligated  itself to pay.  Under
the Hinton Option  Agreement there is also a provision that requires YGC to have
raised and have  available  the Work  Program  funds for the period from July 7,
2005 to December 31, 2006, by May 15 of 2006.

                                       2
The  Hinton  Option  Agreement  contemplates  that upon the  earlier  of:  (i) a
production  decision or (ii) investment of CDN$5.225  million or (iii) YGC has a
minority interest and decides not to spend any more money on the project,  YGC's
relationship  with the Hinton  Syndicate  will  become a joint  venture  for the
further  development  of the property.  Under the terms of the Hinton  Syndicate
Agreement, the party with the majority interest would control the joint venture.
Once the 75% interest is earned, as described above, YGC has a further option to
acquire the remaining 25% interest in the mineral  claims for a further  payment
of CDN$5,000,000.

The Hinton Option Agreement provides that the Hinton Syndicate receive a 2% "net
smelter  returns  royalty."  In the event that we exercise our option to buy-out
the remaining 25% interest of the Hinton Syndicate (which is only possible if we
have reached a 75% interest,  as described  above) then the "net smelter  return
royalty"  would  become 3% and the Hinton  Syndicate  would  retain this royalty
interest  only.  The "net smelter  return  royalty" is a percentage of the gross
revenue  received  from the sale of the ore produced  from our mine less certain
permitted expenses.

The Hinton  Option  Agreement  entitles the Hinton  Syndicate  to recommend  for
appointment one member to the board of directors of the Yukon Gold.

The Hinton Syndicate Agreements provides both parties (YGC and Hinton Syndicate)
with rights of first  refusal in the event that either party  desires to sell or
transfer its interest.

The Hinton Syndicate members, each has the option to receive their share of
property payments in stock of Yukon Gold at a 10% discount to the market and
once Yukon Gold has obtained a listing on a Canadian stock exchange YGC and
Yukon Gold have a further option to pay 40% of any property payment due after
the payment on January 2, 2006 with common stock of Yukon Gold.

The Mount Hinton  Property is located  approximately  6 miles  southeast of Keno
City and 150 north of Whitehorse in the Yukon Territory Canada.

The Hinton Property is located within the Tombstone Gold Belt immediately to the
east of the Keno-Elsa  Silver Camp.  Recognized  as one of the more  prospective
gold  regions in the world,  the  Tombstone  Gold Belt is  comprised  of several
mineral rich  districts  that extend more than 1000 km across the North American
Cordillera  (Alaska and Yukon).  Though  mineralization  types vary they are all
related to a distinctive  northwest trending belt of plutonic  intrusions termed
the Tombstone Suite.

The Mt. Hinton gold veins and silver deposits of the Keno Hill Silver Camp occur
within the Keno Hill Quartzite  where brittle failure has created major fracture
zones for mineral deposition.  The brittle quartzite represents a tectonic sheet
or bed separated by two major faults  called the  Tombstone  and Robert  Service
thrusts.  The Keno Hill Quartzite is 600 metres thick in the silver zones and as
much as 2000 metres thick on the Mt. Hinton property

Economic  silver  deposits  in the  Keno  Hill  are best  developed  within  the
relatively  brittle Keno Hill Quartzite.  Within  productive areas the ore zones
occur  throughout the full  quartzite bed from hanging wall to footwall.  Strike
lengths of individual ore shoots range from 30 to 335 metres,  with  thicknesses
ranging  from 0.3 to 30 metres.  The  Hinton  gold  zones  mirror  the  physical
characteristics  of the Keno  Hill  silver  zones  although  they are much  more
enriched in gold.

Over 50  mineralized  gold  veins,  vein  segments  and float  trains  have been
identified  on the Mount  Hinton  Property.  These veins form a broad vein fault
system,  (Mt. Hinton Gold Trend),  300 metres wide and 3000 metres long. To date
gold  mineralization  has been found over a vertical distance of 426 metres. The
extent of this system may  encompass the entire  lateral and vertical  extent of
the Keno Hill Quartzite bound by the Tombstone and Robert Service thrust faults.
From footwall to hanging wall the  relatively  shallow  dipping  quartzite  unit
represents better then 2000 metres of thickness and 8000 metres of strike length
where it is  intersected  by the Mount Hinton vein fault  system.  Parallel vein
fault systems may also be present.

                                       3
The two  strongest  veins,  the 19 and 52 vein systems  represent the key target
area. The 19 vein has been traced through  mapping,  trenching and a defined air
photo lineament for 366 metres. Current exploration has extended the 52 vein for
1000  metres.  Geochemical  sampling has  outlined a highly  anomalous  gold and
pathfinder element anomaly  representing the projected westerly strike of the 52
Vein.

Gold and silver  mineralization  occurs within quartz veins as well as clay-rich
fault  gouge  zones  that  bound the  veins.  These  clay-rich  zones were never
historically sampled by previous operators whereas recent sampling by Yukon Gold
has shown  that  significant  gold and silver  values may be present  across the
entire vein structures and, therefore,  relatively well developed precious metal
mineralization may be present over greater widths than previously thought.  Grab
samples of 52 Vein material exposed intermittently by hand trenching and machine
trenching on a steep north  facing slope  assayed up to 6.0 g/t Au with 2350 g/t
Ag and 127.5 g/t Au with 1575 g/t Ag and a 1.30 m channel  sample ran 9.0 g/t Au
with  39.0  g/t Ag.  Results  of 2003  and 2004  exploration  on the Mt.  Hinton
property  suggest  that  the  52  vein  system  may  be  well-mineralized   with
significant gold and silver mineralization along its entire strike length.

Other veins of merit within the same area are:

      o     21 vein,  weighted  average of samples over a 22 metre strike length
            ran 42.5 g/t Au and 319 g/t Ag over average width of 105 cm.

      o     35 vein,  weighted average of samples over a 6.1 metre strike length
            ran 16.80 g/t Au and 614 g/t Ag over average width of 183 cm.

These  individual  veins  delineate  continuous  gold  mineralization  over  the
distances sampled and sampling was terminated because of talus thicknesses.

The two bulk metallurgical samples taken from the 15 and 21 veins by United Keno
Hill Mines Ltd. in 1967/68  returned  head grades of 50.88 g/t Au, 144.96 g/t Ag
and 72.32 g/t Au, 659.2 g/t Ag respectively. The geological and structural model
developed  from 100  years  of  mining  similar  structures  in the  Keno  area,
demonstrates  the potential for continuity of gold  mineralization  in the Mount
Hinton trend.  There is a very high probability of locating economic gold lenses
of such  grade  that  direct  shipping  is  possible.  All  attempts  to further
delineate  the ore shoots  contained  within the system  have been  thwarted  by
coarse  talus,  permafrost,  steep  terrain and the  difficulty in sampling clay
mineralization.  Because of the physical  setting of the known  veins,  the most
cost  effective  way  to  test  the  Mount  Hinton  trend  is  via   underground
development.

Item 9.01 Financial Statements and Exhibits.

      Exhibits

99.1 Hinton Option  Agreement  dated with an effective  date of July 7, 2005 and
executed on August 22, 2005.

--------------------------------------------------------------------------------

                                       4
SIGNATURES

      Pursuant to the  requirements of the Securities  Exchange Act of 1934, the
registrant  has duly  caused  this  report  to be  signed  on its  behalf by the
undersigned hereunto duly authorized.

                                        YUKON GOLD CORPORATION, INC.

Date: August 30, 2005                   By: /s/ W. Warren Holmes
                                            ------------------------------------
                                        Name:   W. Warren Holmes
                                        Title:  Chairman and CEO

                                       5