http://morgansolar.com/wp-content/uploads/2015/03/DJI_0044_Edit2.jpg

1. CNBM International Corporation
1.Project Information;
Scope of work; Related license about the FIT land lease,approval for the construction, and etc;
To obtain the final concession /permission to build a 50MW project on the land we have a lease option
on. We have the provisional concession, preliminary drawings provided to obtain this concession have
been provided to you. These are the only drawings prepared to date as this is all that has been required. So
there are no engineering design constraints.
2)Project proposal and engineering drawings
We have the provisional concession approved, preliminary drawings provided to obtain this concession
have been provided to you. These are the only drawings prepared to date as this is all that has been
required. So there are no engineering design constraints
3) FH1 If there is no suitable engineering drawings for construction, please provide:
(1)30-year Average:Monthly Averaged Insolation Incident On A Horizontal Surface,Monthly Averaged
Direct Normal Radiation On A Horizontal Surface,Monthly Averaged Diffuse Radiation Incident On A
Horizontal Surface.
( 2 )transformer substation geographical wiring diagram, power structure and load conditions
We don’t have details of this agreed yet but our site is located next to a new major substation photographs
of which are attached there is a distance of 20 meters from our site to the substation
(3) the primary main wiring diagram of transformer substation
These have not been obtained yet and will form part of the final concession
(4)the primary main wiring diagram of transformer substation, Maximum load, average load, minimum
load, the parameters of the main transformer and breaker
These have not been obtained yet and will form part of the final concession
(5) The voltage level of the station power, The location of the connection point
These have not been obtained yet and will form part of the final concession
(6)Site engineering geological data (geology, topography, groundwater depth, the thickness of the
permafrost, ground resistance)
These studies should be carried out, are part of the proposed Phase II
Ingrid/Pedro can you provide the reports that Ingrid supplied as they are in Spanish you will know which
is which also will you answer questions 7 to 10 from your own knowledge and the information Ingrid
supplied.

2. (7) Local meteorological conditions (wind, lightning, hail, earthquake).
Santiago de los Caballeros in rugged terrain in central Cibao Valley in the central region of the
Dominican Republic, one of the most fertile lands found in the island. The Yaque del Norte River passes
by Santiago, which lies between the Cordillera Central and the Cordillera Septentrional, two of the three
major mountain ranges forming the Cibao Valley.
The average temperature varies little in the city, because the tropical trade winds help mitigate the heat
and humidity throughout the year. Months December and January are the coldest and July and August are
the hottest. Santiago and the rest of the country are in the Caribbean and have a tropical climate, which,
together with the altitude of the city, 183 meters above sea level, causes cloudy conditions to persist
through much of the year. The city and the country are also apart of the hurricane zone, however,
Santiago is more sheltered than other parts of the country due to its location in the Cibao Valley.
Extreme temperatures (records) are: 41.0 ° C (105.8 ° F), the maximum temperature recorded September
13, 1960, 4 and 11.2 ° C (52.2 ° F), minimum temperature recorded on 31 January 1987.5
The annual precipitation of rain is in the order of 1,060 mm., With 111.6 days of rain / year. The driest
months are January, February and July with an average rainfall of 52 mm, The wettest months are May to
178 mm and October and November with 103 mm rainfall. In this country the rains usually come and go
in heavy showers; rains lasting several days, are extremely rare.
The wind regime can be decomposed into two parts: one due to the media or general circulation in the
structure of the atmosphere (trade winds), and other local disturbances in each region (breezes). And we
have to take into account seasonal variations.
Trade winds. These winds prevail on the island throughout the year. Are felt more on mountain systems,
where blow with greater violence.
The trade winds originate in an area of high-pressure-Atlantic anticyclone extending from Bermuda to
Spain. Begin their nearly parallel to the African coast and then turn movement westward. In the West
Indies feel come from the east throughout the year but the trend is blowing Northeast and Southeast in
winter in summer.
The action of the trade winds decisive influence on our climate and are felt more in the most exposed
areas to streams. The opposite occurs in sheltered areas, where there is no free action. The high
temperatures recorded during the summer Sánchez, La Vega, Mao, Jimaní, Villa Vásquez, Pedernales,
etc., Are caused by hills and mountains that cut the trade flows.
Brisas sea - land. These are currents that occur during the day and night in coastal areas. Its cause is the
difference in heating of the land and waters.
The sea breeze - land (sea breeze, or just breeze) ideally begins at 10 am, as a result of the temperature
difference between land and sea in the morning; recorded top speed were you doing at 2 pm then
decreases gradually having a lull in the evening that follows the offshore (land breeze - sea), due to the
different cooling of land and sea during the afternoon and evening, reaching its maximum intensity in the
early hours of the morning.

3. The sea breezes - earth are local winds, low rise, affecting areas near the coast. In the tropics can reach a
height of 1-2 km, penetrating more than 100 km inland, if no mountains that hinder them, and reaching
speeds of 20-30 km / h.
Brisas Valley - mountain. These currents are produced in a similar way to the sea breezes - land,
throughout the year. The mountain slopes are heated and cooled quickly, especially if they are rocky or
deforested, while the valley, protected by the mountains, they made more slowly. When the hot air from
the slopes rises (being replaced by the cooler valley) it cools coming to form clouds over the tops of the
mountains, and if amounts sufficient causes local rainfall, while on the center of the Valley dissolve the
clouds (when descending and warming), reigning good time.
Tropical Storms
They are complex weather phenomena characterized by strong winds, torrential rain and destructive
effects. His area of training varies throughout the hurricane season, being always near the Ecuador: Gulf
of Mexico and Western Caribbean to the island of Cape Verde in Africa.
The term tropical cyclone is applied to all circulations originating over tropical waters. Depending on the
speed of its winds, are classified as Tropical Depression, if not reach 61 km / h; Tropical storm, if you are
between 61 and 177 km / h; and Hurricane, when exceeding 117 km / h.
The south coast is the most affected region, receiving 67% of the cyclones that touch the Dominican
Republic, given its location in the path of cyclones formed east of 70 ° west and below 20 ° N, which are
the affecting the country.
The official hurricane season in the Dominican Republic (and throughout the Caribbean) is 1st. June to
May 1st. November of each year, occasionally cyclones occurring in May and December. The most
affecting the island did not begin until August, September and October being the months in which they
occur most important.
The island of Hispaniola on which is the Dominican Republic is located on the Caribbean Plate Tectonics
having a translational motion as a rigid body of 20 ± 2 mm annually, heading west-northeast (70 °);
contact edges: on the north by the North American Plate, south to the South, the West with the Nazca and
east the Atlantic Ocean Fund.
Earthquakes
On the island of Hispaniola there are several major fault systems, which are:
To the north of the fault of Hispaniola in the sea that is the edge of old plaque where the Puerto Rico
Trench (Milwaukee Trench) is located and the Northern edge active fault in northern plate, which
penetrates to the island Manzanillo Bay and continued in the southern part of the Northern Cordillera
exiting the Bay of Samana, with a length of over 300kms. This failure is similar to that of San Francisco
in California USA.
The other system is located south of the island, which penetrates through southern Haiti and continuing
through San Juan Ocoa, reaching the Caribbean Sea to the Dead Pit, south of Santo Domingo, San Pedro
de Macoris and La Romana .

4. (8)geographic coordinate range of the site
It will be located in El Naranjo section located southwest of the city of Santiago de los
Caballeros in UTM coordinates 193152.66 - 2147408.83, in Nos. 12 and 12-A of Cadastral
District No. 20 of the Municipality of Santiago Plot.
The El Naranjo section corresponds to the coordinates 2,146,500 2,149,000 m ma latitude and
315,000 m 316,000 m in length,
(9) Topographic map (CAD)
These studies should be carried out, are part of the proposed Phase II , Was developed map of the
border line plots only.
(10) NAM Soil survey report
These studies should be carried out, are part of the proposed Phase II
4. The average hourly wage for local construction workers
US$ 6.00 / Hr
5.'Payment terms :www.cnbm.com