Psquare’s House Locked Up Over Failure To Perform At A Show After Getting Paid, Their Security Guard Left Injured (Graphic Photo)

According to report, Lagos high court Sheriffs today stormed the music duo’s home with a court order to seize property following a judgement against them.

When the security men at P-Square’s home refused them entry, saying the brothers were not home, they allegedly forced their way in injuring one security guard.

Source revealed that many years ago there was a show in Benin that they were supposed to perform in. After they were paid N1million, the brothers arrived Benin for the show only to be told that the show had been postponed till the next day.

P-Square refused to stay till the next day and returned to Lagos. The organizer of the show demanded for his money back and when he didn’t get it, took the case to court. He got a court judgement and promptly moved to Lagos.

The source further said the case had been in court all this while but the brother’s weren’t really aware of it as no one represented them. It looks like judgement may have been passed in absentia, which brought the court Sheriffs to their home today. They tried to tow a vehicle after showing the papers brought from the court but no one would allow them take any car away. 

Police Identifies Body Of Woman Found Near School

Police have released the identity of a woman who was found dead near a Newport News middle school Feb. 11.

Police say just before 5 p.m., a woman was walking her dog towards the rear of Gildersleeve Middle School located in the first block of Minton Drive.

The dog found an unresponsive individual lying on the ground near the woodline of the school.

Officers arrived to find an adult female who medics pronounced dead at the scene.

The victim has been identified as 38-year-old Camille Andrea Roush of the 1000 block of Garden Creek Road in Mathews County. Her cause of death has not been determined, police say. Investigators are waiting on toxicology results.

According to police, at this time, the death does not appear to be suspicious.

CHEVRON/NNPC SCHOLARSHIP

Chevron Nigeria Limited, in collaboration with its Joint Venture partner, the Nigerian National Petroleum Corporation (NNPC), is offering a number of University Scholarship Awards to suitably qualified Nigerian students.


Eligibility
E-applications are invited from full-time SECOND YEAR (200 LEVEL) degree students of the under-listed courses in Nigerian Universities:

1. Accountancy

2. Agricultural Engineering/Agricultural Science

3. Architecture

4. Business Administration/Economics

5. Chemical Engineering

6. Civil Engineering

7. Computer Science/Computer Engineering/System Engineering

8. Electrical/Electronic Engineering

9. Environmental Studies/Surveying

10. Geology/Geophysics

11. Law

12. Mass Communication/Journalism

13. Mechanical/Metallurgical & Materials Engineering

14. Human Medicine/Dentistry/Pharmacy

15. Petroleum Engineering

Instructions
In line with our e-scholarship administration system, selected students will be invited for computer-administered qualifying tests in selected examination centers nationwide. Short-listed candidates for the qualifying test will be invited by email and SMS text messages. All applicants are therefore advised to ensure that valid GSM telephone numbers and personal email addresses are properly entered into the e-forms on the web site.

Please note that applicants for the NNPC/CNL JV scholarship are ineligible to apply for any other scholarship program sponsored by Chevron Nigeria Limited, its JV Partners, or any of its affiliates, including the Agbami scholarship program published simultaneously with this NNPC/CNL JV scholarship program

ONLY SHORTLISTED CANDIDATES WILL BE CONTACTED.

APPLICANTS ARE REQUIRED TO ENTER VALID PERSONAL BANK ACCOUNT DETAILS.

MULTIPLE APPLICATION LEADS TO AUTOMATIC DISQUALIFICATION.

Please note that applicants for the NNPC/CNL JV scholarship are ineligible to apply for any other scholarship program sponsored by Chevron Nigeria Limited, its JV Partners, or any of its affiliates, including the Agbami scholarship program published simultaneously with this NNPC/CNL JV scholarship program.

Application is open to full-time SECOND YEAR (200 LEVEL) students admitted during 2014/2015 academic session.

1. Before you start this application, ensure you have clear scanned copies of the following documents

Passport photograph with white background not more than 3 months old (450px by 450px not more than 200kb)
School ID card
Admission letter
Birth certificate
O' Level result
JAMB Result
2. Ensure the documents are named according to what they represent to avoid mixing up documents during upload
3. Ensure you attach the appropriate documents when asked to upload

How To Apply
‡To apply, visit http://www.scholastica.ng/candidate/login?ReturnUrl=%2fschemes%2fapply%2f5056 and follow the steps below:

1. Click on "Register Now" to create an account.
2. Proceed to your email box to activate your account
3. Click on http://scholastica.ng/schemes/cnlawards to return to Scholarship site
4. Enter your registered email and password to upload your information.
5. Enter your personal information, National Identification Number (if available), educational information, other information and upload required scanned documents.
6. Ensure the name used in applications matches the names on all documentation in same order. Upload a sworn affidavit or certificate if otherwise.
7. Ensure you view all documents after uploading, to eliminate errors during uploading.
8. When asked to upload photo, upload a pass-port photograph with a white background.
9. Recheck application information to avoid errors
10. Click "Apply Now" to submit information
11. You will receive an email and a sms that confirms your application was successful.
12. Return to www.scholastica.ng, enter your Email and Password to download your profile and proceed to have your Head of Department sign the document.
13. Upload a scanned copy of the signed profile, this would be used for verification.
14. If National Identification Number (NIN) number was not available in step 6, to obtain your National Identification Number (NIN)
Visit http://ninenrol.gov.ng to register and learn more about the National Identity Number
Click "Create Account" and fill in the required fields
Login with Email and Password to complete the form
After completion, schedule a date for photo and finger print capture
Visit any of the 37 capture centres http://www.nimc.gov.ng/?q=nin-registration-centres to complete the registration process and obtain your National Identity Number
You can also do your total registration at the NIMC office
15. Return to and update application with National Identification Number (NIN) to ensure completion

Note: Multiple applications attract a disqualification penalty from the Scholarship board.

Deadline: Closing date for receipt of e-applications is strictly 9 March, 2016.

GEOLOGY: THE FIELD REPORT ONE

CHAPTER ONE

INTRODUCTION

Geology is a field oriented and field dependent discipline. It is not possible to appreciate the beauty of geology without a substantial portion of time being spent on the field activities. This help to better understand the theoretical background of geology provided in classroom. Geological field mapping exercise require detailed survey, sampling, identification, examination and interpretation of rock samples, fossils and minerals, and the production of valid report including the geological map of the area 

This presents the report of the intensive geological field mapping exercise covering Ogunmakin and environs between longitudes E 003⁰ 45’ to 003⁰ 50’ and latitudes N 07⁰ 10’ 30’’ to 07⁰ 13’ (Fig. 1.1) located on part of Ibadan sheet 281NE (on scale 1:100,000 topographical map), covering approximately 43 square kilometers. Some of the villages in area of study include Omi-Leragun, Omi-Fatokun, Fadipe, Bankole, Olonde, Sola, Seko, Dada, Onigbagbo, Abuku, Olubadan e.t.c. 

The geological field mapping exercise was carried out in these areas between the 30^th of August, 2015 and 9^th of September, 2015. Ogunmakin and  its environs lies within the Pre-Cambrian Basement Complex of southwestern Nigeria composed predominantly of migmatitic and granitic gneisses; quartzite; slightly migmatised to unmigmatised metasedimentary schist and metaigenous rocks; charnokitic, gabbroic and dioritic rocks; and the members of the Older granite suite mainly granites, granodiorites and syenites.

1.2   Objectives

The objectives of the field exercise include the following:

• To identify the lithologic units in the study area.
• To determine the relationships of various lithologic units present in the area.
• To analyze the petrography of the rock samples.
• To produce a detailed geological map of the study area.
• To identify the structural features and determine their orientations.

 1.3       Location and Accessibility

The studied section located within coordinates longitudes E 003⁰ 45’ to 003⁰ 50’ and latitudes N 07⁰ 10’ 30’’ to 07⁰ 13’. Important settlements in the study area include Omi-Leragun, Omi-Fatokun, Fadipe, Bankole, Olonde, Sola, Seko, Dada, Onigbagbo, Abuku, Olubadan among others.

The area is also well accessible by networks of major and minor roads, as well as foot paths linking the villages together. This facilitates easy movement during the mapping exercise. Some of the footpaths have been upgraded to minor roads while new ones have also been created see (Fig.1.2). Figure 1.1 shows the sampling locations while Table 1.1 presents the geographical coordinates for the sample locations

Table 1.1: Coordinates of the outcrops in the area of study

Location No.	Outcrops	Northing	Easting	Elevation (m)
1	A	070 10’ 59.5”	0030 49’19.3”	117.2
	B	070 11’ 03.8”	0030  49’19.2”	105.7
	C	070 11’ 21.9”	0030 49’16.4”	119.6
2		070 11’ 20.5”	0030 46’ 50.4”	118.4
3	A	070 11’ 13.4”	0030 46’57.4”	106.6
	B	070 12’ 20.5”	0030 46’ 24.0”	110
4	A	070 12’ 31.9”	0030 46’ 00.2”	94.4
	B	070  12’20.6”	0030 46’24.0”	108.9
5		07⁰ 12’50.6”	0030 45’48.3”	118.6
6		070 10’56.6”	0030 48’44.8”	130.1
7		070 11’ 54.2”	0030 48’52.0”	128.4
8		070 12’12.6”	0030 48’28.4”	130.7
9		070 11’20.1”	003046’49.8”	109.2
10		07012’08.4”	003049’10.6”	142.8
11		07011’42.5”	0030 49’11.8”	127.6
12		07011’38.7”	003049’57.2”	143.2

1.4. Climate and vegetation

The area is characterized by rain forest; derived savannah (Fig. 1.3a). The rainy season and the dry season alternating each other are typical of the rain forest belt, including the study area. The rainy season starts in March/April and runs through September/October and with annual rainfall of 1000-1500mm (40-60 in). The dry season is between November and March with mean annual temperature of 21⁰C-30⁰C. These two seasons are caused by the moist maritime south western monsoon winds which blow on land from the Atlantic Ocean for the rainy season and dry dust laden winds which blow from the Sahara deserts for dry season (harmattan).

The dry season is usually marked with bright sunshine, the northeast trade winds known as the harmattan keeps the humidity/wetness extremely low, most vegetation remains dry and most of the rivers and streams in the area are dried up or at a relatively low energy level. However, the vegetation of the area have been cultivated into secondary forest type characterized by thick to light vegetation composed mainly of cultivated palm trees, teak, mango, cashew, etc. During cultivation and farming, the natural vegetation is mostly destroyed through bush burning. This has led to deforestation of the natural and cultivated trees. A pictorial view of the type of vegetation present in the area is shown in Figure 1.3b. Hence, this vegetation is made up of palm trees, timbers of all kinds, averagely tall, long grasses and resistant shrubs of various species.

Fig 1.3a: vegetation map of the study area

Fig. 1.3b:  Photograph showing the vegetation of the study area

1.5. Topography and Drainage

The studied area is characterized by moderate relief in some area while in some other area there is presence of flood plain relative to the hills around the area.  The major rock exposures are expressed as hills with the highest elevation being above 140m.

The drainage system is characterized by streams and rivers that flow from the northern end towards the southern end. Most of the rivers and streams are very dry during the period of this mapping exercise, this indicate that they are seasonal. The streams and rivers flow almost parallel to the strike of the rocks in the study area. This is an indication that they are structurally controlled. Their tributaries form a dendritic drainage pattern covering the study area (Fig. 1.4).

GEOLOGY: THE FIELD REPORT

CHAPTER ONE

INTRODUCTION

Geology is a field oriented and field dependent discipline. It is not possible to appreciate the beauty of geology without a substantial portion of time being spent on the field activities. This help to better understand the theoretical background of geology provided in classroom. Geological field mapping exercise require detailed survey, sampling, identification, examination and interpretation of rock samples, fossils and minerals, and the production of valid report including the geological map of the area 

This presents the report of the intensive geological field mapping exercise covering Ogunmakin and environs between longitudes E 003⁰ 45’ to 003⁰ 50’ and latitudes N 07⁰ 10’ 30’’ to 07⁰ 13’ (Fig. 1.1) located on part of Ibadan sheet 281NE (on scale 1:100,000 topographical map), covering approximately 43 square kilometers. Some of the villages in area of study include Omi-Leragun, Omi-Fatokun, Fadipe, Bankole, Olonde, Sola, Seko, Dada, Onigbagbo, Abuku, Olubadan e.t.c. 

The geological field mapping exercise was carried out in these areas between the 30^th of August, 2015 and 9^th of September, 2015. Ogunmakin and  its environs lies within the Pre-Cambrian Basement Complex of southwestern Nigeria composed predominantly of migmatitic and granitic gneisses; quartzite; slightly migmatised to unmigmatised metasedimentary schist and metaigenous rocks; charnokitic, gabbroic and dioritic rocks; and the members of the Older granite suite mainly granites, granodiorites and syenites.

   1.2   Objectives

The objectives of the field exercise include the following:

• To identify the lithologic units in the study area.
• To determine the relationships of various lithologic units present in the area.
• To analyze the petrography of the rock samples.
• To produce a detailed geological map of the study area.
• To identify the structural features and determine their orientations.

 1.3       Location and Accessibility

The studied section located within coordinates longitudes E 003⁰ 45’ to 003⁰ 50’ and latitudes N 07⁰ 10’ 30’’ to 07⁰ 13’. Important settlements in the study area include Omi-Leragun, Omi-Fatokun, Fadipe, Bankole, Olonde, Sola, Seko, Dada, Onigbagbo, Abuku, Olubadan among others.

The area is also well accessible by networks of major and minor roads, as well as foot paths linking the villages together. This facilitates easy movement during the mapping exercise. Some of the footpaths have been upgraded to minor roads while new ones have also been created see (Fig.1.2). Figure 1.1 shows the sampling locations while Table 1.1 presents the geographical coordinates for the sample locations

     Table 1.1: Coordinates of the outcrops in the area of study

Location No.	Outcrops	Northing	Easting	Elevation (m)
1	A	070 10’ 59.5”	0030 49’19.3”	117.2
	B	070 11’ 03.8”	0030  49’19.2”	105.7
	C	070 11’ 21.9”	0030 49’16.4”	119.6
2		070 11’ 20.5”	0030 46’ 50.4”	118.4
3	A	070 11’ 13.4”	0030 46’57.4”	106.6
	B	070 12’ 20.5”	0030 46’ 24.0”	110
4	A	070 12’ 31.9”	0030 46’ 00.2”	94.4
	B	070  12’20.6”	0030 46’24.0”	108.9
5		07⁰ 12’50.6”	0030 45’48.3”	118.6
6		070 10’56.6”	0030 48’44.8”	130.1
7		070 11’ 54.2”	0030 48’52.0”	128.4
8		070 12’12.6”	0030 48’28.4”	130.7
9		070 11’20.1”	003046’49.8”	109.2
10		07012’08.4”	003049’10.6”	142.8
11		07011’42.5”	0030 49’11.8”	127.6
12		07011’38.7”	003049’57.2”	143.2

 1.4. Climate and vegetation

The area is characterized by rain forest; derived savannah (Fig. 1.3a). The rainy season and the dry season alternating each other are typical of the rain forest belt, including the study area. The rainy season starts in March/April and runs through September/October and with annual rainfall of 1000-1500mm (40-60 in). The dry season is between November and March with mean annual temperature of 21⁰C-30⁰C. These two seasons are caused by the moist maritime south western monsoon winds which blow on land from the Atlantic Ocean for the rainy season and dry dust laden winds which blow from the Sahara deserts for dry season (harmattan).

The dry season is usually marked with bright sunshine, the northeast trade winds known as the harmattan keeps the humidity/wetness extremely low, most vegetation remains dry and most of the rivers and streams in the area are dried up or at a relatively low energy level. However, the vegetation of the area have been cultivated into secondary forest type characterized by thick to light vegetation composed mainly of cultivated palm trees, teak, mango, cashew, etc. During cultivation and farming, the natural vegetation is mostly destroyed through bush burning. This has led to deforestation of the natural and cultivated trees. A pictorial view of the type of vegetation present in the area is shown in Figure 1.3b. Hence, this vegetation is made up of palm trees, timbers of all kinds, averagely tall, long grasses and resistant shrubs of various species.

Fig 1.3a: vegetation map of the study area

Fig. 1.3b:  Photograph showing the vegetation of the study area

1.5. Topography and Drainage

The studied area is characterized by moderate relief in some area while in some other area there is presence of flood plain relative to the hills around the area.  The major rock exposures are expressed as hills with the highest elevation being above 140m.

The drainage system is characterized by streams and rivers that flow from the northern end towards the southern end. Most of the rivers and streams are very dry during the period of this mapping exercise, this indicate that they are seasonal. The streams and rivers flow almost parallel to the strike of the rocks in the study area. This is an indication that they are structurally controlled. Their tributaries form a dendritic drainage pattern covering the study area.