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To do so, technique and training are crucial to turning your talent into a career. Taking a certification course will give you confidence to show others that you are serious about using your talents to create a career as an interior design professional.

Growing up watching my mother design our homes, I just thought that was what grownups did for fun. I don’t mean to make it sound glamorous, however. I am leaving out the fact that, while my mother was raising five children on her own, we did not always have our pick of homes. Luckily, growing up in Rhode Island older homes and apartments usually meant incredible architecture, wood floors, and French doors. Usually those features weren’t unveiled until after we’d removed several layers of turpentine to return historical architecture to its original beauty. My mother always believed that a beautiful home was one of the key ingredients to a proud, happy family. Turns out, she was right!

Mom a born decorator had the natural ability to balance objects and harmonize colors while always keeping in mind the function of a space. That being said, Mom would gather us up and explain to us that there was a neighbor who needed our help, and we all knew what that meant. Once again, we had to don our dungarees and fix up our neighbor’s apartment. Yes, you guessed it – Mom was never paid for her decorating talents; it was a gift she gave from her heart and she never thought of herself as deserving of any fee for creating beautiful homes for those in need. To be honest, they could not have paid anything anyway. Mother’s hobby was also her gift and she shared it with many in need.

I hope that sharing my short story will help you decide what comes next for you. After attending a college with a double major – one in fashion design and the other in interior design – I graduated with tens of thousands of dollars in debt, a nice tan, and a lot of technical information but very little hands-on experience or practical knowledge.

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If you run an online business then you probably appreciate the contribution of your website to the success of your business. As soon as your website is hosted, the main job will be to monitor online traffic with promptitude. This process cannot be overlooked since knowing website visitors statistics offers several major benefits.
You can take various steps to improve your websites presence and help it appear in the first page of search engine results page. In order for your site to rank highly, you have to enlist in the SEO optimization and the smart web design to improve its appearance on the cyber space.

The prosperity of your business on the net depends on the necessary steps you take to better it. You must pay special attention to various characteristics of your website’s traffic. This can help you optimize your business activity in many ways.

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Since many business webs are designed in a way that different pages harbor information concerning specific products, knowing how many people visit a particular page translates to the number of people liking the product therein. It is essential that you know the number of visitors for each page of the site.

By having this statistics readily available, you will be able to know the popularity of your products among your clients. It is the best tool to find out specific interests of your potential customers. Further, you can invest more on products and services that are more popular among the surfers and identify areas needing improvement.

Some software are advanced and provides more details on the visitors other than just giving a figure of visitors who surf your page. This information is essential to correctly determine specific visitor interests. This might be essential in helping you know the interests of your customers.

Website visitor statistics shows the location and places clients hail from. This is crucial in the sense that, apart from strengthening the SEO, it gives vital information on how many clients love your products. In addition, information on where visitors come from is essential for proper product and service improvements.

If you manage an online business, you need check the website visitors statistics daily. Although monitoring everyone that surfs your site is challenging, it remains one the most efficient ways to rule the cyber space. Of course, there is hard to find a better way to establish trends among those who visit your site.
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     PHYLLITE/PHYLLITIC SCHIST

This rock was seen widely. It was extensively found at Ojirami Oke. It was a hilly exposure, about 12m wide and 5m high.though, other exposures were lowlying. Generally, the rock is dark grey in colour, has medium sized grains. It appears silky. Contains biotite, quartz, plagioclase feldspar, muscovite, pyroxene, amphibole. The parallel alignment of the biotite gives it a slaty cleavage to slightly spaced cleavage. It is mineralogically banded. The mafic minerals are thin, about 1mm thick. The lighter bands (felsic), are a bit thicker, about 2-3 mm thick. The bands are alternating,which defines its’ foliation.

            QUARTZITE

This rock type is widely distributed. It’s seen near the Akoko-Edo local government secretariat as a on the side of a hill, at a river cut along Auchi-Ibillo road, as an enclave at the toe of the semolika granites. It is highly weathered in the area, and even in some it is observed as rubbles. It even occurs as clasts in some metaconglomerates. It is a light coloured rock. Contains over 90% quartz, also has muscovite and little sillimanite. The preferred alignment of the muscovite plates gives it a foliated texture. At the stream cut at Igarra-Ibillo road, it has a lot of structures.its’ angle of dip varies from gentle to steep/ almost vertical, resulting from shearing, which produced most of the structures there.

      METACONGLOMERATE

This exposure was seen a lot through out the exercise. It was seen as low lying exposures mostly. In some locations, it was seen as a road cut, and in a few cases, as a hill. It is characterized by having clasts embedded in a finer grained matrix, the clasts varies from quartz, gtanites, quartzites and even phyllites in a location. The metaconglomerates in the mapped area are polymicts, since they contain more than one kind of clast. The sizes of the clasts ranged from as small as 3cm, to as long as 1.2cm, and as wide as 7cm.The matrix generally, is fine grained, well sorted, and is lithologically banded with light bands ofcalc-silicate rocks, alternating with dark bands of pellites. The calc-silicate bands comprises of calcite, quartz, biotite and amphiboles. The pellitic bands were further banded into felsic and mafic bands.

In the western part of Igarra, the metaconglomerates were occurring in alternation with quartzites as bands (as was clearly shown using geophysical mapping methods). The metaconglomerates were formed from the metamorphism of basal conglomerates

        FAULT BRECCIA

This rock type was seen as an exposure during the Igarra northern tracverse – the river traversing, also in baboon hill, in contact with the lamprophyre dyke, and in the final granite/granodiorite locality. It is a special kind of metaconglomerate, that has very angular pebbles(thus a breccia), which are randomly oriented through out the outcrop. They are an indication of a fault zone around the areas in which they are found. The composition of the pebbles varies just like in the metaconglomerates.

 CALC-GNEISS AND MARBLE

We mapped outcrops of this rock type along the road to Ikao tpwn, west of Igarra, at southern Igwe, and we saw it in the two quarrys we visited during the course of the exercise. Its’ colour varies from dark greenish grey, to light grey at some localities, to even sky blue at the quarry. Grain size is medium to coarse. The lithological banding of the greenish and light grey bands with bands, define it’s gneissic fabric. Its’ mineralogy includes calcite, quartz, biotite, amphibole.  

GRANITE

The granites occur over a wide area. At Semolika, they are exposed as batholiths. At some localities, they were clasts in the metaconglomerates. It is light grey with pinkish patches. The grain sizes are coarse. The granites are porphyritic, with the k-feldspars forming the phenocrysts, in a ground matrix of quartz, biotite, plagioclase feldspar, other mafic minerals. The k-spars gives the rock it’s pinkish colouration. The quartz in the matrix occur as ribbons. The granite has a massive structure, but the mica in some parts of the rock had a kind of discontinuous alignment

             SYENITE

This rock type occurs as a dyke in the studied area. It is exposed as a low-lying outcrop and as a low hill. We saw it on the way to hyena hill, and on the way to baboon hill. It is dark grey green patches and has grain sizes from fine to medium.  Moving along the hyena hill, there is a coarsening upwards of the grain sizes. At first, we saw a mafic syenite, then as we moved forward, we saw a felsic syenite.  At a point on the steep slope, felsic syenite was seen inter-tonguing with the mafic syenite through fractures from this we can deduce that during the multiple intrusions of the syenite into the country rock, the mafic variety intruded first before the felsi, thus, is older.

          LAMPROPHYRE

This rock type occurs mostly as a dyke cutting across the country rocks – metaconglomerate, phyllite, and calc-gneiss. We saw it at in the southern traverse as a dyke in the metamaconglomerate without clasts(meta mar), in a river cut. We also saw it at ekpesi, in contact with the calc-silicate gneiss, pegmatite,and phyllite. We then saw it at okpe, in contact witn the quartzite, phyllitic schist, granite and quartz vein. It is dark grey in colour with fine to medium grain size. Its thickness ranges from 5 to 30cm. It contains very large plates of biote, standing out and aligned in a particular direction, then embedded within a finer-grained matrix of quartz, K-feldspars and greenish minerals.

             PEGMATITE

This rock type occurs as a dyke and pebbles in granitic bodies, quartzites, metaconglomerate etc. It has a white- pinkish colouration. It was found developed a chilled margin along the contact with the country rocks. It is granitic in composition. At the last granite/granodiorite locality, it contained very large crystals of very pinkish feldspars. The feldspars ranged from 3cm to 18cm in width, and cm to 21cm in length.

          VEIN QUARTZ

 It is an igneous intrusion which occurs almost in all the outcrops, emplaced along fractures and veining through rocks in different directions. Its dimension varies from 6cm to 1.6m and the grain size is generally medium – coarse. Deformation effect on the vein quartz resulted in sigmoidal forms in some localities.

           DOLERITE

This occurs as a dyke. The dolerite dyke has been identified as the youngest in this area. The cross-cutting relationship between dolerite and syenite reveal their age relationships. It is dark gray in colour because of its mafic composition and it is fine- grained. 

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For example, far too many people die each year because there are no working smoke detectors in the home. I say “working” because while there are smoke detectors in the home, either the battery is missing or it is simply dead and should have been replaced.

Keeping home and family safe is important to all of us but often, we don’t take action until something unpleasant happens and drives home how important it really is to be proactive and take steps to protect our families and our homes. For example, far too many people die each year because there are no working smoke detectors in the home. I say “working” because while there are smoke detectors in the home, either the battery is missing or it is simply dead and should have been replaced.

While smoke detectors that go off every time someone cooks can be annoying, it is simply too risky to disconnect them or take the battery out. Instead, open a window, use a fan, or install a vent hood over the stove to make sure that smoke and odors are being eliminated. Smoke detectors are there to save your life and the lives of your family members and should never, ever be disabled. In fact, you should test them once a month to make sure they are still working and replace the battery on a regular basis. Many experts suggest checking your smoke detectors at the beginning or end of daylight savings time because you are resetting your clocks and that is another chore you could do quickly.

Use Timers and Lights for Home Security

Whether or not you have a home security system installed, making good use of lighting and timers can help to protect your home and your family. Burglars like to work in the dark so make sure your home is one they will want to pass up by installing outside motion detectors that will turn lights on when motion is detected. These same outside lights can be used to prevent spills and falls as they will come on when they sense your motion in the dark as well. Keep entryways, driveways, and any area where there are steps well lit and you will help to prevent dangerous falls and you will also help to prevent intruders from sneaking around in the dark.

Fire Extinguishers

Keep fire extinguishers on every floor of your home and teach everyone in the family how and when to use them. Keep one in the kitchen as well and another one in the garage or workshop. Make sure you get the appropriate kind of fire extinguishers and teach your family never to pour water on electrical fires or grease fires. Keeping a fire extinguisher in your vehicle is also a good idea as well.

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Lean, juicy beef, mutton, and veal, form the basis of all good soups; therefore it is advisable to procure those pieces which afford the richest succulence, and such as are fresh-killed. Stale meat renders them bad, and fat is not so well adapted for making them. The principal art in composing good rich soup, is so to proportion the several ingredients that the flavour of one shall not predominate over another, and that all the articles of which it is composed, shall form an agreeable whole. To accomplish this, care must be taken that the roots and herbs are perfectly well cleaned, and that the water is proportioned to the quantity of meat and other ingredients. Generally a quart of water may be allowed to a pound of meat for soups, and half the quantity for gravies. In making soups or gravies, gentle stewing or simmering is incomparably the best. It may be remarked, however, that a really good soup can never be made but in a well-closed vessel, although, perhaps, greater wholesomeness is obtained by an occasional exposure to the air. Soups will, in general, take from three to six hours doing, and are much better prepared the day before they are wanted. When the soup is cold, the fat may be much more easily and completely removed; and when it is poured off, care must be taken not to disturb the settlings at the bottom of the vessel, which are so fine that they will escape through a sieve. A tamis is the best strainer, and if the soup is strained while it is hot, let the tamis or cloth be previously soaked in cold water. Clear soups must be perfectly transparent, and thickened soups about the consistence of cream. To thicken and give body to soups and gravies, potato-mucilage, arrow-root, bread-raspings, isinglass, flour and butter, barley, rice, or oatmeal, in a little water rubbed well together, are used. A piece of boiled beef pounded to a pulp, with a bit of butter and flour, and rubbed through a sieve, and gradually incorporated with the soup, will be found an excellent addition. When the soup appears to be  too thin  or  too weak , the cover of the boiler should be taken off, and the contents allowed to boil till some of the watery parts have evaporated; or some of the thickening materials, above mentioned, should be added. When soups and gravies are kept from day to day in hot weather, they should be warmed up every day, and put into fresh scalded pans or tureens, and placed in a cool cellar. In temperate weather, every other day may be sufficient.

Various herbs and vegetables are required for the purpose of making soups and gravies. Of these the principal are, Scotch barley, pearl barley, wheat flour, oatmeal, bread-raspings, pease, beans, rice, vermicelli, macaroni, isinglass, potato-mucilage, mushroom or mushroom ketchup, champignons, parsnips, carrots, beetroot, turnips, garlic, shalots and onions. Sliced onions, fried with butter and flour till they are browned, and then rubbed through a sieve, are excellent to heighten the colour and flavour of brown soups and sauces, and form the basis of many of the fine relishes furnished by the cook. The older and drier the onion, the stronger will be its flavour. Leeks, cucumber, or burnet vinegar; celery or celery-seed pounded. The latter, though equally strong, does not impart the delicate sweetness of the fresh vegetable; and when used as a substitute, its flavour should be corrected by the addition of a bit of sugar. Cress-seed, parsley, common thyme, lemon thyme, orange thyme, knotted marjoram, sage, mint, winter savoury, and basil. As fresh green basil is seldom to be procured, and its fine flavour is soon lost, the best way of preserving the extract is by pouring wine on the fresh leaves.

For the seasoning of soups, bay-leaves, tomato, tarragon, chervil, burnet, allspice, cinnamon, ginger, nutmeg, clove, mace, black and white pepper, essence of anchovy, lemon-peel, and juice, and Seville orange-juice, are all taken. The latter imparts a finer flavour than the lemon, and the acid is much milder. These materials, with wine, mushroom ketchup, Harvey’s sauce, tomato sauce, combined in various proportions, are, with other ingredients, manipulated into an almost endless variety of excellent soups and gravies. Soups, which are intended to constitute the principal part of a meal, certainly ought not to be flavoured like sauces, which are only designed to give a relish to some particular dish.
 

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