Be Careful "The Right Abdominal Pain"

Our stomach is a hollow organ, so they have such a variety of organs located on each position, the right side of the upper abdominal organs are liver, gall bladder, kidney, small intestine and colon, whereas on the right side at the bottom There Colon, Appendix / Appendix, urinary tract, and specifically in women are ovarian Channel.

So if we are experiencing abdominal pain on the right, just look at the top or bottom, when the pain upper, it is likely that the impaired organs located on the right above, among the various organs before, the most common disorders of the the left is liver disorders, inflammation of the gall bladder due to stones, and sometimes inflammation of the small intestine can occur. But if this place was a little pain in the middle and the pain till it reached backward, it is possible that another organ kidney problems.

When the pain occur at the bottom right, the most frequent cause is inflammation of the appendix / Appendicitis, then other causes which quite often is a urinary tract infection, or the woman suspect the existence of inflammation of the ovaries.

To differentiate between appendicitis with urinary tract infections are: In the appendix accompanying symptoms are fever, may also be accompanied by nausea to vomiting and diarrhea can sometimes also be accompanied, usually a very strong pain until the patient is always bent over with suppressed pain in the lower right abdomen. While on urinary tract infections usually are frequent urination, pain when urinating, as well as the pain at the time of urine, can also be accompanied by high fever and nausea also vomited. The above picture to help identify if there are problems around the area, to make sure they still require a more thorough examination of the other and you should consult with your doctor.

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ZMAP "Seismological Software"

ZMAP is a tool that has a GUI that is designed to assist seismologist in analyzing seismic catalogs. ZMAP first introduced by Stefan Wiemer's in 1994.

Some of the capabilities and applications of ZMAP can be used among others in assessing the quality of earthquake catalogs and data exploration, mapping the values ​​of b (b value) beneath a volcano magma to infer the location information, estimates seismicity changes caused by an earthquake, stress-tensor inversion in a grid to measure the heterogeneity of stress field, mapping the magnitude of complete reporting and other applications are still a lot we can get from ZMAP.

We can meet Tool in the ZMAP include Histogram, Data Import, and Catalog Comparison, Time Series Analysis, Data Subset Selection, Map, Genas, Declustering, Mapping seismicity rates, Aftershock Decay rates, Frequency-magnitude Distribution, Magnitude of Completeness, Fractal Dimension, Quarry Maps, Time to Failure, Stress Tensor, Cumulative Misfit which each course has a purpose

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Very Local Tsunami Warning System

The establishment of the tsunami warning system is based on the fact, that the seismic waves propagate faster then tsunami wave. The tsunami wave arrive in the shore line after the earthquake parameters can be determined, so that there is time left to evaluate the earthquake, whether the earthquake is tsunamigenic or not, disseminated the information or warning to the target area, and finally to do evacuation if necessary. For the tele-tsunami, in which the tsunami will arrive in the beach more then one hour after the origin time of earthquake, generally there is enough time to do all of those processes, so that the warning can be disseminate in 100 % confidence level. For local tsunami, in which the tsunami will arrive in the beach less then one hour, the warning is disseminated in the lower the confidence level.

For example, Indonesia Tsunami Warning System (InaTEWS) is designed for local tsunami warning for Indonesian region. Any tsunami-genic earthquake occurs in the Indian Ocean plate boundary, the tsunami wave will sweep the closest shore line within 20-40 minutes after the origin time of the earthquake. The warning is determined just only based on the evaluation of the earthquake parameters and tsunami modeling. It is difficult to add sea level data to increase the confidence level of he warning. Although the confidence level is lower, the tsunami warning could be disseminated.

In some cases, especially for the eastern of Indonesia, the tsunami can be generated within inner sea, such as Flores sea, Banda sea, Ceram sea, Maluku sea, and any others. In that cases, tsunami wave will reach the closest shore line within 10 minutes or less. This tsunami may be called as very local tsunami. By evaluating the time line for issuing the tsunami warning, it is clear that very critical to disseminate tsunami warning based on the available technology recently. The effectiveness of the warning is very small, therefore another possibility warning for very local tsunami should be designed.

In this presentation, we propose to use natural signs as the warning. As we might know that in general tsunami can be generated by large earthquake. This kind earthquake could be felt strongly by most peoples. This natural sign could be applied as a tsunami warning. The other possibility is to use rather simple technology, as compliment to the natural warning. A very local tsunami warning system can be designed as the following. The warning system consist of two devices, those are a three component broadband seismograph and a local siren. The seismograph can be used to monitor and estimate the magnitude of the local earthquake and the siren can be used to warn the people if the earthquake is possible to generate tsunami. Although, the natural signs and the simple technology could be combine to establish the very local tsunami warning system, the important is to educate people so that they understand the earthquake, tsunami, and how they can save from those disasters.

Key word: Tsunami, InaTEWS, Tsunami Preparedness

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Omac "Obyek Wisata Air Cokro"

OMAC is ± 17 km towards the north of the city Klaten precisely in the Village District Cokro Tulung . OMAC has an area of ​​±15,000 m2 and is one of the favorite tourist attraction in Klaten. OMAC sidelines flowing river stretches from north to south. Water tourist area is always crowded because its location is cool, clear waters edged and beautiful views of the river flow.

Visitors who will enter these places to walk the suspension bridge that is precisely the attraction itself from other tourist objects. Panorama OMAC is cool and beautiful trees are influenced by the manager of the conserved water source that also live up to the citizens of the city of Surakarta. In addition to a convenient place for a giant surrounded by dozens of towering trees, the eye continues to flow to meet its water baths. Really clear and refreshing.

The facilities available to visitors include water boom and flying fox slide from a height above the water sliding), Water Sliding (slid into the water and the flow of water). Since the addition of water boom and flying fox, the more visitors that come each day. Especially when the weekends, Saturday and Sunday.

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This is my blog. A place to share and sharing of information and all knowledge...

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