I redirect to other page on dbase matters

reference link;

I continue via this link informations due to dbase matters (mybloginfrmtns.blogspot.com)

Update 3/23:

There are selective shaking news on Magnitude-Distance relation for Tiran;

Realities based on geologic of region

Tiran:Albania's capital and biggest city.

A geologic frame based on dense shaking phenomena;

Tiranë river flows through the city, as does the Lanë river.

I say to important stru conds reflectory seismic waves for region descripted of W part of Shkoder Lake;

There are selective shaking news on Magnitude-Distance relation for Split;

Realities based on geologic of region

Split:the second largest city of Croatia, the largest city in the region of Dalmatia and the largest city in the Adriatic coast of Croatia. 

A geologic frame based on dense shaking phenomena;

Split is situated on a peninsula between the eastern part of the Gulf of Kaštela and the Split Channel.

I say to important stru conds reflectory seismic waves for region descripted of Tihaljina Geography;

There are selective shaking news on Magnitude-Distance relation for Podgorica;

Realities based on geologic of region

Podgorica: The capital and largest city of Montenegro

A geologic frame based on dense shaking phenomena;

The area is crossed with rivers and the city itself is only 15 kilometres (9.3 mi) north of Lake Skadar. The Morača and Ribnica rivers flow through the city, while the Zeta, Cijevna, Sitnica and Mareza flow nearby. Morača is the largest river in the city, being 70 m or 230 ft wide near downtown, and having carved a 20 m or 66 ft deep canyon for the length of its course through the city.Except for the Morača and Zeta, other rivers have an appearance of small creeks. The richness in bodies of water is a major feature of the city.

I say to important stru conds reflectory seismic waves for region descripted of Western Niksic;

There are selective shaking news on Magnitude-Distance relation for Skopje;

Realities based on geologic of region

Skopje:The capital and largest city of North Macedonia

A geologic frame based on dense shaking phenomena;

The city was built in the Skopje valley, oriented on a west–east axis, along the course of the Vardar river, which flows into the Aegean Sea in Greece. The valley is approximately 20 kilometres (12 miles) wide and it is limited by several mountain ranges to the north and south. These ranges limit the urban expansion of Skopje, which spreads along the Vardar and the Serava, a small river which comes from the North.

The Skopje valley belongs to the Vardar geotectonic region, the subsoil of which is formed of Neogene and Quaternary deposits. The substratum is made of Pliocene deposits including sandstone, marl and various conglomerates. It is covered by a first layer of Quaternary sands and silt, which is between 70 and 90 m deep. The layer is topped by a much smaller layer of clay, sand, silt and gravel, carried by the Vardar river. It is between 1.5 and 5.2 m deep.

In some areas, the subsoil is karstic. It led to the formation of canyons, such as the Matka Canyon, which is surrounded by ten caves. They are between 20 and 176 m deep.

Several rivers meet the Vardar within the city boundaries. The largest is the Treska, which is 130 kilometres (81 miles) long. It crosses the Matka Canyon before reaching the Vardar on the western extremity of the City of Skopje. The Lepenac, coming from Kosovo, flows into the Vardar on the northwestern end of the urban area.

I say to important stru conds reflectory seismic waves for region descripted of Seferaj-Hakanje Geography;

Update 5/2:

There are selective shaking news on Magnitude-Distance relation for Tbilisi;

Realities based on geologic of region

Tbilisi:The capital and the largest city of Georgia

A geologic frame based on dense shaking phenomena;

The city lies in Eastern Georgia on both banks of the Kura River (locally known as Mtkvari).

The relief of Tbilisi is complex. The part of the city which lies on the left bank of the Mt'k'vari River extends for more than 30 km (19 mi) from the Avchala District to River Lochini. The part of the city which lies on the right side of the Mt'k'vari River, on the other hand, is built along the foothills of the Trialeti Range, the slopes of which in many cases descend all the way to the edges of the river Mt'k'vari. The mountains, therefore, are a significant barrier to urban development on the right bank of the Mt'k'vari River. This type of a geographic environment creates pockets of very densely developed areas while other parts of the city are left undeveloped due to the complex topographic relief.

To the north of the city, there is a large reservoir (commonly known as the Tbilisi Sea) fed by irrigation canals.

I say to important stru conds reflectory seismic waves for region;