Alissa W. Zinoviena

Alissa W. Zinoviena

Descripción

Minsk, my birth place, is located on the southeastern slope of the Minsk Hills, a region of rolling hills running from the southwest (upper reaches of the river Nioman) to the northeast – that is, to Lukomskaye Lake in northwestern [Belarus]. The average altitude above sea level is 220 metres (720 ft). The geography of Minsk was formed during the two most recent ice ages. The Svislach River, which flows across the city from the northwest to the southeast, is located in the urstromtal, an ancient river valley formed by water flowing from melting ice sheets at the end of the last Ice Age. Minsk was initially developed on the hills, which allowed for defensive fortifications. However, in the 20th century, it grew to include the relatively flat plains in the southeast.[citation needed] The western parts of the city are the most hilly.

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Intereses

Fe, filosofía y espiritualidad Músicas del mundo y otras Historia y humanidades


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Comentarios

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La hora de Kayako

Gracias por seguirnos!!! Estamos muy agradecidos de que te guste nuestro programa... Un saludo!

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radiobanyeres

Gracias por apoyar el audio de nuestra compañera y amiga Martha Escudero. Desde Radio Banyeres te deseamos unas felices fiestas

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Tojo

Gracias Alissa ,un saludo desde Madrid

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Superduque

Never I´ll would imagine I`ll found you again in a web of mine. About your question, actually I`m in Spain due to my job. Better kisses from your always friend..... Love, Super.

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Marta

Gracias Alissa por tus recomendaciones, me alegro que te gusten. Un beso

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Juan Manuel Pérez Gu

Alissa W. Zinoviebna te saludo desde Tabasco , México

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Alissa W. Zinoviebna

Minsk, my birth place, is located on the southeastern slope of the Minsk Hills, a region of rolling hills running from the southwest (upper reaches of the river Nioman) to the northeast – that is, to Lukomskaye Lake in northwestern [Belarus]. The average altitude above sea level is 220 metres (720 ft). The geography of Minsk was formed during the two most recent ice ages. The Svislach River, which flows across the city from the northwest to the southeast, is located in the urstromtal, an ancient river valley formed by water flowing from melting ice sheets at the end of the last Ice Age. Minsk was initially developed on the hills, which allowed for defensive fortifications. However, in the 20th century, it grew to include the relatively flat plains in the southeast.[citation needed] The western parts of the city are the most hilly.

Por decisión del propietario, no se aceptan comentarios anónimos. Regístrate en iVoox para comentarlo.

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