First off, it is largely rural. There are a few medium-sized cities here, but other than that, this is a very rural area. The fact that our overall living standards are high and good is both a pro and a drawback; they are expensive, but most jobs pay well enough (well regulated minimum wages). The politicians, despite their flaws, are generally not outright wicked people who exploit us, and the checks and balances system works. It is one of the safest countries, fairly egalitarian, has no true social hierarchy (compared to most of the rest of the world), and has strong press freedom. Strong worker rights exist, and society as a whole functions well. And of course its spacious and a lot of decent natural sites. Yeah, as another con i can add that it may be hard, unless you have a very outgoing personality to get friends as an adult. Of course it is easier if you are in certain organizations (sports, hobby, religious).
Its the national flood insurance program.
The fact that the global ecosystems form broad latitudinal belts is mostly because of climatic reasons. It works very simply, the shape of the Earth doesn't allow the sun to heat up the surface equally in every place, so on the equator and around it the sun heats up the Earth the most, as the latitude changes the sun rays become weaker and weaker because they fall at a smaller angle and are dispersing much more, this forms the different climatic regions on Earth thus creating different ecosystems with it, ecosystems that have their borders mostly on the lines of change in climate from one region to another, so we mostly have latitudinal belts of ecosystems.
You might be just stuck at the border. If you're on the train to Moscow, you'd be thrown out at the Polish-Belarusian border at Terespol. How you get back is your problem, just as when you are<span> allowed in.</span>
Answer:
Granite changes into sandstone by means of weathering and erosion. Through the passage of time, fragments of granite are broken down into smaller pieces, or sediments, which are transported and deposited at the bottom of the oceans or rivers. These particles form layers of sand and pebbles that undergo compaction and cementation to create sandstone.
