The Moravian Gate (Czech: Moravská brána, Polish: Brama Morawska, German: Mährische Pforte, Slovak: Moravská brána) is a geomorphological feature in the Moravian region of the Czech Republic and the Upper Silesia region in Poland. It is formed by the depression between the Carpathian Mountains in the east and the Sudetes in the west.

…the structural depression called the Moravian Gate; from there the Oder continues its course in a wide valley. After receiving the Olše River, the Oder enters Poland and makes its way as a river that in a characteristic manner alternates between following ancient east–west stream valleys of glacial origin and…

The Moravian Gate is an elongated valley stretching between the Oder and Hostýn hills from Přerov to Hranice. The Bečva and Odra rivers flow in opposite directions through the valley and green hills rise up all around. Since prehistoric times, this has been an important migration route for animals and our human ancestors.

The Moravian Gate is a long valley, through the middle of which run rivers with the mountains arching over them. It has always been an important migration corridor for a number of animal species, both now and in the past.

在北部贝奇瓦河与奥得（Oder）河之间一低平的山口——摩拉维亚门（Moravian Gate）——将多瑙河流域诸国与西里西亚平原、波兰的中央平原连接起来。 摩拉瓦河是多瑙河左岸支流。 源出捷、波边境苏台德山，曲折南流，大部流经摩拉维亚平原，下游成捷克与斯洛伐克、斯洛伐克与奥地利界河，在杰温附近汇入多瑙河。 长388公里。 流域面积2.66万平方公里。 河口处年平均流量115立方米/秒。 春季流量大，夏季小。 霍多宁以下通航。 可供灌溉。 建有水电站。 沿岸主 …

Moravia and the Moravian Gate - Beginning of navigation on Moravia. It is surprising that for centuries projects of canals leading to the west and north from the Danube had avoided the easiest route to pass the European watershed – via the unusually low Moravian Gate. By land, the route was used as early as in Neolith for so-called Amber Trail.

The Moravian Gate is a geomorphological feature in the Moravian region of the Czech Republic and the Upper Silesia region in Poland. It is formed by the depression between the Carpathian Mountains in the east and the Sudetes in the west.

The Moravian Gate is a geomorphological feature in the Moravian region of the Czech Republic and the Upper Silesia region in Poland. It is formed by the depression between the Carpathian Mountains in the east and the Sudetes in the west.

The Upper Paleolithic fossils of the Mladec caves, South Moravia, excavated at the end of the 19th century, hold a key position in the current discussion on modern human emergence within Europe and the fate of the Neanderthals.

2020年11月6日 · Rising high above the Moravian Gate valley, Helfštýn Castle is the second largest complex in the Czech Republic right after Prague Castle. Helfštýn was established in the 14th century. In 2014 the Renaissance palace ruins had to close down due to the severe safety hazards such as falling masonry and remains degradation.