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13 de abr. de 2024 · The Great Marsh (Japanese: 大湿原 Great Marsh) is an area located in Pastoria City. It is Sinnoh's Safari Zone and contains some Pokémon that cannot be found anywhere else in Sinnoh. It is filled with marshy areas, which, unlike normal marsh tiles, have tall grass inhabited by wild Pokémon.
- Gumshoos
Release information. This card was included in the Ultra...
- Discussion
I’ve been doing extensive research on the bait/mud mechanic...
- Marshy Areas
A marsh tile is a special tile introduced in Pokémon Diamond...
- A Skuffle with Skorupi
Through binoculars, Diamond watches a Carnivine inside the...
- Parks
Pages in category "Parks" The following 21 pages are in this...
- Game Freeze
A game freeze is an event where a game stops responding to...
- Gumshoos
El Gran Pantano (Great Marsh en inglés; だいしつげん Gran Pantano en japonés) es un lugar situado al norte de Ciudad Pradera en Sinnoh.
The Great Marsh is the Sinnoh Safari Zone where you can catch various Pokémon with Bait or Mud. Learn how to use binoculars to find daily special Pokémon and their flee rates.
The Great Marsh is a region in the Pokémon game Sinnoh, where the Safari Zone is located. It has six areas with different Pokémon and items, and daily special encounters.
El Gran Pantano (Great Marsh en inglés, だいしつげん Gran Pantano en japonés) es un lugar situado al norte de Ciudad Pradera en Sinnoh. Se trata de una gran extensión de terreno dividida en seis sectores formados por hierba alta y baja, barro (donde el personaje puede quedar atascado) y agua en su mayoría.
20 de ago. de 2023 · This is a map and walkthrough for Great Marsh, the Sinnoh region's very own safari zone in Pokemon Brilliant Diamond and Shining Pearl (BDSP). Learn about the mechanics of the Great Marsh, the Great Marsh Daily Pokemon, what Pokemon are found in each area, and what trainers, items, and events are encountered here.
The Great Black Swamp (also known simply as the Black Swamp) was a glacially fed wetland in northwest Ohio and northeast Indiana, United States, that existed from the end of the Wisconsin glaciation until the late 19th century.
