Much of the southern border is formed by tributaries of the Congo River, with the Mbomou River in the east merging with the Uele River to form the Ubangi River.

Much of southern and western Connecticut ( along with the majority of the state's population ) is part of the New York metropolitan area ; three of Connecticut's eight counties are statistically included in the New York City combined statistical area, the same area is widely referred to as the Tri-State area.

Much of the western, southern, and central mountains are open woodland ; supporting pine forest interspersed with some oak, scrub, and grassy clearings.

Much of Khammouan Province and the eastern part of all the southern provinces are mountainous.

Much of central and western Mongolia, including Ulaanbaatar, is antipodal to southern Patagonia.

Much of the continent has just one species of rabbit, the tapeti, while most of South America's southern cone is without rabbits.

Much of the population of the Scandinavian Peninsula is naturally concentrated in its southern part, which is also its agricultural region.

Much of Baltimore County is suburban in character, straddling the border between the Piedmont plateau and, in the southern regions of the county, the Atlantic coastal plain.

Much of the southern region is semi-arid and desert.

Much of the southern portion of the county lies within the Catskill Mountains.

Much larger forms are found in the later rocks of the upper part of the Jurassic and the lower part of the Cretaceous, such as Titanites from the Portland Stone of Jurassic of southern England, which is often 53 centimetres ( 2 feet ) in diameter, and Parapuzosia seppenradensis of the Cretaceous period of Germany, which is one of the largest known ammonites, sometimes reaching 2 metres ( 6. 5 feet ) in diameter.

Much of the terrain of eastern Polk County is mountainous, including Big Frog Mountain, constituting part of the southern Appalachian Mountains.

Much of the southern border of the county runs directly along the Ohio River.

Much of the southern part of the route runs through rural areas of Salem and Gloucester counties, passing through the communities of Woodstown and Mullica Hill.

Much of the city's southern border is shared with the Talladega National Forest.

Much of southern Ontario still contains dairy farms and other agricultural farms.

Much of the southern section of town is urbanized and is difficult to distinguish from neighboring New Haven.

Much of Peru is forested, with a large portion of the northern third of town covered by a wildlife management area, and much of the southern third covered by the Peru and Middlefield State Forests.

Much of the population is concentrated in two areas ; one, the Lebanon Mills and Perrins Crossing neighborhoods in the north, and the other, the southern neighborhoods of Luthers Corners and South Seekonk, mostly located between Interstate 195 and Route 44.

Much of the central and southern part of town is covered by Monroe State Forest, which extends into neighboring Florida.

Much of Hanover's eastern and southern borders consist of three waterways, the North and Indian Head rivers along the south and southeast, and the Third Herring Brook along the east.

Much of southern Allegheny County is undermined, and the PADEP indicates that all of Bethel Park was undermined.

Much of the town's southern ramparts were destroyed in this process and converted into residential areas.

Much of the material culture of the Kofun period demonstrates that Japan at this time was in close political and economic contact with continental Asia, especially with the southern dynasties of China, via the countries of the Korean peninsula.

Much of central Asia and southern Russia was won over to Islam through the missionary work of the ṭarīqahs, and the majority of Indonesia's population, where a Muslim army never set foot, was converted to Islam by the perseverance of both Muslim traders and Sufi missionaries.

Much money has been spent for land amelioration projects involving the installation of drainage pipes, the straightening and deepening of natural streams, the digging of drainage ditches, and the construction of polder dams.

Much of the rest of the county tended to be swampy due to the level ground and lack of sufficient natural waterways, so drainage channels had to be dug to make the land suitable for farming.

Much of the township lies within the drainage area of Flowerfield Creek, which is part of the Rocky River Sub-Watershed, itself part of the larger St. Joseph River Watershed.

Much of Wagga Wagga is situated on heavy clay soils in a large drainage basin with a small catchment discharge point.

Much as how a watershed in British and Australian usage refers to " the ridge or crest line dividing two drainage areas ", a television watershed also serves as a dividing line – it divides the time between where content for families and / or children has to be aired, and where content aimed towards an adult audience can be aired ( there is no obligation to ).

Much of its drainage basin is fertile silt and clay deposited by former glacial Lake Souris.

Much of the modern suburb is located within the former Perth Wetlands area, with significant drainage work being conducted in the area between 1832 and the 1880s.

Much of the Forked Deer drainage basin was initially wetlands ; however much of this area has been drained and most Forked Deer tributaries have been channelized for agricultural In the mid-20th century much of this was done under the auspices of the Obion-Forked Deer Basin Authority, a Tennessee state agency.

Much of it was actually marshland or slough -- a drainage area for the neighborhood.

Much of the bored sections are 21 – 23 m below the surface, with the lowest point at Marino, towards the southern end, a point that also hosts the tunnel's drainage sump.

Much of the drainage of the karstic region is not on the surface but travels in underground channels.

Much of the area to the south and west of Boston, some, was inundated by the Great Flood of 1763, and against this background, the Black Sluice Drainage and Navigation Act 1765 was obtained which created the Black Sluice Commissioners, giving them power to raise taxes and authority to carry out drainage works.

Much of the land surrounding Howden is separated by many drainage dykes.

Much of the emissions from peatlands in Borneo are due to changes in their hydrological regime, caused by drainage from nearby plantations ( particularly oil palm ).

Much of the canal beyond has been filled in, although drainage channels closely follow its route.

Much of this habitat has been degraded or destroyed by drainage of the salt marshes for agriculture or development and by runoff from surrounding farms and the city of Lincoln.