An estuary is the area where a river meets the sea or ocean, where fresh water from the river meets salt water from the sea.

The soil in the delta regions are Alluvial soil.

Largest delta in India is Sunderban delta.

In the upper course of a river gradients are steep and river channels are narrow. Vertical erosion is greatest in the upper course of a river. As the result of this typical features include steep valley sides, interlocking spurs, rapids, gorges and waterfalls.

C. Khartoum

Khartoum State is one of the eighteen states of Sudan. The city is located in the heart of Sudan at the confluence of the White Nile and the Blue Nile, where the two rivers unite to form the River Nile. The confluence of the two rivers creates a unique effect. As they join, each river retains its own color which is the White Nile with its bright whiteness and the Blue Nile with its alluvial brown color. These colors are more visible in the flood season.

Land between two tributaries of a river means 'Doab'. The place where two small streams join together and results in the formation of a big river is called a DOAB. The small streams might be the tributaries of a river also.

The National River Linking Project (NRLP) is designed to ease water shortages in western and southern India while mitigating the impacts of recurrent floods in the eastern part of the Ganga basin. 

The group of depositional features formed by the Himalayan rivers is Meanders, ox-bow lake and Delta.

River system having the largest drainage system in the world is Amazon river

The flow velocity, or speed of flow, can influence the shape and rate of erosion of a river system. The cross-sectional shape of a river dictates how much friction will impact the flow of water within a river. Finally, the sediment load, or the amount of rocks and soil in the river, impacts its flow velocity and shape.

The last past of the river when it reaches the end of its journey, it is called an old river or the old stage. The end of the river is called the mouth. At the mouth, there is often a river delta, a large, silty area where the river splits into many different slow-flowing channels that have muddy banks. At this stage deposition is the only work of the river.

Erosion is the action of surface processes that remove soil, rock, or dissolved material from one location on the Earth's crust, and then transport it away to another location. The particulate breakdown of rock or soil into clastic sediment is referred to as physical or mechanical erosion; this contrasts with chemical erosion, where soil or rock material is removed from an area by its dissolving into a solvent, followed by the flow away of that solution. Eroded sediment or solutes may be transported just a few millimeters, or for thousands of kilometers.

Natural rates of erosion are controlled by the action of geomorphic drivers, such as rainfall or bedrock wear in rivers or coastal erosion by the sea and waves or glacial plucking, abrasion, and scour; areal flooding; wind abrasion; groundwater processes; and mass movement processes in steep landscapes like landslides and debris flows.

The place of origin of a river is called Source of the river. The beginning of a river, when it flows quickly with lots of energy, is called the young stage or the source. This age is also called as upper age. The river here is smaller and usually has a rapid, tumbling flow that cuts a narrow channel through rocky hills or mountains.

The V-shaped valley is formed in the youthful stage of the fluvial cycle of erosion and in the initial stage of valley development. It is deep and steep-sided river valley, both the valley sides meet together at the valley floor and thus water always touches the valley sides. The V-shaped valley is the result of the accelerated rate of downcutting.

Brahmaputra river is known as Jamua in Bangladesh.

The Sundarban forest lies in the vast delta on the Bay of Bengal formed by the super confluence of the Ganges, Hooghly, Padma, Brahmaputra and Meghna rivers across southern Bangladesh. The seasonally flooded Sundarbans freshwater swamp forests lie inland from the mangrove forests on the coastal fringe.

The Brahmaputra River, also called Yarlung Tsangpo in Tibetan language. The river originates on the Angsi Glacier located on the northern side of the Himalayas in Burang County of Tibet.

The basin comprises semi-arid valleys in the rain shadow north of the Himalaya, densely forested mountains south of the highest ranges, the scrubby Shiwalik foothills and the fertile Gangetic Plains.

Ox-bow lakes are seen in the plains of Ganga- Brahmaputra basin.

The Ganga-Brahmaputra river basin region experiences a monsoon type of climate. As is the case for a monsoon climate area, the summers are hot and the winters cool. The Ganga-Brahmaputra basin is the largest river basin in the country.

The Ganga Brahmaputra basin is situated at $10^0N$ to $30^0N$ in the sub-tropical region. The basin is formed as a result of the many tributaries from Ganga and Brahmaputra river. Some of the tributaries of Ganga or the Ganges joining the basin are the Ghaghra, the Son, the Gandhak, the Chambal, and the Kosi. The tributaries of the Brahmaputra joining the basin are Teesta and Meghna.

False.

The earliest reference to the Magadha people occurs in the Atharvaveda, where they are found listed along with the Angas, Gandharis and Mujavats. The core of the kingdom was the area of Bihar south of the Ganges.its first capital was Rajagriha (modern day Rajgir), then Pataliputra (modern Patna).

Ganga-Brahmaputra is a river basin. As a result, it gets flooded every now and then. Therefore the bulk of the soil present in the basin region will be alluvial soil.

Brahmagiri archaeological site is located in the Chitradurga district in the state of Karnataka.

At Sringaverapura near Allahabad in Uttar Pradesh, India, there exists an extraordinary example of hydraulic engineering dating back to the end of the 1st century BC. It comprises three percolation-cum-storage tanks, fed by an 11 m wide and 5 m deep canal that used to skim the floodwaters off the monsoon-swollen Ganga.

Ghod River is located in Pune District, Maharashtra, western India. It is a tributary of the Bhima River. The Ghod originates on the eastern slopes of the Western.