NDA GK Questions 2026

The declaration was signed on 10 January 1966 at Tashkent in the Soviet Union by Prime Minister Lal Bahadur Shastri and President Mohammad Ayub Khan of Pakistan, with Soviet Premier Alexei Kosygin acting as mediator; it closed the war of 1965 and provided for withdrawal to the positions held before…

The Treaty of Sugauli ended the Anglo-Nepal War fought from 1814 to 1816 in the time of Lord Hastings.

Also called the Delhi Pact, it was signed by Mahatma Gandhi and Viceroy Lord Irwin.

At the Lucknow session the Congress and the Muslim League agreed on a joint demand for self-government, and the Congress accepted separate electorates for Muslims; Bal Gangadhar Tilak and Muhammad Ali Jinnah were the chief architects, and the moderates and extremists of the Congress, divided since the Surat split of…

The Communal Award of August 1932 had given the Depressed Classes separate electorates.

Fought between 1790 and 1792 between Tipu Sultan and Lord Cornwallis, supported by the Nizam and the Marathas, it ended with the Treaty of Srirangapatnam, under which Tipu surrendered about half his territory and paid a heavy war indemnity, and two of his sons were taken as hostages.

Defeated by the Holkars at Poona, the Peshwa took shelter with the Company and signed the Treaty of Bassein in December 1802, accepting Wellesley's subsidiary alliance and a British force at his capital.

That war began after the Treaty of Surat of 1775, by which the Bombay government supported Raghunath Rao's claim to the Peshwa's seat, and it ended with the Treaty of Salbai in 1782 between Warren Hastings and Mahadji Scindia.

It was signed in 1765 by Robert Clive with the Mughal Emperor Shah Alam II and Nawab Shuja-ud-Daula of Awadh after the Company's victory at Buxar in 1764.

The crust is the outermost and thinnest layer of the earth and is of two kinds. The continental crust, made largely of lighter granitic rock rich in silica and aluminium, averages about thirty kilometres in thickness and reaches about seventy kilometres under young fold mountains such as the Himalaya.

Plate tectonics, propounded in 1967, holds that the lithosphere is broken into seven major plates and a number of minor ones that move over the plastic asthenosphere.

Near Easter Island in the South Pacific the rise spreads at more than fifteen centimetres a year, the highest rate measured, while the Arctic Ridge in option A has the slowest rate of less than two and a half centimetres a year.

It lies between South America and the Pacific plate and is one of the well known minor plates, along with the Cocos, Arabian, Philippine, Caribbean, Juan de Fuca, Scotia, Caroline and Fuji plates.

Along the San Andreas Fault the Pacific plate and the North American plate slide horizontally past each other.

The Indian plate moved northwards and met the Eurasian plate. Both carry light continental crust, so neither could sink far into the mantle; instead the sediments of the Tethys Sea lying between them were compressed, folded and thrust upwards to form the Himalaya, and the collision is still going on…

After the detailed mapping of the ocean floor during and after the Second World War revealed mid-oceanic ridges, deep trenches and a surprisingly thin cover of sediment, Hess proposed in 1961 that molten material rises along the ridge, forms new ocean floor and pushes the older floor away on both…

When Pangaea began to break about two hundred million years ago, it parted into a northern mass called Laurasia or Angaraland and a southern mass called Gondwanaland, and the long narrow Tethys Sea lay between the two.

Wegener attributed the horizontal movement of the continents to the pole-fleeing force, which arises from the rotation of the earth and the bulge of the equator, and to the tidal force, which arises from the attraction of the moon and the sun.

Wegener held that about two hundred and fifty million years ago all the land of the earth lay together as one mass, Pangaea, and that one enormous ocean, Panthalassa, surrounded it.

Wegener, a German meteorologist and climatologist, put forward the continental drift theory in 1912 and developed it in his book The Origin of Continents and Oceans; he argued that all the continents once formed a single landmass, Pangaea, which broke up about two hundred million years ago.