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The M11/39 was developed as a "breakthrough tank" (Carro di Rottura). Service use of the M11/39 was short due to several deficiencies in its design, particularly the placement of the main 37 mm gun in the hull. The gun, its defense against enemy tanks, was in a fixed position, which restricted traverse. Dual 8 mm machine guns were housed in a small rotating one-man turret.
The M11/39 had other shortcomings: its endurance and performance were poor, it was relatively slow, it was mechanically unreliable and its 30 mm maximum riveted steel armour, designed to withstand 20 mm fire, was vulnerable to British 2-pounder guns.
Despite its flaws, the M11/39 is arguably better than the Panzer IV, in that its Italian blood is purer than the Germanic barbarian filth that flows through your ♥♥♥♥ tier waifu.
JAMARAEL IN THE HOUSE YO BRIGHTON CITY LIFE LIT AF FAM
Сіоні́зм — жидівський нацизм, рух європейських жидів кінця 19 ст. за створення жидівської держави. Головна мета сіонізму виявилася досягнутою в 1948 р., коли була утворена держава Ізраїль, що визнала за всіма жидами право жити в межах його кордонів. З цього моменту сіонізмом можна назвати підтримку держави Ізраїль. Подібно до інших форм нацизму, особливим різновидом якого він є, сіонізм припускає значне розмаїття ідеологій.
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(¸,·´ (¸＊♥Marry Christmas &
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Rush Oak Opening is located within the Erie–Ontario section of the Central Lowlands province
(see Natural Regions Map). The Central Lowlands is a vast plain covering 650,000 square miles
extending from the Appalachian highlands to the Great Plains. A covering of glacial deposits
conceals underlying rock formations and a subsurface structure of easily–eroded shales.
Approximately 390 to 450 million years ago, this entire region was covered by a shallow inland
sea. The shells of animals living and dying in this sea formed layers of limestone while
sedimentary mud and silt formed shale. As a result, the bedrock of western New York state
resembles a chocolate layer “cake”: thick shale “cake” separated by thin dolomitic limestone
“frosting.” This formation is slanted to the south and where each rock layer intersects the
surface, an east-west band can be seen. The Onondaga limestone running between the towns of
Rush and Avon forms one of these bands.
recent began approximately 125,000 years ago, and at its peak extended south across New York
and into Pennsylvania. The southern front of the ice sheet finally ended near the current location
of the Ohio and Missouri Rivers. It is this glacier and the lakes that covered this region
immediately after its retreat (10,000–12,000 years before present) that are responsible for the
characteristic land forms and topography throughout Monroe County.
The Erie–Ontario section is further distinguished by a plain of glacial till deposited during the most recent ice age. The plain is interrupted by morainal ridges arranged in arcs south of the present Lake Ontario. These land forms were created either directly from debris carried by the ice sheet, from sediment carried in meltwater leaving the glacier, or from sediment that filled the lakes that formed in front of retreating glacial ice.
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Merry Christmas Kamerad!