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<div class="wp-block-cover is-light has-custom-content-position is-position-bottom-center"><span aria-hidden="true" class="wp-block-cover__background has-background-dim"></span><img class="wp-block-cover__image-background" alt="" src="https://img.rawpixel.com/s3fs-private/rawpixel_images/website_content/a010-markusspiske-jan19-msp_0709_8832.jpg?w=1200&amp;h=1200&amp;fit=clip&amp;crop=default&amp;dpr=1&amp;q=75&amp;vib=3&amp;con=3&amp;usm=15&amp;cs=srgb&amp;bg=F4F4F3&amp;ixlib=js-2.2.1&amp;s=81b80c4b527f7afa9ceed195f02d27f3" data-object-fit="cover" /><div class="wp-block-cover__inner-container"><!-- wp:paragraph {"align":"center","fontSize":"large"} -->
<p class="has-text-align-center has-large-font-size">Mountain nature scene</p>
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<p>A <strong>mountain</strong> is an elevated portion of the <a href="https://en.wikipedia.org/wiki/Earth%27s_crust">Earth's crust</a>, generally with steep sides that show significant exposed <a href="https://en.wikipedia.org/wiki/Bedrock">bedrock</a>. A mountain differs from a <a href="https://en.wikipedia.org/wiki/Plateau">plateau</a> in having a limited summit area, and is larger than a <a href="https://en.wikipedia.org/wiki/Hill">hill</a>, typically rising at least 300 metres (1000 feet) above the surrounding land. A few mountains are isolated <a href="https://en.wikipedia.org/wiki/Summit_(topography)">summits</a>, but most occur in <a href="https://en.wikipedia.org/wiki/Mountain_range">mountain ranges</a>.</p>
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<p><a href="https://en.wikipedia.org/wiki/Mountain_formation">Mountains are formed</a> through <a href="https://en.wikipedia.org/wiki/Tectonic_plate">tectonic forces</a>, <a href="https://en.wikipedia.org/wiki/Erosion">erosion</a>, or <a href="https://en.wikipedia.org/wiki/Volcanism">volcanism</a>, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly levelled through the action of <a href="https://en.wikipedia.org/wiki/Weathering">weathering</a>, through <a href="https://en.wikipedia.org/wiki/Slump_(geology)">slumping</a> and other forms of <a href="https://en.wikipedia.org/wiki/Mass_wasting">mass wasting</a>, as well as through <a href="https://en.wikipedia.org/wiki/Erosion">erosion</a> by <a href="https://en.wikipedia.org/wiki/River">rivers</a> and <a href="https://en.wikipedia.org/wiki/Glacier">glaciers</a>.</p>
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