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user: 그레이 스케일 필터와 2개의 열이 있는 영웅 이미지.

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<p class="has-text-align-center has-large-font-size">산의 자연 풍경</p>
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<p><strong>산</strong>은 지각의 높은 부분으로, 일반적으로 가파른 면이 노출된 <a href="https://en.wikipedia.org/wiki/Earth%27s_crust">암반</a>이 있는 <a href="https://en.wikipedia.org/wiki/Bedrock">지형</a>입니다. 산은 정상 면적이 제한되어 있다는 점에서 <a href="https://en.wikipedia.org/wiki/Plateau">고원</a>과 다르며, 일반적으로 주변 땅에서 최소 300미터(1000피트) 이상 솟아 있는 <a href="https://en.wikipedia.org/wiki/Hill">언덕</a>보다 더 큽니다. 몇몇 산은 고립된 <a href="https://en.wikipedia.org/wiki/Summit_(topography)">정상</a>이지만, 대부분은 <a href="https://en.wikipedia.org/wiki/Mountain_range">산맥</a>에 속해 있습니다.</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 leveled 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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