Nine Elms
150px
Nine Elms is our new interpretation of the classic 1930s transitional serif newspaper typeface designed by Victor Lardent and Stanley Morison, updated for modern times. Its Roman and Italic variable fonts both feature Optical Size and extensive Weight axes.
Designers
Writing Systems
Text Optical Size
Caption Optical Size
SubHead Optical Size
Headline Optical Size
OUR NATURAL WORLD
From Magma to Mountains
From towering mountain ranges to the pebbles underfoot on a sandy beach, rocks are the testament of Earth’s dynamic history, painting a story that has been billions of years in the making. These natural sculptures, with their myriad forms, colours, and compositions, are a fundamental part of our planet’s crust, playing a pivotal role in the narrative of our natural world.
Rocks come to life through three primary processes: igneous, sedimentary, and metamorphic formation. Each process lends unique characteristics to the rocks it produces, and each tells a tale of Earth’s ceaseless transformation.
Igneous rocks are born from the fiery depths of the Earth. Magma, which is molten rock material beneath the Earth’s crust, cools and solidifies, either underground or on the surface, to form igneous rocks. Those that solidify beneath the surface, like granite, are termed “intrusive” or “plutonic” and tend to have larger crystals due to slower cooling. On the other hand, rocks like basalt, which solidify quickly on the Earth’s surface following a volcanic eruption, are termed “extrusive” or “volcanic” and typically have a finer texture.
Sedimentary rocks chronicle the passage of time, layer by layer. Formed from the accumulation and compression of sediment – which can be anything from sand and mud to the remains of ancient organisms – these rocks are often found in layered strata. Over time, the accumulated sediment is subjected to pressure, leading to the formation of rocks like sandstone, limestone, and shale. Fossils, the remnants of ancient life, are often discovered within these layers, providing critical clues about the Earth’s past.
Metamorphic rocks are, as the name suggests, rocks that have undergone a transformation. When existing rocks, whether igneous or sedimentary, are subjected to immense heat and pressure, but not enough to melt them, they change in form, texture, or mineral composition. The results are often stunning – slate, which originates from shale, or marble, the metamorphosed form of limestone, are just two examples.
The tale of rock formation is a saga of fire and time, of pressures immense and transformations profound. As you next look upon a mountain, a stone, or even a pebble, remember that it holds within it the story of our Earth, a testament to the dynamic and ever-evolving natural world in which we live.
At the very core of our planet’s tapestry lies the intricate and timeless narrative of rocks. These seemingly inert formations are in fact nature’s chronicles, telling tales of Earth’s history, its processes, and its transformations. But how do these guardians of natural history form?
Our planet boasts three primary types of rocks: igneous, sedimentary, and metamorphic. Each is birthed through distinct processes, painting a comprehensive picture of the Earth’s dynamic systems.
Igneous rocks, the architects of our continents, are born from the fiery depths of our planet. As molten magma from the Earth’s mantle rises, it eventually reaches the crust and sometimes the surface. Upon cooling and solidifying, it crystallizes into igneous rock. Two varieties exist based on their origin: intrusive rocks (like granite), which cool slowly beneath the Earth’s surface, forming larger crystals, and extrusive rocks (like basalt), which cool quickly on the surface, resulting in smaller crystals.
Sedimentary rocks, on the other hand, are the storytellers of time’s passage. These rocks are formed from the accumulation and compression of sediments, which could be fragments of other rocks, organic materials, or mineral deposits. Over aeons, these layers accumulate, compact, and eventually cement together to form rocks like limestone, sandstone, or shale. Often, they are characterized by their distinct layered appearance and may preserve ancient relics of life, such as fossils.
Lastly, metamorphic rocks stand as testaments to transformation. Originating from existing rocks, whether igneous, sedimentary, or even another metamorphic rock, they undergo a metamorphosis under extreme heat and pressure without melting. This process alters their mineralogical composition and structural characteristics. Examples include marble, which is limestone’s regal transformation, or schist, showcasing beautiful foliated patterns.
It’s essential to grasp that rocks are not perennial in their form; they undergo a continual cycle of change. Igneous rocks erode into sediments, which may later form sedimentary rocks. These, under Earth’s shifting tectonic dance, might be pushed deep below the surface, altering into metamorphic types. And with enough heat, any rock can melt back into magma, restarting the cycle.
In the grand theatre of our natural world, rocks are the ever-evolving stage upon which the drama of life unfolds. They are not just inert masses, but dynamic entities that mould landscapes, influence ecosystems, and offer insights into our planet’s rich tapestry of history.
The story of rocks is a tale as old as our planet itself. Rocks, in their myriad forms, textures, and colours, are the timeless memoirs written by Earth, charting its history and the intricate processes that sculpt its surface. Understanding how rocks form offers insights not only into the geological narrative of our world but also its dynamic nature.
Rocks can be categorized into three primary types: igneous, sedimentary, and metamorphic, each formed through distinct processes.
Igneous rocks originate from molten magma that has cooled and solidified. This can happen either beneath the Earth’s crust, forming intrusive or plutonic rocks like granite, or on the surface due to volcanic activity, resulting in extrusive or volcanic rocks such as basalt. The rate at which this magma cools and the minerals present determine the rock’s texture and composition.
Sedimentary rocks, on the other hand, tell the tale of time and erosion. As rocks and minerals wear down over aeons, the resultant particles – ranging from microscopic clay to larger sand and gravel – accumulate in layers, often in basins or the beds of ancient seas. Over time, the weight of these layers, combined with the natural cementing of minerals, results in the formation of sedimentary rocks like sandstone, shale, or limestone. These rocks often capture fossils, offering invaluable windows into past ecosystems and climates.
Lastly, metamorphic rocks arise from the transformation of pre-existing rock types under intense heat and pressure within the Earth’s crust. Without melting the original rock, these conditions realign and recrystallize the minerals, producing rocks with new textures and mineralogical compositions. Slate, which originates from shale, and marble, which comes from limestone, are classic examples of metamorphic rocks.
In essence, the formation of rocks is a cyclic process, known as the rock cycle. Igneous rocks can erode to become sediments, which then solidify into sedimentary rocks. Sedimentary and igneous rocks, when subjected to heat and pressure, can metamorphose. And any rock type, when melted and then cooled, gives birth to new igneous rocks.
Our planet is in a constant state of change, with tectonic forces driving the recycling of rocks and the continents themselves. Observing the rocks around us thus becomes a way to understand our natural world in its grandest sense – a world that is ever-evolving, always in motion, and endlessly fascinating.
Features
fader
Font Styles
36px
Variable Axes
36px
Hairline | |
Hairline Italic | |
Thin | |
Thin Italic | |
Light | |
Light Italic | |
Regular | |
Italic | |
Medium | |
Medium Italic | |
SemiBold | |
SemiBold Italic | |
Bold | |
Bold Italic | |
XBold | |
XBold Italic | |
Black | |
Black Italic |
36px
Hairline | |
Hairline Italic | |
Thin | |
Thin Italic | |
Light | |
Light Italic | |
Regular | |
Italic | |
Medium | |
Medium Italic | |
SemiBold | |
SemiBold Italic | |
Bold | |
Bold Italic | |
XBold | |
XBold Italic | |
Black | |
Black Italic |
36px
Hairline | |
Hairline Italic | |
Thin | |
Thin Italic | |
Light | |
Light Italic | |
Regular | |
Italic | |
Medium | |
Medium Italic | |
SemiBold | |
SemiBold Italic | |
Bold | |
Bold Italic | |
XBold | |
XBold Italic | |
Black | |
Black Italic |
36px
Hairline | |
Hairline Italic | |
Thin | |
Thin Italic | |
Light | |
Light Italic | |
Regular | |
Italic | |
Medium | |
Medium Italic | |
SemiBold | |
SemiBold Italic | |
Bold | |
Bold Italic | |
XBold | |
XBold Italic | |
Black | |
Black Italic |
Buy Licences
① Choose Fonts
Nine Elms 1-Axis Variable Font Weight Axis: Hairline to Black, Text Optical Size only, Upright only. Also includes a Family Pack of the 9 matching static fonts. Show styles | From £100.00 |
Nine Elms 2-Axis Variable Font Weight Axis: Hairline to Black, Optical Size Axis: Caption to Headline, Upright only. Also includes a Family Pack of the 36 matching static fonts. Show styles | From £205.00 |
Nine Elms 3-Axis Variable Font Weight Axis: Hairline to Black, Optical Size Axis: Caption to Headline, Italic Axis: Upright and Italic. Also includes a Family Pack of the 72 matching static fonts. Show styles | From £405.00 |
Static Fonts
Hairline | Nine Elms Text Hairline | From £34.00 |
Thin | Nine Elms Text Thin | From £34.00 |
Light | Nine Elms Text Light | From £34.00 |
Regular | Nine Elms Text Regular | From £34.00 |
Medium | Nine Elms Text Medium | From £34.00 |
SemiBold | Nine Elms Text SemiBold | From £34.00 |
Bold | Nine Elms Text Bold | From £34.00 |
XBold | Nine Elms Text XBold | From £34.00 |
Black | Nine Elms Text Black | From £34.00 |
Hairline Italic | Nine Elms Text Hairline Italic | From £34.00 |
Thin Italic | Nine Elms Text Thin Italic | From £34.00 |
Light Italic | Nine Elms Text Light Italic | From £34.00 |
Italic | Nine Elms Text Italic | From £34.00 |
Medium Italic | Nine Elms Text Medium Italic | From £34.00 |
SemiBold Italic | Nine Elms Text SemiBold Italic | From £34.00 |
Bold Italic | Nine Elms Text Bold Italic | From £34.00 |
XBold Italic | Nine Elms Text XBold Italic | From £34.00 |
Black Italic | Nine Elms Text Black Italic | From £34.00 |
Hairline | Nine Elms Caption Hairline | From £34.00 |
Thin | Nine Elms Caption Thin | From £34.00 |
Light | Nine Elms Caption Light | From £34.00 |
Regular | Nine Elms Caption Regular | From £34.00 |
Medium | Nine Elms Caption Medium | From £34.00 |
SemiBold | Nine Elms Caption SemiBold | From £34.00 |
Bold | Nine Elms Caption Bold | From £34.00 |
XBold | Nine Elms Caption XBold | From £34.00 |
Black | Nine Elms Caption Black | From £34.00 |
Hairline Italic | Nine Elms Caption Hairline Italic | From £34.00 |
Thin Italic | Nine Elms Caption Thin Italic | From £34.00 |
Light Italic | Nine Elms Caption Light Italic | From £34.00 |
Italic | Nine Elms Caption Italic | From £34.00 |
Medium Italic | Nine Elms Caption Medium Italic | From £34.00 |
SemiBold Italic | Nine Elms Caption SemiBold Italic | From £34.00 |
Bold Italic | Nine Elms Caption Bold Italic | From £34.00 |
XBold Italic | Nine Elms Caption XBold Italic | From £34.00 |
Black Italic | Nine Elms Caption Black Italic | From £34.00 |
Hairline | Nine Elms SubHead Hairline | From £34.00 |
Thin | Nine Elms SubHead Thin | From £34.00 |
Light | Nine Elms SubHead Light | From £34.00 |
Regular | Nine Elms SubHead Regular | From £34.00 |
Medium | Nine Elms SubHead Medium | From £34.00 |
SemiBold | Nine Elms SubHead SemiBold | From £34.00 |
Bold | Nine Elms SubHead Bold | From £34.00 |
XBold | Nine Elms SubHead XBold | From £34.00 |
Black | Nine Elms SubHead Black | From £34.00 |
Hairline Italic | Nine Elms SubHead Hairline Italic | From £34.00 |
Thin Italic | Nine Elms SubHead Thin Italic | From £34.00 |
Light Italic | Nine Elms SubHead Light Italic | From £34.00 |
Italic | Nine Elms SubHead Italic | From £34.00 |
Medium Italic | Nine Elms SubHead Medium Italic | From £34.00 |
SemiBold Italic | Nine Elms SubHead SemiBold Italic | From £34.00 |
Bold Italic | Nine Elms SubHead Bold Italic | From £34.00 |
XBold Italic | Nine Elms SubHead XBold Italic | From £34.00 |
Black Italic | Nine Elms SubHead Black Italic | From £34.00 |
Hairline | Nine Elms Headline Hairline | From £34.00 |
Thin | Nine Elms Headline Thin | From £34.00 |
Light | Nine Elms Headline Light | From £34.00 |
Regular | Nine Elms Headline Regular | From £34.00 |
Medium | Nine Elms Headline Medium | From £34.00 |
SemiBold | Nine Elms Headline SemiBold | From £34.00 |
Bold | Nine Elms Headline Bold | From £34.00 |
XBold | Nine Elms Headline XBold | From £34.00 |
Black | Nine Elms Headline Black | From £34.00 |
Hairline Italic | Nine Elms Headline Hairline Italic | From £34.00 |
Thin Italic | Nine Elms Headline Thin Italic | From £34.00 |
Light Italic | Nine Elms Headline Light Italic | From £34.00 |
Italic | Nine Elms Headline Italic | From £34.00 |
Medium Italic | Nine Elms Headline Medium Italic | From £34.00 |
SemiBold Italic | Nine Elms Headline SemiBold Italic | From £34.00 |
Bold Italic | Nine Elms Headline Bold Italic | From £34.00 |
XBold Italic | Nine Elms Headline XBold Italic | From £34.00 |
Black Italic | Nine Elms Headline Black Italic | From £34.00 |
② Choose Licences
③ Confirm Your Selection
Item | ||
---|---|---|
Selected Fonts | Licences | |
Nothing selected | ||
Subtotal | VAT or sales tax will be calculated at checkout, depending on your location | £0.00 |
VAT or sales tax will be calculated at checkout, depending on your location