A 10-style OpenType family by travis kochel
Otari
Pyroclastic flow
Beware of subduction!
fissures & rift valleys
Ngauruhoe
ANDESITE CINDER CONE
Explosive Caldera
Supervolcano POSSIBLE LAHAR ZONE
highly viscous bombs of lava
Mafic basalt magma
ABCDEFGHIJK LMNOPQRSTU V WXYZ abcdefghijklmn opqrstuv wxyz
Otari Bold 96 pt
Light & Light Italic Regular & Regular Italic Medium & Medium Italic Bold & Bold Italic Heavy & Heavy Italic 72 pt
Light BAS IC ALPHABE T
PRES E T AND ARBIT RARY FRAC T IONS
ABCDEFGHIJKLMNOPQRSTUVWXYZ abcdefghijklmnopqrstuvwxyz
0/0 1/2 1/3 2/3 1/4 2/4 3/4 1/5 2/5 3/5 4/5 1/6 3/6 5/6 1/7 2/7 3/7 4/7 5/7 6/7 1/8 3/8 5/8 7/8 1/9 2/9 4/9 5/9 7/9 8/9 376/958
PUNC T UAT ION AND SYMBOLS
,;:.…!¡?¿‘’“”‚„‘”‹›«»#@&•·()[]{}/|¦\-–—_^~*†‡§¶©®™ªº +−±×÷=≠<>≤≥¬∂ΩΔΠ∑μπμ∫∞√≈◊
S UPERIOR AND INFERIOR
0123456789(.,+-=/) 0123456789(.,+-=/) L ANGUAGE S UPPORT
00123456789$¢€£¥ 00123456789$¢€£¥
ÀÁÂÃÄÅĀĂĄÆÇĆĈĊČĎĐÈÉÊËĒĔĖĘĚĜĞĠĢĤĦ ÌÍÎÏĨĪĬĮİIJĴĶĹĻĿĽŁŃŅÑŇŊÒÓÔÕÖŌŎŐŒØŔŖŘŚ ŜŞŠŢ Ț Ť ŦÙÚÛÜŨŪŬŮŰŲŴÝŶŸŹŻŽÞ àáâãäåāăąæçćĉċčďđðèéêëēĕėęěĝğġģĥħìíîïĩīĭįı ijĵķĸĺŀļľ łńņňʼnñŋòóôõöōŏőœøŕŗřśŝşšșţțťŧùúûüũ ūŭůűųŵÿ ý ŷźżžſþĸ
PR OPORT IONAL & TABUL AR LINING NU MERALS
SMALL CAP S & ALL SMALL CAP S
LIGAT URES
fi ff ffi fj ffj fl ffl fb fh fk fl tt ft Tb Th Tk Tl Ti ch ck ct st PR OPORT IONAL & TABUL AR OLD ST YLE NU MERALS
00123456789$¢€£¥ 0012345689$¢€£¥
abcdefghijklmnopqrstuvwxyz0123456789&¡!¿?@\|/ ()[]{}àáâãäåāăąæçćĉċčďđèéêëēĕėęěĝğġģĥħìíî ïĩīĭįıijĵķĸĺŀļľłńņňʼnñŋòóôõöōŏőœøŕŗřśŝşšșţ țťŧùúûüũūŭůűųŵÿýŷźżžþ
Light Italic BAS IC ALPHABE T
PRES E T AND ARBIT RARY FRAC T IONS
ABCDEFGHIJKLMNOPQRSTUVWXYZ abcdefghijklmnopqrstuvwxyz
0/0 1/2 1/3 2/3 1/4 2/4 3/4 1/5 2/5 3/5 4/5 1/6 3/6 5/6 1/7 2/7 3/7 4/7 5/7 6/7 1/8 3/8 5/8 7/8 1/9 2/9 4/9 5/9 7/9 8/9 376/958
PUNC T UAT ION AND SYMBOLS
,;:.…!¡?¿‘’“”‚„‘”‹›«»#@&•·()[]{}/|¦\-–—_^~*†‡§¶©®™ªº +−±×÷=≠<>≤≥¬∂ΩΔΠ∑μπμ∫∞√≈◊
S UPERIOR AND INFERIOR
0123456789(.,+-=/) 0123456789(.,+-=/) L ANGUAGE S UPPORT
00123456789$¢€£¥ 00123456789$¢€£¥
ÀÁÂÃÄÅĀĂĄÆÇĆĈĊČĎĐÈÉÊËĒĔĖĘĚĜĞĠĢĤ ĦÌÍÎÏĨĪĬĮİIJĴĶĹĻĿĽŁŃŅÑŇŊÒÓÔÕÖŌŎŐŒØŔŖŘ ŚŜŞŠŢ Ț Ť ŦÙÚÛÜŨŪŬŮŰŲŴÝŶŸŹŻŽÞ àáâãäåāăąæçćĉċčďđðèéêëēĕėęěĝğġģĥħìíîïĩīĭ įıijĵķĸĺŀļľ łńņňʼnñŋòóôõöōŏőœøŕŗřśŝşšșţțťŧùúûü ũūŭůűųŵÿýŷźżžſþĸ
PR OPORT IONAL & TABUL AR LINING NU MERALS
SMALL CAP S & ALL SMALL CAP S
LIGAT URES
fi ff ffi fj ffj fl ffl fb fh fk fl tt ft Tb Th Tk Tl Ti ch ck ct st PR OPORT IONAL & TABUL AR OLD ST YLE NU MERALS
00123456789$¢€£¥ 0012345689$¢€£¥
abcdefghijklmnopqrstuvwxyz0123456789&¡!¿?@\|/ ()[]{}àáâãäåāăąæçćĉċčďđðèéêëēĕėęěĝğġģĥħì íîïĩīĭįıijĵķĸĺŀļľłńņňʼnñŋòóôõöōŏőœøŕŗřśŝşš șţțťŧùúûüũūŭůűųŵÿýŷźżžþ
Regular BAS IC ALPHABE T
PRES E T AND ARBIT RARY FRAC T IONS
ABCDEFGHIJKLMNOPQRSTUVWXYZ abcdefghijklmnopqrstuvwxyz
0/0 1/2 1/3 2/3 1/4 2/4 3/4 1/5 2/5 3/5 4/5 1/6 3/6 5/6 1/7 2/7 3/7 4/7 5/7 6/7 1/8 3/8 5/8 7/8 1/9 2/9 4/9 5/9 7/9 8/9 376/958
PUNC T UAT ION AND SYMBOLS
,;:.…!¡?¿‘’“”‚„‘”‹›«»#@&•·()[]{}/|¦\-–—_^~*†‡§¶©®™ªº +−±×÷=≠<>≤≥¬∂ΩΔΠ∑μπμ∫∞√≈◊
S UPERIOR AND INFERIOR
0123456789(.,+-=/) 0123456789(.,+-=/) L ANGUAGE S UPPORT
00123456789$¢€£¥ 00123456789$¢€£¥
ÀÁÂÃÄÅĀĂĄÆÇĆĈĊČĎĐÈÉÊËĒĔĖĘĚĜĞĠĢĤĦ ÌÍÎÏĨĪĬĮİIJĴĶĹĻĿĽŁŃŅÑŇŊÒÓÔÕÖŌŎŐŒØŔŖŘŚ ŜŞŠŢȚŤŦÙÚÛÜŨŪŬŮŰŲŴÝŶ ŸŹŻŽÞ àáâãäåāăąæçćĉċčďđðèéêëēĕėęěĝğġģĥħìíîïĩīĭįı ijĵķĸĺŀļľ łńņňʼnñŋòóôõöōŏőœøŕŗřśŝşšșţțťŧùúûüũ ūŭůűųŵÿýŷźżžſþĸ
PR OPORT IONAL & TABUL AR LINING NU MERALS
SMALL CAP S & ALL SMALL CAP S
LIGAT URES
fi ff ffi fj ffj fl ffl fb fh fk fl tt ft Tb Th Tk Tl Ti ch ck ct st PR OPORT IONAL & TABUL AR OLD ST YLE NU MERALS
00123456789$¢€£¥ 0012345689$¢€£¥
abcdefghijklmnopqrstuvwxyz0123456789&¡!¿?@\|/ ()[]{}àáâãäåāăąæçćĉċčďđðèéêëēĕėęěĝğġģĥħ ìíîïĩīĭįıijĵķĸĺŀļľłńņňʼnñŋòóôõöōŏőœøŕŗřśŝş šșţ ț ť ŧùúûüũūŭůűųŵÿýŷźżžþ
Regular Italic BAS IC ALPHABE T
PRES E T AND ARBIT RARY FRAC T IONS
ABCDEFGHIJKLMNOPQRSTUVWXYZ abcdefghijklmnopqrstuvwxyz
0/0 1/2 1/3 2/3 1/4 2/4 3/4 1/5 2/5 3/5 4/5 1/6 3/6 5/6 1/7 2/7 3/7 4/7 5/7 6/7 1/8 3/8 5/8 7/8 1/9 2/9 4/9 5/9 7/9 8/9 376/958
PUNC T UAT ION AND SYMBOLS
,;:.…!¡?¿‘’“”‚„‘”‹›«»#@&•·()[]{}/|¦\-–—_^~*†‡§¶©®™ªº +−±×÷=≠<>≤≥¬∂ΩΔΠ∑μπμ∫∞√≈◊
S UPERIOR AND INFERIOR
0123456789(.,+-=/) 0123456789(.,+-=/) L ANGUAGE S UPPORT
00123456789$¢€£¥ 00123456789$¢€£¥
ÀÁÂÃÄÅĀĂĄÆÇĆĈĊČĎĐÈÉÊËĒĔĖĘĚĜĞĠĢĤĦ ÌÍÎÏĨĪĬĮİIJĴĶĹĻĿĽŁŃŅÑŇŊÒÓÔÕÖŌŎŐŒØŔŖŘŚ ŜŞŠŢȚŤŦÙÚÛÜŨŪŬŮŰŲŴÝŶŸŹŻŽÞ àáâãäåāăąæçćĉċčďđðèéêëēĕėęěĝğġģĥħìíîïĩīĭį ıijĵķĸĺŀļľ łńņňʼnñŋòóôõöōŏőœøŕŗřśŝşšșţțťŧùúûü ũūŭůűųŵÿýŷźżžſþĸ
PR OPORT IONAL & TABUL AR LINING NU MERALS
SMALL CAP S & ALL SMALL CAP S
LIGAT URES
fi ff ffi fj ffj fl ffl fb fh fk fl tt ft Tb Th Tk Tl Ti ch ck ct st PR OPORT IONAL & TABUL AR OLD ST YLE NU MERALS
00123456789$¢€£¥ 0012345689$¢€£¥
abcdefghijklmnopqrstuvwxyz0123456789&¡!¿?@\|/ ()[]{}àáâãäåāăąæçćĉċčďđðèéêëēĕėęěĝğġģĥħ ìíîïĩīĭįıijĵķĸĺŀļľłńņňʼnñŋòóôõöōŏőœøŕŗřśŝş šșţțťŧùúûüũūŭůűųŵÿýŷźżžþ
Medium BAS IC ALPHABE T
PRES E T AND ARBIT RARY FRAC T IONS
ABCDEFGHIJKLMNOPQRSTUVWXYZ abcdefghijklmnopqrstuvwxyz
0/0 1/2 1/3 2/3 1/4 2/4 3/4 1/5 2/5 3/5 4/5 1/6 3/6 5/6 1/7 2/7 3/7 4/7 5/7 6/7 1/8 3/8 5/8 7/8 1/9 2/9 4/9 5/9 7/9 8/9 376/958
PUNC T UAT ION AND SYMBOLS
,;:.…!¡?¿‘’“”‚„‘”‹›«»#@&•·()[]{}/|¦\-–—_^~*†‡§¶©®™ ªº+−±×÷=≠<>≤≥¬∂ΩΔΠ∑μπμ∫∞√≈◊
S UPERIOR AND INFERIOR
0123456789(.,+-=/) 0123456789(.,+-=/) L ANGUAGE S UPPORT
00123456789$¢€£¥ 00123456789$¢€£¥
ÀÁÂÃÄÅĀĂĄÆÇĆĈĊČĎĐÈÉÊËĒĔĖĘĚĜĞĠĢĤĦ ÌÍÎÏĨĪĬĮİIJĴĶĹĻĿĽŁŃŅÑŇŊÒÓÔÕÖŌŎŐŒØŔŖŘŚ ŜŞŠŢ Ț Ť ŦÙÚÛÜŨŪŬŮŰŲŴÝŶ ŸŹŻŽÞ àáâãäåāăąæçćĉċčďđðèéêëēĕėęěĝğġģĥħìíîïĩīĭįı ijĵķĸĺŀļľ łńņňʼnñŋòóôõöōŏőœøŕŗřśŝşšșţțťŧùúûüũ ūŭůűųŵÿýŷźżžſþĸ
PR OPORT IONAL & TABUL AR LINING NU MERALS
SMALL CAP S & ALL SMALL CAP S
LIGAT URES
fi ff ffi fj ffj fl ffl fb fh fk fl tt ft Tb Th Tk Tl Ti ch ck ct st PR OPORT IONAL & TABUL AR OLD ST YLE NU MERALS
00123456789$¢€£¥ 0012345689$¢€£¥
abcdefghijklmnopqrstuvwxyz0123456789&¡!¿?@\|/ ()[]{}àáâãäåāăąæçćĉċčďđðèéêëēĕėęěĝğġģĥħ ìíîïĩīĭįıijĵķĸĺŀļľłńņňʼnñŋòóôõöōŏőœøŕŗřśŝş šșţțťŧùúûüũūŭůűųŵÿýŷźżžþ
Medium Italic BAS IC ALPHABE T
PRES E T AND ARBIT RARY FRAC T IONS
ABCDEFGHIJKLMNOPQRSTUVWXYZ abcdefghijklmnopqrstuvwxyz
% 1/2 1/3 2/3 1/4 2/4 3/4 1/5 2/5 3/5 4/5 1/6 3/6 5/6 1/7 2/7 3/7 4/7 5/7 6/7 1/8 3/8 5/8 7/8 1/9 2/9 4/9 5/9 7/9 8/9 376/958
PUNC T UAT ION AND SYMBOLS
,;:.…!¡?¿‘’“”‚„‘”‹›«»#@&•·()[]{}/|¦\-–—_^~*†‡§¶©®™ªº +−±×÷=≠<>≤≥¬∂ΩΔΠ∑μπμ∫∞√≈◊
S UPERIOR AND INFERIOR
0123456789(.,+-=/) 0123456789(.,+-=/) L ANGUAGE S UPPORT
00123456789$¢€£¥ 00123456789$¢€£¥
ÀÁÂÃÄÅĀĂĄÆÇĆĈĊČĎĐÈÉÊËĒĔĖĘĚĜĞĠĢĤĦ ÌÍÎÏĨĪĬĮİIJĴĶĹĻĿĽŁŃŅÑŇŊÒÓÔÕÖŌŎŐŒØŔŖŘŚ ŜŞŠŢ Ț Ť ŦÙÚÛÜŨŪŬŮŰŲŴÝŶŸŹŻŽÞ àáâãäåāăąæçćĉċčďđðèéêëēĕėęěĝğġģĥħìíîïĩīĭį ıijĵķĸĺŀļľ łńņňʼnñŋòóôõöōŏőœøŕŗřśŝşšșţțťŧùúûü ũūŭůűųŵÿýŷźżžſþĸ
PR OPORT IONAL & TABUL AR LINING NU MERALS
SMALL CAP S & ALL SMALL CAP S
LIGAT URES
fi ff ffi fj ffj fl ffl fb fh fk fl tt ft Tb Th Tk Tl Ti ch ck ct st PR OPORT IONAL & TABUL AR OLD ST YLE NU MERALS
00123456789$¢€£¥ 0012345689$¢€£¥
abcdefghijklmnopqrstuvwxyz0123456789&¡!¿?@\| /()[]{}àáâãäåāăąæçćĉċčďđðèéêëēĕėęěĝğġģĥ ħìíîïĩīĭįıijĵķĸĺŀļľłńņňʼnñŋòóôõöōŏőœøŕŗřśŝ şšșţțťŧùúûüũūŭůűųŵÿýŷźżžþ
Bold BAS IC ALPHABE T
PRES E T AND ARBIT RARY FRAC T IONS
ABCDEFGHIJKLMNOPQRSTUVWXYZ abcdefghijklmnopqrstuvwxyz
0/0 1/2 1/3 2/3 1/4 2/4 3/4 1/5 2/5 3/5 4/5 1/6 3/6 5/6 1/7 2/7 3/7 4/7 5/7 6/7 1/8 3/8 5/8 7/8 1/9 2/9 4/9 5/9 7/9 8/9 376/958
PUNC T UAT ION AND SYMBOLS
,;:.…!¡?¿‘’“”‚„‘”‹›«»#@&•·()[]{}/|¦\-–—_^~*†‡§¶©®™ ªº+−±×÷=≠<>≤≥¬∂ΩΔΠ∑μπμ∫∞√≈◊
S UPERIOR AND INFERIOR
0123456789(.,+-=/) 0123456789(.,+-=/) L ANGUAGE S UPPORT
00123456789$¢€£¥ 00123456789$¢€£¥
ÀÁÂÃÄÅĀĂĄÆÇĆĈĊČĎĐÈÉÊËĒĔĖĘĚĜĞĠĢĤ ĦÌÍÎÏĨĪĬĮİIJĴĶĹĻĿĽŁŃŅÑŇŊÒÓÔÕÖŌŎŐŒØŔŖ ŘŚŜŞŠŢ Ț Ť ŦÙÚÛÜŨŪŬŮŰŲŴÝŶ ŸŹŻŽÞ àáâãäåāăąæçćĉċčďđðèéêëēĕėęěĝğġģĥħìíîïĩīĭįı ijĵķĸĺŀļľ łńņňʼnñŋòóôõöōŏőœøŕŗřśŝşšșţțťŧùúûü ũūŭůűųŵ ÿ ý ŷźżžſþĸ
PR OPORT IONAL & TABUL AR LINING NU MERALS
SMALL CAP S & ALL SMALL CAP S
LIGAT URES
fi ff ffi fj ffj fl ffl fb fh fk fl tt ft Tb Th Tk Tl Ti ch ck ct st PR OPORT IONAL & TABUL AR OLD ST YLE NU MERALS
00123456789$¢€£¥ 0012345689$¢€£¥
abcdefghijklmnopqrstuvwxyz0123456789&¡!¿?@\| /()[]{}àáâãäåāăąæçćĉċčďđðèéêëēĕėęěĝğġģĥ ħìíîïĩīĭįıijĵķĸĺŀļľłńņňʼnñŋòóôõöōŏőœøŕŗřś ŝşšșţ ț ť ŧùúûüũūŭůűųŵ ÿýŷźżžþ
Bold Italic BAS IC ALPHABE T
PRES E T AND ARBIT RARY FRAC T IONS
ABCDEFGHIJKLMNOPQRSTUVWXYZ abcdefghijklmnopqrstuvwxyz
0/0 1/2 1/3 2/3 1/4 2/4 3/4 1/5 2/5 3/5 4/5 1/6 3/6 5/6 1/7 2/7 3/7 4/7 5/7 6/7 1/8 3/8 5/8 7/8 1/9 2/9 4/9 5/9 7/9 8/9 376/958
PUNC T UAT ION AND SYMBOLS
,;:.…!¡?¿‘’“”‚„‘”‹›«»#@&•·()[]{}/|¦\-–—_^~*†‡§¶©®™ ªº +−±×÷=≠<>≤≥¬∂ΩΔΠ∑μπμ∫∞√≈◊
S UPERIOR AND INFERIOR
0123456789(.,+-=/) 0123456789(.,+-=/) L ANGUAGE S UPPORT
00123456789$¢€£¥ 00123456789$¢€£¥
ÀÁÂÃÄÅĀĂĄÆÇĆĈĊČĎĐÈÉÊËĒĔĖĘĚĜĞĠĢĤ ĦÌÍÎÏĨĪĬĮİIJĴĶĹĻĿĽŁŃŅÑŇŊÒÓÔÕÖŌŎŐŒØŔŖ ŘŚŜŞŠŢ Ț Ť ŦÙÚÛÜŨŪŬŮŰŲŴÝŶ ŸŹŻŽÞ àáâãäåāăąæçćĉċčďđðèéêëēĕėęěĝğġģĥħìíîïĩīĭ įıijĵķĸĺŀļľ łńņňʼnñŋòóôõöōŏőœøŕŗřśŝşšșţțťŧùúû üũūŭůűųŵÿýŷźżžſþĸ
PR OPORT IONAL & TABUL AR LINING NU MERALS
SMALL CAP S & ALL SMALL CAP S
LIGAT URES
fi ff ffi fj ffj fl ffl fb fh fk fl tt ft Tb Th Tk Tl Ti ch ck ct st PR OPORT IONAL & TABUL AR OLD ST YLE NU MERALS
00123456789$¢€£¥ 0012345689$¢€£¥
abcdefghijklmnopqrstuvwxyz0123456789&¡!¿?@\| /()[]{}àáâãäåāăąæçćĉċčďđðèéêëēĕėęěĝğġģĥ ħìíîïĩīĭįıijĵķĸĺŀļľłńņňʼnñŋòóôõöōŏőœøŕŗřś ŝşšșţ ț ť ŧùúûüũūŭůűųŵ ÿýŷźżžþ
Heavy BAS IC ALPHABE T
PRES E T AND ARBIT RARY FRAC T IONS
ABCDEFGHIJKLMNOPQRSTUVWXYZ abcdefghijklmnopqrstuvwxyz
% 1/2 1/3 2/3 1/4 2/4 3/4 1/5 2/5 3/5 4/5 1/6 3/6 5/6 1/7 2/7 3/7 4/7 5/7 6/7 1/8 3/8 5/8 7/8 1/9 2/9 4/9 5/9 7/9 8/9 376/958
PUNC T UAT ION AND SYMBOLS
,;:.…!¡?¿‘’“”‚„‘”‹›«»#@&•·()[]{}/|¦\-–—_^~*†‡§¶©® ™ªº+−±×÷=≠<>≤≥¬∂ΩΔΠ∑μπμ∫∞√≈◊
S UPERIOR AND INFERIOR
0123456789(.,+-=/) 0123456789(.,+-=/) L ANGUAGE S UPPORT
00123456789$¢€£¥ 00123456789$¢€£¥
ÀÁÂÃÄÅĀĂĄÆÇĆĈĊČĎĐÈÉÊËĒĔĖĘĚĜĞĠĢĤ ĦÌÍÎÏĨĪĬĮİIJĴĶĹĻĿĽŁŃŅÑŇŊÒÓÔÕÖŌŎŐŒØŔ ŖŘŚŜŞŠŢ Ț Ť ŦÙÚÛÜŨŪŬŮŰŲŴÝŶ ŸŹŻŽÞ àáâãäåāăąæçćĉċčďđðèéêëēĕėęěĝğġģĥħìíîïĩī ĭįıijĵķĸĺŀļľ łńņňʼnñŋòóôõöōŏőœøŕŗřśŝşšșţțťŧù úûüũūŭůűųŵÿ ý ŷźżžſþĸ
PR OPORT IONAL & TABUL AR LINING NU MERALS
SMALL CAP S & ALL SMALL CAP S
LIGAT URES
fi ff ffi fj ffj fl ffl fb fh fk fl tt ft Tb Th Tk Tl Ti ch ck ct st PR OPORT IONAL & TABUL AR OLD ST YLE NU MERALS
00123456789$¢€£¥ 0012345689$¢€£¥
abcdefghijklmnopqrstuvwxyz0123456789&¡!¿?@ \|/()[]{}àáâãäåāăąæçćĉċčďđðèéêëēĕėęěĝğġģ ĥħìíîïĩīĭįıijĵķĸĺŀļľłńņňʼnñŋòóôõöōŏőœøŕŗ řśŝşšșţ ț ť ŧ ùúûüũūŭůűųŵÿýŷźżžþ
Heavy Italic BAS IC ALPHABE T
PRES E T AND ARBIT RARY FRAC T IONS
ABCDEFGHIJKLMNOPQRSTUVWXYZ abcdefghijklmnopqrstuvwxyz
% 1/2 1/3 2/3 1/4 2/4 3/4 1/5 2/5 3/5 4/5 1/6 3/6 5/6 1/7 2/7 3/7 4/7 5/7 6/7 1/8 3/8 5/8 7/8 1/9 2/9 4/9 5/9 7/9 8/9 376/958
PUNC T UAT ION AND SYMBOLS
,;:.…!¡?¿‘’“”‚„‘”‹›«»#@&•·()[]{}/|¦\-–—_^~*†‡§¶©® ™ªº+−±×÷=≠<>≤≥¬∂ΩΔΠ∑μπμ∫∞√≈◊
S UPERIOR AND INFERIOR
0123456789(.,+-=/) 0123456789(.,+-=/) L ANGUAGE S UPPORT
00123456789$¢€£¥ 00123456789$¢€£¥
ÀÁÂÃÄÅĀĂĄÆÇĆĈĊČĎĐÈÉÊËĒĔĖĘĚĜĞĠĢĤ ĦÌÍÎÏĨĪĬĮİIJĴĶĹĻĿĽŁŃŅÑŇŊÒÓÔÕÖŌŎŐŒØŔ ŖŘŚŜŞŠŢ Ț Ť ŦÙÚÛÜŨŪŬŮŰŲŴÝŶŸŹŻŽÞ àáâãäåāăąæçćĉċčďđðèéêëēĕėęěĝğġģĥħìíîïĩ īĭįıijĵķĸĺŀļľ łńņňʼnñŋòóôõöōŏőœøŕŗřśŝşšșţțťŧ ùúûüũūŭůűųŵÿýŷźżžſþĸ
PR OPORT IONAL & TABUL AR LINING NU MERALS
SMALL CAP S & ALL SMALL CAP S
LIGAT URES
fi ff ffi fj ffj fl ffl fb fh fk fl tt ft Tb Th Tk Tl Ti ch ck ct st PR OPORT IONAL & TABUL AR OLD ST YLE NU MERALS
00123456789$¢€£¥ 0012345689$¢€£¥
abcdefghijklmnopqrstuvwxyz0123456789&¡!¿?@ \|/()[]{}àáâãäåāăąæçćĉċčďđðèéêëēĕėęěĝğġ ģĥħìíîïĩīĭįıijĵķĸĺŀļľłńņňʼnñŋòóôõöōŏőœøŕ ŗřśŝşšșţțťŧùúûüũūŭůűųŵÿýŷźżžþ
WELLING TONâ&#x20AC;&#x2122;S EAR T HQUAKES, VOLCANOES & TSUNA MIS
REGULARLY
stumble cause the sheep, grazing in the bush, to
flail and wish they lived somewhere that was much safer.*
*Perhaps the lovely state of Pennsylvania.
Mount Ruapehu blows its top Trampers narrowly escape fury of the mountain three australians on holiday were taken by surprise — as well as GNS’s lead volcanologists — as Mt. Ruapehu unexpectedly erupted last night. The three climbers were about halfway up the summit of Ruapehu before they began to feel the first tremors. “At first we didn’t think much of it,” Brent Jacobs said. “We checked with the DOC Ranger before heading out in the morning and everything looked great. The weather was perfect. No signs of activity on Ruapehu” Jacobs and his group continued up the mountain for another 20 minutes before realizing what was actually happening. “We looked up and suddenly there were massive vents of smoke rising from the top, and heaps of massive molten rocks flying toward us. The ground was shaking so bad we could barely stand. We took off as fast as we could down the mountain, and probably made it down in about a quarter of the time it took to go up.”
The GNS was just as surprised by the eruption. “Nature is unpredictable,” Brian Carter exclaimed. “We have teams out there constantly monitoring the volcanoes, looking for signs of activity. This one just completely took us by surprise. Luckily not many people were on the mountain.” Meanwhile, surrounding towns and villages have been evacuated, and a camp has been set up outside of Taumaranui to provide basic necessities for displaced residents. No major damage has been reported yet, but the activity shows no signs of slowing down. The DOC has closed all major roads in the area and is prohibiting entry into the park until further notice. Ruapehu’s last eruption in 2007 sent a lahar carrying approximately 1.4 million cubic meters of mud, rock, and water down the Whangaehu river. The events of this story are completely fictitious.
Major Volcanoes of New Zealand NAME
ELEVATION (m)
LAST ERUPTED
Auckland Volcanic Field................................... 260.............................. 1350 Maroa.. ....................................................... 1,156................................ 180 Monowai Seamount...................................... -100.............................. 2008 Mount Ngauruhoe.. ...................................... 2,291.............................. 1977 Okataina..................................................... 1,111.............................. 1973 Raoul Island................................................... 516.............................. 2006 Reporoa caldera.. ............................................ 592.............................. 1180 Mount Ruapehu.. ......................................... 2,797.............................. 2007 Mount Taranaki.. .......................................... 2,518.............................. 1755 Lake Taupo..................................................... 760................................ 181 Mount Tarawera........................................... 1,131.............................. 1886 Mount Tongariro.......................................... 1,968.............................. 1926 Waiotapu....................................................... 592.............................. 1180 White Island.. ................................................. 321.............................. 2001
Sample Text OTARI LIGHT 6/8
In 1855 an earthquake, with an estimated magnitude of 8.2, struck the Waiarapa fault line. In some areas the ground was uplifted up to six metres. Wellington’s central business district sits almost entirely on land that was below sea level before what is believed to be NZ’s most powerful earthquake since European colonization.
OTARI LIGHT 8/10
In 1855 an earthquake, with an estimated magnitude of 8.2, struck the Waiarapa fault line. In some areas the ground was uplifted up to six metres. Wellington’s central business district sits almost entirely on land that was below sea level before what is believed to be NZ’s most powerful earthquake since European colonization.
OTARI LIGHT 10/1 2 In 1855 an earthquake, with an estimated magnitude of 8.2, struck the Waiarapa fault line. In some areas the ground was uplifted up to six metres. Wellington’s central business district sits almost entirely on land that was below sea level before what is believed to be NZ’s most powerful earthquake since European colonization. OTARI LIGHT 1 2/15
In 1855 an earthquake, with an estimated magnitude of 8.2, struck the Waiarapa fault line. In some areas the ground was uplifted up to six metres. Wellington’s central business district sits almost entirely on land that was below sea level before what is believed to be NZ’s most powerful earthquake since European colonization.
OTARI LIGH T 14/17
In 1855 an earthquake, with an estimated magnitude of 8.2, struck the Waiarapa fault line. In some areas the ground was uplifted up to six metres. Wellington’s central business district sits almost entirely on land that was below sea level before what is believed to be NZ’s most powerful earthquake since European colonization. OTARI LIGHT 18/22
In 1855 an earthquake, with an estimated magnitude of 8.2, struck the Waiarapa fault line. In some areas the ground was uplifted up to six metres. Wellington’s central business district sits almost entirely on land that was below sea level before what is believed to be NZ’s most powerful earthquake since European colonization. OTARI LIGHT 24/28
In 1855 an earthquake, with an estimated magnitude of 8.2, struck the Waiarapa fault line. In some areas the ground was uplifted up to six...
OTARI LIGHT ITALIC 6/8 In 1855 an earthquake, with an estimated magnitude of 8.2, struck the Waiarapa fault line. In some areas the ground was uplifted up to six metres. Wellington’s central business district sits almost entirely on land that was below sea level before what is believed to be NZ’s most powerful earthquake since European colonization.
OTARI LIGHT ITALIC 8/10
In 1855 an earthquake, with an estimated magnitude of 8.2, struck the Waiarapa fault line. In some areas the ground was uplifted up to six metres. Wellington’s central business district sits almost entirely on land that was below sea level before what is believed to be NZ’s most powerful earthquake since European colonization.
OTARI LIGHT ITALIC 10/1 2 In 1855 an earthquake, with an estimated magnitude of 8.2, struck the Waiarapa fault line. In some areas the ground was uplifted up to six metres. Wellington’s central business district sits almost entirely on land that was below sea level before what is believed to be NZ’s most powerful earthquake since European colonization. OTARI LIGHT ITALIC 1 2/15
In 1855 an earthquake, with an estimated magnitude of 8.2, struck the Waiarapa fault line. In some areas the ground was uplifted up to six metres. Wellington’s central business district sits almost entirely on land that was below sea level before what is believed to be NZ’s most powerful earthquake since European colonization.
OTARI LIGHT ITALIC 14/17
In 1855 an earthquake, with an estimated magnitude of 8.2, struck the Waiarapa fault line. In some areas the ground was uplifted up to six metres. Wellington’s central business district sits almost entirely on land that was below sea level before what is believed to be NZ’s most powerful earthquake since European colonization. OTARI LIGHT ITALIC 18/22
In 1855 an earthquake, with an estimated magnitude of 8.2, struck the Waiarapa fault line. In some areas the ground was uplifted up to six metres. Wellington’s central business district sits almost entirely on land that was below sea level before what is believed to be NZ’s most powerful earthquake since European colonization. OTARI LIGHT ITALIC 24/28
In 1855 an earthquake, with an estimated magnitude of 8.2, struck the Waiarapa fault line. In some areas the ground was uplifted up to six...
OTARI REGUL AR 6/8
In 1855 an earthquake, with an estimated magnitude of 8.2, struck the Waiarapa fault line. In some areas the ground was uplifted up to six metres. Wellington’s central business district sits almost entirely on land that was below sea level before what is believed to be NZ’s most powerful earthquake since European colonization.
OTARI REGUL AR 8/10 In 1855 an earthquake, with an estimated magnitude of 8.2, struck the Waiarapa fault line. In some areas the ground was uplifted up to six metres. Wellington’s central business district sits almost entirely on land that was below sea level before what is believed to be NZ’s most powerful earthquake since European colonization.
OTARI REGUL AR 10/1 2 In 1855 an earthquake, with an estimated magnitude of 8.2, struck the Waiarapa fault line. In some areas the ground was uplifted up to six metres. Wellington’s central business district sits almost entirely on land that was below sea level before what is believed to be NZ’s most powerful earthquake since European colonization. OTARI REGUL AR 1 2/15
In 1855 an earthquake, with an estimated magnitude of 8.2, struck the Waiarapa fault line. In some areas the ground was uplifted up to six metres. Wellington’s central business district sits almost entirely on land that was below sea level before what is believed to be NZ’s most powerful earthquake since European colonization.
OTARI REGUL AR 14/17
In 1855 an earthquake, with an estimated magnitude of 8.2, struck the Waiarapa fault line. In some areas the ground was uplifted up to six metres. Wellington’s central business district sits almost entirely on land that was below sea level before what is believed to be NZ’s most powerful earthquake since European colonization. OTARI REGUL AR 18/22
In 1855 an earthquake, with an estimated magnitude of 8.2, struck the Waiarapa fault line. In some areas the ground was uplifted up to six metres. Wellington’s central business district sits almost entirely on land that was below sea level before what is believed to be NZ’s most powerful earthquake since European colonization. OTARI REGUL AR 24/28
In 1855 an earthquake, with an estimated magnitude of 8.2, struck the Waiarapa fault line. In some areas the ground was uplifted up to six...
OTARI REGUL AR ITALIC 6/8 In 1855 an earthquake, with an estimated magnitude of 8.2, struck the Waiarapa fault line. In some areas the ground was uplifted up to six metres. Wellington’s central business district sits almost entirely on land that was below sea level before what is believed to be NZ’s most powerful earthquake since European colonization.
OTARI REGUL AR ITALIC 8/10 In 1855 an earthquake, with an estimated magnitude of 8.2, struck the Waiarapa fault line. In some areas the ground was uplifted up to six metres. Wellington’s central business district sits almost entirely on land that was below sea level before what is believed to be NZ’s most powerful earthquake since European colonization.
OTARI REGUL AR ITALIC 10/1 2 In 1855 an earthquake, with an estimated magnitude of 8.2, struck the Waiarapa fault line. In some areas the ground was uplifted up to six metres. Wellington’s central business district sits almost entirely on land that was below sea level before what is believed to be NZ’s most powerful earthquake since European colonization. OTARI REGUL AR ITALIC 1 2/15
In 1855 an earthquake, with an estimated magnitude of 8.2, struck the Waiarapa fault line. In some areas the ground was uplifted up to six metres. Wellington’s central business district sits almost entirely on land that was below sea level before what is believed to be NZ’s most powerful earthquake since European colonization.
OTARI REGUL AR ITALIC 14/17
In 1855 an earthquake, with an estimated magnitude of 8.2, struck the Waiarapa fault line. In some areas the ground was uplifted up to six metres. Wellington’s central business district sits almost entirely on land that was below sea level before what is believed to be NZ’s most powerful earthquake since European colonization. OTARI REGUL AR ITALIC 18/22
In 1855 an earthquake, with an estimated magnitude of 8.2, struck the Waiarapa fault line. In some areas the ground was uplifted up to six metres. Wellington’s central business district sits almost entirely on land that was below sea level before what is believed to be NZ’s most powerful earthquake since European colonization. OTARI REGUL AR ITALIC 24/28
In 1855 an earthquake, with an estimated magnitude of 8.2, struck the Waiarapa fault line. In some areas the ground was uplifted up to six...
OTARI MEDIU M 6/8
In 1855 an earthquake, with an estimated magnitude of 8.2, struck the Waiarapa fault line. In some areas the ground was uplifted up to six metres. Wellington’s central business district sits almost entirely on land that was below sea level before what is believed to be NZ’s most powerful earthquake since European colonization.
OTARI MEDIU M 8/10
In 1855 an earthquake, with an estimated magnitude of 8.2, struck the Waiarapa fault line. In some areas the ground was uplifted up to six metres. Wellington’s central business district sits almost entirely on land that was below sea level before what is believed to be NZ’s most powerful earthquake since European colonization.
OTARI MEDIU M 10/1 2 In 1855 an earthquake, with an estimated magnitude of 8.2, struck the Waiarapa fault line. In some areas the ground was uplifted up to six metres. Wellington’s central business district sits almost entirely on land that was below sea level before what is believed to be NZ’s most powerful earthquake since European colonization. OTARI MEDIU M 1 2/15
In 1855 an earthquake, with an estimated magnitude of 8.2, struck the Waiarapa fault line. In some areas the ground was uplifted up to six metres. Wellington’s central business district sits almost entirely on land that was below sea level before what is believed to be NZ’s most powerful earthquake since European colonization.
OTARI MEDIU M 14/17
In 1855 an earthquake, with an estimated magnitude of 8.2, struck the Waiarapa fault line. In some areas the ground was uplifted up to six metres. Wellington’s central business district sits almost entirely on land that was below sea level before what is believed to be NZ’s most powerful earthquake since European colonization. OTARI MEDIU M 18/22
In 1855 an earthquake, with an estimated magnitude of 8.2, struck the Waiarapa fault line. In some areas the ground was uplifted up to six metres. Wellington’s central business district sits almost entirely on land that was below sea level before what is believed to be NZ’s most powerful earthquake since European colonization. OTARI MEDIU M 24/28
In 1855 an earthquake, with an estimated magnitude of 8.2, struck the Waiarapa fault line. In some areas the ground was uplifted up to six...
OTARI MEDIU M ITALIC 6/8 In 1855 an earthquake, with an estimated magnitude of 8.2, struck the Waiarapa fault line. In some areas the ground was uplifted up to six metres. Wellington’s central business district sits almost entirely on land that was below sea level before what is believed to be NZ’s most powerful earthquake since European colonization.
OTARI MEDIU M ITALIC 8/10
In 1855 an earthquake, with an estimated magnitude of 8.2, struck the Waiarapa fault line. In some areas the ground was uplifted up to six metres. Wellington’s central business district sits almost entirely on land that was below sea level before what is believed to be NZ’s most powerful earthquake since European colonization.
OTARI MEDIU M ITALIC 10/1 2 In 1855 an earthquake, with an estimated magnitude of 8.2, struck the Waiarapa fault line. In some areas the ground was uplifted up to six metres. Wellington’s central business district sits almost entirely on land that was below sea level before what is believed to be NZ’s most powerful earthquake since European colonization. OTARI MEDIU M ITALIC 1 2/15
In 1855 an earthquake, with an estimated magnitude of 8.2, struck the Waiarapa fault line. In some areas the ground was uplifted up to six metres. Wellington’s central business district sits almost entirely on land that was below sea level before what is believed to be NZ’s most powerful earthquake since European colonization.
OTARI MEDIU M ITALIC 14/17
In 1855 an earthquake, with an estimated magnitude of 8.2, struck the Waiarapa fault line. In some areas the ground was uplifted up to six metres. Wellington’s central business district sits almost entirely on land that was below sea level before what is believed to be NZ’s most powerful earthquake since European colonization. OTARI MEDIU M ITALIC 18/22
In 1855 an earthquake, with an estimated magnitude of 8.2, struck the Waiarapa fault line. In some areas the ground was uplifted up to six metres. Wellington’s central business district sits almost entirely on land that was below sea level before what is believed to be NZ’s most powerful earthquake since European colonization. OTARI MEDIU M ITALIC 24/28
In 1855 an earthquake, with an estimated magnitude of 8.2, struck the Waiarapa fault line. In some areas the ground was uplifted up to six...
OTARI BOLD 6/8
In 1855 an earthquake, with an estimated magnitude of 8.2, struck the Waiarapa fault line. In some areas the ground was uplifted up to six metres. Wellington’s central business district sits almost entirely on land that was below sea level before what is believed to be NZ’s most powerful earthquake since European colonization.
OTARI BOLD 8/10
In 1855 an earthquake, with an estimated magnitude of 8.2, struck the Waiarapa fault line. In some areas the ground was uplifted up to six metres. Wellington’s central business district sits almost entirely on land that was below sea level before what is believed to be NZ’s most powerful earthquake since European colonization.
OTARI BOLD 10/1 2 In 1855 an earthquake, with an estimated magnitude of 8.2, struck the Waiarapa fault line. In some areas the ground was uplifted up to six metres. Wellington’s central business district sits almost entirely on land that was below sea level before what is believed to be NZ’s most powerful earthquake since European colonization. OTARI BOLD 1 2/15
In 1855 an earthquake, with an estimated magnitude of 8.2, struck the Waiarapa fault line. In some areas the ground was uplifted up to six metres. Wellington’s central business district sits almost entirely on land that was below sea level before what is believed to be NZ’s most powerful earthquake since European colonization.
OTARI BOLD 14/17
In 1855 an earthquake, with an estimated magnitude of 8.2, struck the Waiarapa fault line. In some areas the ground was uplifted up to six metres. Wellington’s central business district sits almost entirely on land that was below sea level before what is believed to be NZ’s most powerful earthquake since European colonization. OTARI BOLD 18/22
In 1855 an earthquake, with an estimated magnitude of 8.2, struck the Waiarapa fault line. In some areas the ground was uplifted up to six metres. Wellington’s central business district sits almost entirely on land that was below sea level before what is believed to be NZ’s most powerful earthquake since European colonization. OTARI BOLD 24/28
In 1855 an earthquake, with an estimated magnitude of 8.2, struck the Waiarapa fault line. In some areas the ground was uplifted up to six...
OTARI BOLD ITALIC 6/8
In 1855 an earthquake, with an estimated magnitude of 8.2, struck the Waiarapa fault line. In some areas the ground was uplifted up to six metres. Wellington’s central business district sits almost entirely on land that was below sea level before what is believed to be NZ’s most powerful earthquake since European colonization.
OTARI BOLD ITALIC 8/10
In 1855 an earthquake, with an estimated magnitude of 8.2, struck the Waiarapa fault line. In some areas the ground was uplifted up to six metres. Wellington’s central business district sits almost entirely on land that was below sea level before what is believed to be NZ’s most powerful earthquake since European colonization.
OTARI BOLD ITALIC 10/1 2 In 1855 an earthquake, with an estimated magnitude of 8.2, struck the Waiarapa fault line. In some areas the ground was uplifted up to six metres. Wellington’s central business district sits almost entirely on land that was below sea level before what is believed to be NZ’s most powerful earthquake since European colonization. OTARI BOLD ITALIC 1 2/15
In 1855 an earthquake, with an estimated magnitude of 8.2, struck the Waiarapa fault line. In some areas the ground was uplifted up to six metres. Wellington’s central business district sits almost entirely on land that was below sea level before what is believed to be NZ’s most powerful earthquake since European colonization.
OTARI BOLD ITALIC 14/17
In 1855 an earthquake, with an estimated magnitude of 8.2, struck the Waiarapa fault line. In some areas the ground was uplifted up to six metres. Wellington’s central business district sits almost entirely on land that was below sea level before what is believed to be NZ’s most powerful earthquake since European colonization. OTARI BOLD ITALIC 18/22
In 1855 an earthquake, with an estimated magnitude of 8.2, struck the Waiarapa fault line. In some areas the ground was uplifted up to six metres. Wellington’s central business district sits almost entirely on land that was below sea level before what is believed to be NZ’s most powerful earthquake since European colonization. OTARI BOLD ITALIC 24/28
In 1855 an earthquake, with an estimated magnitude of 8.2, struck the Waiarapa fault line. In some areas the ground was uplifted up to six...
OTARI HEAV Y 6/8
In 1855 an earthquake, with an estimated magnitude of 8.2, struck the Waiarapa fault line. In some areas the ground was uplifted up to six metres. Wellington’s central business district sits almost entirely on land that was below sea level before what is believed to be NZ’s most powerful earthquake since European colonization.
OTARI HEAV Y 8/10
In 1855 an earthquake, with an estimated magnitude of 8.2, struck the Waiarapa fault line. In some areas the ground was uplifted up to six metres. Wellington’s central business district sits almost entirely on land that was below sea level before what is believed to be NZ’s most powerful earthquake since European colonization.
OTARI HEAV Y 10/ 1 2 In 1855 an earthquake, with an estimated magnitude of 8.2, struck the Waiarapa fault line. In some areas the ground was uplifted up to six metres. Wellington’s central business district sits almost entirely on land that was below sea level before what is believed to be NZ’s most powerful earthquake since European colonization. OTARI HEAV Y 1 2/15
In 1855 an earthquake, with an estimated magnitude of 8.2, struck the Waiarapa fault line. In some areas the ground was uplifted up to six metres. Wellington’s central business district sits almost entirely on land that was below sea level before what is believed to be NZ’s most powerful earthquake since European colonization.
OTARI HEAV Y 14/17
In 1855 an earthquake, with an estimated magnitude of 8.2, struck the Waiarapa fault line. In some areas the ground was uplifted up to six metres. Wellington’s central business district sits almost entirely on land that was below sea level before what is believed to be NZ’s most powerful earthquake since European colonization. OTARI HEAV Y 18/22
In 1855 an earthquake, with an estimated magnitude of 8.2, struck the Waiarapa fault line. In some areas the ground was uplifted up to six metres. Wellington’s central business district sits almost entirely on land that was below sea level before what is believed to be NZ’s most powerful earthquake since European colonization. OTARI HEAV Y 24/28
In 1855 an earthquake, with an estimated magnitude of 8.2, struck the Waiarapa fault line. In some areas the ground was uplifted up to ...
OTARI HEAV Y ITALIC 6/8
In 1855 an earthquake, with an estimated magnitude of 8.2, struck the Waiarapa fault line. In some areas the ground was uplifted up to six metres. Wellington’s central business district sits almost entirely on land that was below sea level before what is believed to be NZ’s most powerful earthquake since European colonization.
OTARI HEAV Y ITALIC 8/10
In 1855 an earthquake, with an estimated magnitude of 8.2, struck the Waiarapa fault line. In some areas the ground was uplifted up to six metres. Wellington’s central business district sits almost entirely on land that was below sea level before what is believed to be NZ’s most powerful earthquake since European colonization.
OTARI HEAV Y ITALIC 10/1 2 In 1855 an earthquake, with an estimated magnitude of 8.2, struck the Waiarapa fault line. In some areas the ground was uplifted up to six metres. Wellington’s central business district sits almost entirely on land that was below sea level before what is believed to be NZ’s most powerful earthquake since European colonization. OTARI HEAV Y ITALIC 1 2/15
In 1855 an earthquake, with an estimated magnitude of 8.2, struck the Waiarapa fault line. In some areas the ground was uplifted up to six metres. Wellington’s central business district sits almost entirely on land that was below sea level before what is believed to be NZ’s most powerful earthquake since European colonization.
OTARI HEAV Y ITALIC 14/17
In 1855 an earthquake, with an estimated magnitude of 8.2, struck the Waiarapa fault line. In some areas the ground was uplifted up to six metres. Wellington’s central business district sits almost entirely on land that was below sea level before what is believed to be NZ’s most powerful earthquake since European colonization. OTARI HEAV Y ITALIC 18/22
In 1855 an earthquake, with an estimated magnitude of 8.2, struck the Waiarapa fault line. In some areas the ground was uplifted up to six metres. Wellington’s central business district sits almost entirely on land that was below sea level before what is believed to be NZ’s most powerful earthquake since European colonization. OTARI HEAV Y ITALIC 24/28
In 1855 an earthquake, with an estimated magnitude of 8.2, struck the Waiarapa fault line. In some areas the ground was uplifted up to...
The Story otari, Travis Kochelâ&#x20AC;&#x2122;s first type effort, aims to capture the essence of Wellington, New Zealand in a single typeface. The contrast of a colorful art scene and the conservative colonial British aesthetic, which is still evident in the capital city, laid the groundwork for this design. Otari is vibrant and contemporary, but serious and built to last. Its character shines in display type, but doesnâ&#x20AC;&#x2122;t interfere at text sizes. The name Otari is a nod to the Otari-Wilton Bush, a fantastic natural reserve in Wellington, where a number of the initial sketches were produced. T HE DES IGNER Travis Kochel grew up in rural Pennsylvania, and attended the School of the Art Institute of Chicago, where he received a Bachelor of Fine Arts in 2008. Travis is currently based in Wellington, New Zealand, where he makes a living as a self-employed graphic designer, focusing spare energy on type design, screenprinting and hiking around the country.
Various design around Wellington that served as inspiration for Otari
64.4.889.2996 design@traviskochel.com www.traviskochel.com www.traviskochel.com/tktype Š2009 Travis Kochel. All rights reserved